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BÜKÜ KETERANGAN 

PETA SATUAN LAHAN DAN TANAH 

LEMBAR TANJUNGKARANG, SUMATERA 

EXPLANATORY BOOKLET OF THE LAND UNIT AND SOIL MAP 

OF THE TANJUNGKARANG SHEET, SUMATERA 

Oleh/By : 

Junus Dai, H. Darul SWP, A. Hidayat, H.Y. Sumulyadi, Hendra S., Yayat AH, 

A. Hermawan, P. Buurman, T. Balsem 

SEKALAISCALE 1 : 250.000 

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3° -. \ ^V 

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-6° 

i i i i i i 

1011 

IQJOÄ 

LEMBARjSHEET : 1110 

105° 

ii!\ 1211 

1 t 

1210 

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Penanggung jawab 

Head of the Project 

DR. M. SUDJADI 

Kepala Pusat Penelitian Tanah 

Badan Penelitian dan Pengembangan Pertanian 

Depaitemen Pertanian 

The Director of the Center for Soil Research 

Agency for Agricultural Research and Development 

Department of Agriculture 

Urusan mengenai publikasi ini harus dialamatkan kepada: 

Kepala Pusat Penelitian Tanah 

Jalan H. Juanda 98, Tilpon 23012 

Bogor 16123, Indonesia 

Correspondence concerning this publication should be addressed to: 

The Director of the Center for Soil Research 

Jalan H. Juanda 98, Phone 23012 

Bogor 16123, Indonesia

BUKU KETERANGAN 

PETA SATUAN LAHAN dan TANAH LEMBAR TANJUNGKARÄNG (1110), SUMATERA 

Explanatory booklet of the 

LAND UNIT and SOIL map of the Tanjungkarang Sheet (1110), Sumatra 

Sekala/Scale 1 : 250.000 

Oleh/By: 

Junus Dai, H.Darul SWP, A.Hidayat, H.Y.Sumulyadi, Hendra S., 

Yayat A.H., A.Hermawan, P.Buurman dan/and T.Balsem. 

Buku Keterangan Peta Satuan Lahan dan Tanah ini dihasilkan oleh Tim 

Pengelolaan Data Base Tanah dari Proyek Perencanaan dan Evaluasl 

Sumber Daya Lahan, program kerja sama teknis antara Pemerintah 

Republik Indonesia dan Bank Pembangunan Asia, .dilaksanakan oleh 

Pusat Penelitian Tanah (Badan Penelitian dan 'Pengembangan Pertanian, 

Departemen Pertanian) dan dikoordinasikan oleh Badan Koordinasi 

Survei dan Pemetaan Nasional (BAKOSURTANAL). Survei dan 

pemetaan dilaksanakan oleh Pusat Penelitian Tanah bekeriasama 

dengan konsultan dari HASKONING Royal Dutch Consulting Engineers 

and Architects. 

This Explanatory Booklet and the accompanying Land Unit and Soil 

map have been produced by the Soil Data Base Management Team of the 

Land Resource Evaluation and Planning Project (LREP, part II), a 

technical cooperation programme between the Government of the 

Republic of Indonesia and the Asian Development Bank, executed by 

the Center for Soil Research (part of the Agency for Agricultural 

Research and Development of the Department of Agriculture) and supervised 

by the National Coordination Agency for Surveys and Mapping 

(BAKOSURTANAL). The survey and mapping were carried out by 

the Center for Soil Research, in cooperation with the consultants 

of HASKONING Royal Dutch Consulting Engineers and Architects. 

PUSAT PENELITIAN TANAH 

BADAN PENELITIAN DAN PENGEMBANGAN PERTANIAN 

DEPARTEMEN PERTANIAN 

CENTER for SOIL RESEARCH 

AGENCY for AGRICULTURAL RESEARCH and DEVELOPMENT 

DEPARTMENT of AGRICULTURE

Hak cipta dilindungi. Tidak sebagianpun dari publikasi ini dapat direproduksi 

kembali, disimpan dalam suatu sistim penyimpanan dan penarikan data, atau 

dipindahkan kedalam bentuk apapun atau dengan alat/cara seperti : elektronik, 

elektrostatik, pita magnetik, mekanik, fotokopi, direkam atau sejenisnya tanpa 

adanya ijin secara tertulis dari penerbit. 

Edisi pertama, 1989. 

All Rights Reserved. No part of this publication may be reproduced, stored in a 

retrieval system or transmitted in any form or by any means: electronic, 

electrostatic, magnetic tape, mechanical, photocopying, recording or otherwise, 

without permission in writing from the publishers. 

First edition, 1989. 

Cara merujuk buku ini: 

Junus Dai, H.Darul SWP, A.Hidayat, H.Y.Sumulyadi, Hendra S., Yayat A.H.,, 

A.Hermawan, P.Buurman dan T.Balsem, 1989. Buku Keterangan Peta Satuan Lahan 

dan Tanah lembar Tanjungkarang (1110), Sumatera. Pusat Penelitlan Tanah. Bogor. 

How to cite this book: 

Junus Dai, H.Darul SWP, A.Hidayat, H.Y.Sumulyadi, Hendra S., Yayat A.H.', 

A.Hermawan, P.Buurman and T.Balsem, 1989. Explanatory booklet of the Land 

Unit and Soil map of the Tanjungkarang Sheet (1110), Sumatra. Center for Soil 

Research, Bogor. 

Scanned from original by ISRIC - World Soil Information, as ICSU 

World Data Centre for Soils. The purpose is to make a safe 

depository for endangered documents and to make the accrued 

information available for consultation, following Fair Use 

Guidelines. Every effort is taken to respect Copyright of the 

materials within the archives where the identification of the 

Copyright holder is clear and, where feasible, to contact the 

originators. For questions please contact soil.isric@wur.nl 

indicating the item reference number concerned. 

1110 - ii

PENUNTON UNTÜK PEMAKAI USER MANUAL 

Buku keterangan ini adaiah penjelasan 

dari Peta Satuan Lahan dan Tanah lembar 

Tanjungkarang (1110), Sumatera, 

sekala 1:250.000. 

Legenda peta berisikan satuan lahan 

yang merupakan satuan geomorfik dan 

dibatasi dengan cara menginterpretasi 

foto udara, citra satelit dan citra 

Radar. Isi dari tiap satuan lahan 

diperiksa di lapangan dan kemudian 

dicatat. Hanya sebagian dari semua informasi 

ini disajikan dalam peta, 

sedangkan sebagian lagi diberikan 

secara ringkas dalam Buku Keterangan 

ini; informasi yang -lebih lengkap 

dapat tersedia jika diminta. 

Simbol peta menunjukan grup fisiografi 

(huruf besar), tipe batuan (huruf 

kecil), dan pembagian lebih lanjut 

berdasarkan atas lereng dan tingkat 

torehan (pada daerah berlereng dan 

angkatan) atau berdasarkan lingkungan 

pengendapan/hidrologinya (pada daerah 

aluvial resen dan marin), yang ditunjukan 

oleh angka. Huruf kecil yang 

berada dimuka kode. grup fisiografi 

menunjukan adanya tutupan dari bahan 

lain, seperti tutupan abu volkan pada 

perbukitan dari batuan sedimen atau 

lapisan bahan organik tipis pada 

dataran aluvial. 

Grup fisiografi tersebut adaiah : 

Kubah Gambut, Aluvial, Marin, Teras 

Marin, Dataran Tuf Masam, Dataran, Tuf 

Masam Toba, Volkan, Karst, Perbukitan, 

Pegunungan/Plato dan Aneka Bentuk. 

Grup Dataran Tuf Masam, Tuf Masam 

Toba, Volkan, Kubah Gambut dan Karst 

pembagiannya didasarkan pada tipe 

batuan dan morfologi yang spesifik 

yang hubungannya erat dengan sifat 

tanah yang spesifik. Grup yang lainnya 

sebagian besar hanya berdasarkan pada 

morfologi. 

Untuk semua satuan lahan, data keadaan 

tanah dan hubungari tanah dengan bentang 

alam disajikan pada Uraian 

1110 - iii 

This booklet, is an explanation of the 

1:250,000 scale Land Unit and Soil map 

of the Tanjungkarang mapsheet (1110), 

Sumatra. 

The legend of the map consists of Land 

Units, which are geomorphic units, 

delineated by interpretation of images 

such as aerial photographs, satellite 

imagery and Synthetic Aperture Radar. 

The contents of each of the units is 

checked in the field and recorded. 

Only part of this information can be 

represented in the map; the remainder 

is briefly documented in the present 

explanatory notes, • and more complete 

information is available upon request. 

Map symbols indicate physiographic 

group (capital letter), rock type 

(lower case letter), and subdivisions 

according to slope and dissection (in 

sloping and uplifted areas) or to 

sedimentary/'hydrologieal environment 

(in recent alluvial and marine areas), 

indicated with numbers. Lower case 

letters preceding the physiographic 

group code are used to indicate covers 

of material with differing composition, 

such as volcanic ash covers on 

hills of sedimentary rocks, or thin 

peat on alluvial plain units. 

The physiographic groups are : Peat 

Domes, Alluvial, Marine, Marine Terrace, 

Acid Tuff Plains, Plains, Toba 

Acid Tuff, Volcanic, Karst, Hill, 

Mountain/Plateau and Miscellaneous. 

The Acid Tuff Plain, the Toba Acid 

Tuff, the Volcanic, the Peat Domes and 

the Karst group are based on rock type 

and specific morphology, with a close 

link to specific soil characterestics. 

The other groups are largely morphological 

. 

For all land units, data on soils and 

soil/landscape relations are presented 

in the Land Unit Descriptions. These

Satuan Lahan. Uraian satuan lahan ini 

merupakan bagian terpenting dari Buku 

Keterangan ini sebab semua informasi 

yang diperlukan untuk mengevaluasi 

setiap satuan lahan untuk penggunaan 

tertentu disajikan disini. 

Semua informasi geografik dapat 

diperoleh dal am format komputer 

(didigitasi). Semua data utama dari 

tanah (dari profil yang dianalisis) 

juga disimpan dalam komputer dan dapat 

tersedia bagi para pemakai yang memerlukan. 

Pada tahap selanjutnya, 

limai; imi-nlr 

I «I,,,— 4- 1 

yang mempergunakan parameter-parameter 

yang ada pada diskripsi satuan lahan 

akan segera disidiakan oleh Proyek 

Pengelolaan Data Base Tanah (PDBT). 

Permintaan untuk penilaian Kesesuaian 

Lahan dari tiap satuan lahan untuk 

berbagai keperluan dapat diajukan ke 

Pusat Penelitian Tanah, Bogor. 

1110 - iv 

descriptions form an essential part of 

the Explanatory Notes, because all information 

that is necessary to 

evaluate a land unit for specific uses 

is listed here. 

All geographic information is available 

in computer (digitized) format. 

All primary soil information (analyzed 

profiles) is also computerized and can 

be made available to the user. At a 

later stage, land evaluation software 

which uses the parameters listed in 

made available by the Soil Data Base 

Management Proyect (SDBM). 

Requests for suitability ratings of 

the land units for various purposes 

can be submitted to the Center for 

Soil Research, Bogor.

I DAFTAR 

ISI 

1. Pendahuluan 

Hal aman 

1 

1.1. Latar belakang 1 

1.2. Konsepsi legenda 1 

1.3. Struktur legenda satuan lahan 2 

2 . Metodologi 3 

2.1. Peta dasar 3 

2.2. Interpretasi citra 4 

2.3. Survei dan data lapangan 4 

2.4. Uraian satuan lahan : 5 

2.5. Data base dan pengelolaan data 6 

2.6. Relaibilitas peta 9 

3. Lokasi daerah peta dan sumber informasi 10 

3.1. Lokasi dan batas administrasi 10 

3.2. Sumber informasi 10 

4. Keadaan umum fisik daerah 10 

4.1. Geologi 10 

4.2. Fisiografi 16 

4.3. Hidrologi 18 

5. Satuan lahan 19 

5.1. Satuan lahan dan tanah 19 

5.2. I si uraian satuan lahan 24 

6. Daf tar pustaka 25 

Laporan pemetaan tanah 25 

Daftar Gambaran 

Gambar 1. Lokasi peta dan batas administrasi 7 

Gambar 2. Relaibilitas peta 8 

Gambar 3. Indeks peta topografi dan jalur terbang potret udara_ 11 

Gambar 4. Indeks citra Radar STAR-1 dan Landsat . . . 12 

Gambar 5. Indeks laporan survei dan pemetaan tanah 13 

Gambar 6. Peta geologi bagan. 14 

Gambar 7. Grup fisiograf i 15 

Gambar 8. Satuan lahan, blok diagram dan penampang melintang 23 

Daftar Tabel 

Tabel 1. Grup fisiografi 2 

Tabel 2. Analisis standar dan tambahan PDBT 5 

Tabel 3. Nomor dan nama lembaran peta topografi sekala 1:50.000 10 

Lampiran 

Lampiran 1. Uraian satuan lahan 26 

1110 - v

CONTENTS 

1. Introduction 

Page 

1 

1.1. Background 1 

1.2. Legend concept 1 

1.3. Structure of the land unit legend. . 2 

2. Methodology 3 

2.1. Base maps 3 

2.2. Image interpretation 4 

2.3. Field survey and field data ' 4 

2.4. Land unit description 5 

2.5. Data bases and data processing 6 

2.6. Map reliability .... " 

2. (Hay location and sources of information) 10 

3.1. (Location and administrative boundaries) 10 

3.2. (Sources of information) 10 

4. (General physiography of the area) 10 

4.1. (Geology) 10 

4.2. (Physiography) 16 

4.3. (Hydrology) 18 

5. (Land units) 19 

5.1. (Land units and soils) 19 

5.2. (Contents of a land unit description) 24 

6. (References) 25 

(Soil survey reports) 25 

List of Figures 

Figure 1. Location and administrâtive boundaries 7 

Figure 2. Map reliability 8 

Figure 3. Index of topographic maps and flight lines of aerial photos .. 11 

Figure 4. Index of STAR-1 Radar and Landsat imagery 12 

Figure 5. Index of soil survey reports 13 

Figure 6. Geological sketch map : 14 

Figure 7. Physiographic groups 15 

Figure 8. Land units, block diagram and cross section' 23 

List of Tables 

Table 1. Physiographic groups 2 

Table 2. Standard and additional SDBM soil analyses 5 

Table 3. Numbers and names of 1:50,000 topographic maps 10 

Appendix 

Appendix 1 : Land unit descriptions •....• 27 

1110 - vi

1. PENDAHULUAN 2. INTRODUCTION 

l.l.Latar belakang 

Buku Keterangan dan Peta Satuan Lahan 

& Tanah ini merupakan sebagian hasil 

akhir survei tanah tinjau Sumatra yang 

dilaksanakan untuk Proyek Perencanaan 

dan Evaluasi Sumber Daya Lahan dan 

diprakarsai tahun 1985 oleh Pemerintah 

Indonesia serta dibiayai oleh Bank 

Pembangunan Asia. 

Pelaksanaan survei dilakukan oleh Tim 

Survei Tanah dari Pusat Penelitian 

Tanah, sedangkan korelasinya dilakukan 

pada bulan Januari - Februari 1989. 

1.2.Konsepsi legenda 

Legenda untuk survei ini didasarkan 

pada pendekatan satuan lahan. Pendekatan 

ini dianggap paling sesuai untuk 

survei ini, sebab pada sekala 

1:250.000 dengan intensitas pengamatan 

lapangan yang kurang, semua batas 

satuan dapat ditarik dengan cara 

menginterpretasi citra. Legenda satuan 

lahan memungkinkan adanya pembatasan 

setiap satuan dengan sembarang ukuran 

yang masih dapat dipetakan (tergantung 

skala peta) dengan memanfaatkan namanama 

morfologi sederhana dan 

berulang. Pendekatan ini menunjang 

Struktur hirarki dan merupakan sistem 

terbuka sehingga dapat diperbaharui 

sesuai dengan penerapannya di Indonesia; 

ia tidak memuat parameter 

iklim (parameter ikllm disimpan dalam 

data base terpisah dan dapat digabung 

dengan data base satuan lahan). 

Tambahan pula legenda satuan lahan 

erat hubungannya dengan legenda terdahulu 

di Indonesia mengenai bentuk 

lahan, sistem lahan dan satuan lahan 

tanpa keliru penggunaannya 

(Desaunettes, 1977; RePPProT, 1985- 

1988; Kips et al., 1981). 

Satuan Lahan ini diberi batasan berupa 

lahan dimana satu atau lebih komponennya 

mempunyai ciri-ciri khusus dan 

merupakan satuan lingkungan dengan 

sembarang ukuran yang dapat dibatasi 

pada peta. Satuan terkecil yang masih 

1110 - 1 

2.2.Background 

This explanatory booklet and the included 

maps are part of the final 

results of the reconnaissance soil 

survey of Sumatra, which was carried 

out for the Land Resources Evaluation 

and Planning Project (LREP), initiated 

in 1985 by the Goverment of the 

Republic Indonesia and financed by the 

Asian Development Bank. 

The sheet was surveyed by teams of 

Center for Soil Research (CSR). Map 

correlation was done in January 

February 1989. 

1.2.Legend concept 

The legend for this survey is based on 

the Land Unit approach. This approach 

is considered most suitable for this 

survey, because at a scale of 

1:250,000 , with low-density field 

checks, all unit boundaries are obtained 

by image interprétât ion. The 

land unit legend allows the delineation 

of mappable units of any size 

(depending on map scale), it makes use 

of morphological names which are 

simple and recurrent, it supports an 

hierarchical structure, it is an open 

system that can be amended for use 

anywhere in Indonesia, and it does not 

contain climatic parameters (the 

climatic parameters are stored in a 

separate data base which can, be combined 

with the land unit data base). 

Furthermore, the land unit legend is 

closely related to previous Indonesian 

land form, land system and land unit 

legends (Desaunettes, 1977; RePPProT, 

1985-1988; Kips et al., 1981) without 

being confusing. 

A Land Unit is defined here as an area 

of land of which one or more attributes 

have special characteristics, 

and it refers to an environmental unit 

of any size that can be delineated. 

The smallest unit that can be

dapat dibatasi tanpa menghiraukan 

sekalanya berukuran 2 mm lebarnya bila 

bentük memanjang dan kurang lebih 3 

sampai 4 mm bila berbentuk bulat. Pada 

sekala 1:250.000, suatu satuan yang 

membulat dengan diagonal 4 mm meliputi 

kurang lebih 80 ha. 

Satuan lahan dikelompokkan dalam grupgrup 

fisiografi dan kadang-kadang 

dibagi lagi kedalam sub-grup. 

Untuk informasi lebih lengkap, lihat 

pada Buurman et al (1988) dan Balsem 

et al, (1989) 

1.3.Struktur legenda satuan lahan 

Semua satuan lahan diberi kode berupa 

huruf dan angka/dijit; masing-masing 

dengan konotasi khusus tergantung 

t ingkat kla s i f ika sinya. 

Contoh:Au.l.l.3- Dataran aluvial luas, 

tanggul sungai/alur-alur drainase. 

Grup Fisiografi 

Relief, ukuran besarnya 

Au.1.1.3 -Bentuk lahan/torehan/veqetasi 

Iitoloqi_ ' Sub-grup: Horfologi 

Tabel 1 ntenyajikan Grup Fisiografi 

yang diidentifikasi di Sumatra dan 

pulau-pulau di luarnya. Contoh-contoh 

pembagian lanjut hanya disajikan untuk 

grup Kubah Gambut dan grup Dataran. 

Tabel 1. Grup Fisiografi 

A. 

B. 

D. 

H-. 

I. 

K. 

M. 

P. 

Q. 

T. 

V. 

X. 

ALUVIAL 

MARIN 

KUBAH GAMBUT 

PERBUKITAN 

DATARAN TUF MASAM 

KARST 

PEGUNUNGAN/PLATO 

DATARAN 

TUF MASAM TOBA 

TERAS MARIN 

VOLKAN 

ANEKA BENTUK 

*) 

*) 

*) 

*) 

*) Tidak dijumpai pada lembar peta 

ini. 

delineated on any map, irrespective of 

scale is about 2 mm wide if it is a 

linear feature and about 3 to 4 mm 

across if it is a circular feature. 

At a scale of 1:250,000, a circular 

unit of 4 mm across has a surface of 

nearly 80 ha. 

Land units are grouped together in 

Physiographic Groups and, in some 

cases, in Sub-Groups. 

For more detailed information, see 

Buurman et al., (1988) and Balsem et 

al., (1989) 

1 -1 ^»-"'rt-jr: zf tha lotaî unit legend 

All mapping units are coded by means 

of a sequence of characters and 

digits, each with its specific connotation 

which depends on its level in 

the classification. 

Example: Au.1.1.3 -Broad Alluvial 

Plain; levee/spillway. 

Physiographic Group 

Relief magnitude 

I 

Au. 1.1.3 —Landf on/dissection 

/vegetation 

Lithology Subgroup : morphology 

Table 1 lists the Physiographic Groups 

which have been identified in Sumatra 

and the outer islands. Examples of 

subdivisions are given for the Peat 

Dome and Plain groups only. 

Table 1 : PhysiographicGroups 

A. 

B. 

D. 

H. 

I. 

K. 

M. 

P. 

Q- 

T. 

V. 

X. 

1110 - 2 

Alluvial 

Marine 

Peat Domes 

Hilly 

Acid Tuff Plain 

Karst 

Mountain/Plateau 

Plain 

Toba Acid Tuff 

Marine Terrace 

Volcanic 

Miscellaneous 

*) 

*) 

*) 

*) 

*) Not present in this mapsheet.

Pembagian lanjut grup Kubah Gambut dan Subdivision of the Peat Domes and 

Dataran adalah sebagai berikut. 

Plain groups : 

Kubah Gaabut - 

Dataran—litologi— 

eutrofik — 

oligotrofik- 

Bentuk wilayah 

datar— 

air tawar- 

tipis 2m 

pasang surut/bagian tepi 

kubah bergaram jsda 

air tawar ]Sda 

pasang sumt/bagian tepi 

kubah bergaram —|Sda 

Penorehan 

tanpa 

sedikit 

sedang 

sangat 

ekstrim 

datar - berombak 1 Sda 

beronbak 1 Sda 

beroibak - bergeloinbang-|Sda 

bergeloibang 1 Sda 

datar berbukit kecil —I Sda 

berombak berbukit kecil-j Sda 

Struktur legenda disusun demikian rupa 

sehingga lanskap datar, melandai, tertoreh, 

bergunung, dsb. dengan mudah 

d"apat dipilih oleh komputer. Struktur 

ini langsung berkait'an dengan potensi 

lahan untuk pertanian. 

2. METODOLOGI 

2.1.Peta dasar 

Peta dasar untuk keperluan pencetakan 

Peta Satuan Lahan & Tanah disediakan 

oleh BAKOSURTANAL. Untuk lembar peta 

ini, peta dasar yang digunakan adalah 

peta JOINT OPERATIONS GRAPHICS (JOG), 

Lembar SB48-7, Seri 1501, Edisi 3, 

Tanjungkarang yang dikeluarkan oleh 

Royal Australian Survey Corps, 1988. 

1110 - 3 

Peat Doues— I 

Plain—lithology— 

eutrophic— 

oligotrophic 

Land form 

flat- 

fresh water 

thin 2m 

tidal/saline fringes 

of domes—|ditto 

fresh water-1 ditto 

tidal/saline fringes 

of domes—| ditto 

Dissection 

none 

slight 

moderate 

strong 

extreme 

flat to undulating 1 ditto 

undulating 1 ditto 

undulating to rolling—|ditto 

rolling 1 ditto 

flat with hillocks 1 ditto 

undulating with hillocks| ditto 

The legend structure is such, Chat 

flat, sloping, dissected, mountainous 

landscapes, etc., are easily selected 

by computer. The structure is directly 

related to agricultural potential of 

the land. 

2. METHODOLOGY 

2.1.Base maps 

Base maps for the printed Land Unit 

and Soil map were provided by BAKOSUR- 

TANAL. For the present sheet, the base 

map was the Joint Operations Graphics 

(JOG), Sheet SBU8-7, Series 1501, Edition 

3, Tanjungkarang, published by 

The Royal Australian Survey Corps 

1988.

2.2.Interpretasi citra 2.2.Image interpretation 

Survei tinjau ini sebagian besar 

didasarkan pada interpretasi citra dan 

batas-batas satuan sesungguhnya 

ditarik berdasarkan citra. Macam citra 

yang digunakan adalah sebagai berikut: 

-potret udara hitam/putih sekala 

1:100.000, Angkatan Udara Australia 

1976 (umumnya kualitas rendah karena 

dicetak berulang kali dan pemrosesan 

yang kurang baik). 

-LANDSAT komposit warna (band 4-5-6) 

sekala 1:250.000 tahun 1984/85 yang 

dioerni »V> H2r^ L»\rAlï (kualitas bervariasi, 

sekala kurang teliti). 

-citra Radar stereo STAR-1, 1988 

(cetakan hitäm putih, kualitas tak 

optimal). 

2.3.Survei dan data lapangan. 

Pelaksanaan survei tinjau dapat dibagi 

dalam beberapa tahapan kerja: 

l.penelaahan data dan informasi dari 

peta dan laporan tersedia. 

2.interpretasi citra dan penetapan 

daerah kunci 

3.pengamatan lapangan dan pemasukandata 

ke komputer 

4.penyusunan satuan lahan dan 

pemasukan data ke komputer. 

5.analisis contoh tanah 

ö.melengkapi uraian satuan lahan dengan 

data analisis. 

7.korelasi/verifikasi lapangan 

8.produksi peta akhir 

9.dijitasi peta dan pemrosesan data 

base lainnya. 

Semua pengamatan di lapangan (pemboran 

dan profil) dicatat, . diberi kode dan 

dimasukan sesuai dengan prosedur standar 

PDBT, seperti diuraikan dalam 

Laporan Tehnis PDBT No.5 (Balsem et 

al., 1988). Kode ini terutama diadap-~ 

tasi dari standar FAO dan USDA (FAO, 

1977; SCS, 1978; Gallup, 1978). 

Contoh tanah yang représentatif 

dianalisis sifat-sifatnya seperti yang 

disajikan pada Tabel 2. 

1110 - 4 

The surveys are extensively based on 

image interpretation and virtually all 

unit boundaries are imagery-based. The 

following imagery, was used: 

- 1:100,000 scale black/white aerial 

photography, Australian Airforce, 

1976, (usually poor quality due to 

recopying and poor processing). 

- 1:250,000 LANDSAT colour composites 

(bands 4-5-6), 1984/85, obtained 

from LAPAN ("Sirylïiè HâiiLy, macurate 

scale). 

- 1:250,000 STAR-1 stereo Radar imagery, 

1988 (black/white positive 

prints, quality not optimal). 

2.3.Field survey and field data 

The implementation of the reconnaissance 

survey can be split up into a 

number of essential steps : 

1. perusal of existing maps and reports 

2. image interpretation and selection 

of sample/key areas 

3. field observations and computer data 

entry 

4. preliminary land unit descriptions 

and computer data entry 

5. soil sample analyses 

6. completion of land unit descriptions 

with analytical data 

7. correlation/field verification 

8 . final map production 

9. map digitizing and other data base 

operations. 

All ob servations in the field 

(auger ings and profile pits) were 

described, coded and entered according 

to standard SDBH procedures as 

described in SDBM Technical Report 

No.5 (Balsem et al., 1988). These 

codes are mainly adapted from standard 

FAO and USDA codes (FAO, 1977; 

SCS,1978; Gallup, 1978). 

Representative soils were analyzed for 

the properties listed in Table 2.

Tabel 2. Analisis tanah standar dan 

tambahan PDBT. 

Analisis Standar 

1. tekstur 

2. karbon organik 

3. KTK NH40AC pH 7 

4. basa dapat ditukarkan dalam NH40Ac 

5. AI dalam KCl IM 

6. kerapatan lindak pF 2,5 

7. kadar air pF 4,2 

8. pH (H20, KCl , 1:2,5) 

9. N total 

10.K tersedia 

11.P tersedia 

Analisis tambahan 

untuk tanah volkanik: 

-kemasaman terekstraksi dalam BaC^- 

TEA (pH 8.2) 

- AI, Fe dan Si terekstraksi oksalat 

- mineralogi pasir 

- retensi fosfat 

untuk Oksisol: 

- mineralogi pasir 

untuk Spodosol: 

- Fe, A1,C terekstraksi pirofosfat 

- Fe, AI terekstraksi ditionit 

untuk endapan marin: 

- garam terlarut 

- kadar sulfur 

- kadar air lapangan (tanah belum 

matang) 

untuk tanah berkapur: 

- kadar karbonat 

untuk tanah Gambut: 

- kadar serat 

- kadar abu 

- kerapatan lindak 

2.4. Uraian satuan lahan 

Uraian satuan lahan berupa uraian umum 

yang dibuat untuk setiap satuan peta. 

Uraian yang dibuat ini merupakan 

generalisasi dari beberapa pengamatan. 

Atribut satuan lahan (lihat bab 5.2) 

digunakan untuk évaluasi lahan ybs. 

Struktur uraian satuan lahan 

didasarkan. pada suatu cara yang telah 

dipublikasikan oleh RePPProT (1988) 

dengan beberapa tambahan. Disamping 

dari pengamatan di lapangan dalam 

penyusunan uraian satuan lahan ini, 

Table 2. Standard and additional SDBM 

soil analyses. 

Standard Analyses 

1. 

2. 

3. 

4. 

5. 

6. 

1110 - 5 

teksture 

organic Carbon 

CEC NHUOAc pH 7 

exch. Bases in NH40Ac 

Al in 1 M KCl 

bulk density pF 2.5 

7. water content pF U.2 

8. pH (H2O, KCl, 1:2.5 

9. total N 

10 .available K 

11.available 

P 

Additional Analyses 

for Volcanic soils: 

- extractable acidity in BaC12-TEA 

- oxalate extractable Al, Fe and Si 

- sand mineralogy 

- phosphate retention 

for Oxisols: 

- sand mineralogy 

for Spodosols: 

- pyrophosphate extractable Fe, Al, C 

- dithionite extractable Fe, Al 

for marine deposits: 

- soluble salts 

- sulphur content 

- field moisture content (unripe 

soils) 

for calcareous soils: 

- carbonate content 

for peat soils: 

- fibre content 

- ash content 

- bulk density 

2.4.Land unit description 

Land Unit descriptions are general 

descriptions which are made for each 

of the mapping units. Such descriptions 

are generalizations of point observations. 

The land unit attibutes 

(5.2) are used for land evaluation. 

The structure of the land unit 

descriptions is based on those published 

by RePPProT (1988) with amendments. 

In addition to the field observations, 

the following sources were

juga dipergunakan beberapa inf.ormasi 

lain terutama dari : 

-RePPProT, 1988: Review of Phase I 

Results, Sumatra. 

-PPPG, 1978: Peta Geologi.Lembar Tânjungkarang, 

Sumatera, Sekala 

1:250.000. 

-Semua laporan survei yang tersedia 

dari daerah ybs (Gambar 5). 

2.5. Data Base dan Pengolahan Data. 

Seperti disebutkan diatas, semua data 

lapangan dan anal î cf.; disiuipari aal am 

data base. Data base yang utama ialah: 

-pengamatan lapangan (pemboran dan 

penampang tanah). 

-data analisis 

-uraian Satuan Lahan 

Data base pengamatan lapangan berisi 

semua parameter yang dapat diukur di 

lapangan dari setiap tempat pengamatan. 

Yang didiskripsi dan disimpan 

adalah nomor tempat/site, tempat, 

lereng, vegetasi/penggunaan lahan dan 

semua sifat-sifat tanah yang diukur di 

lapangan seperti Struktur, porositas, 

tekstur, warna, dll. (lihat Laporan 

Teknis PDBT No 5a, Versi 1.1 - Balsem 

et al., 1988). 

Data base analisis berisi semua hasil 

analisis kimia, fisika dan mineralogi 

serta semua data hasil perhitungan 

dari analisis ini yang biasanya dipergunakan 

untuk menilai kesuburan atau 

klasifikasi tanah (Lihat Laporan 

Teknis No 7a - Buurman, 1988; Laporan 

Teknis No 17, Muslihat et al., 1989). 

Pada data base pengamatan lapangan dan In both the field observations and in 

data base analisis, data dapat the analytical data base, data can be 

dikeluarkan dengan cara memanggil retrieved by observations number, map- 

/menuliskan nomor pengamatan, nomor sheet , legend unit, administrative 

lembar peta, satuan pada legenda, ad- area (province, kabupaten), and other 

ministrasi (kabupaten atau provinsi) areas defined by geographic coor- 

atau dengan yang lainnya yang ditentukan 

oleh koordinat geografik. 

dinates. 

Data base uraian satuan lahan berisi 

uraian umum dari tiap satuan peta untuk 

seluruh Pulau Sumatera yang 

dikatalogkan menurut lembar peta. 

1110 - 6 

used in the compilation of the land 

unit descriptions: 

- RePPProT, 1988 : Review of Phase I 

Results, Sumatra 

- GRDC, 1978 : Geologic Map of the 

Tanjungkarang Quadrangle, Sumatra, 

Scale 1:250 000. 

- All available survey reports for the 

area (Figure 5). 

2.5.Data bases and data processing 

As mentioned above, all field 

analyti »' dzta are stored in computerized 

data bases. The main data 

bases are : 

- field observations (auger and pit). 

- analytical data 

- land unit descriptions 

The field observations data base contains 

all parameters that were 

measured in the field, for each of the 

observations sites. Described and 

stored are site number, location, 

slope, vegetation/landuse and all soil 

properties that are measured in the 

field, such as structure, porosity, 

teksture, colour etc (see Technical 

Report No 5, Version 1.1 -Balsem et 

al., 1988). 

The analytical data base contains all 

results of chemical, physical and 

mineralogical analyses and all 

properties used for fertility appraisal 

or classification, that are 

calculated with these analyses (see 

Technical Report Nó 7 - Buurman, 1988; 

and Technical Report No 17 - Muslihat 

et al., 1989). 

The land unit description data base 

contains the general description of 

each mapping unit for the whole island 

of Sumatra, catalogued by mapsheet.

sr 

6°00' 

GAMBAR 1 : LOKASI FETA DAN BATAS ADHINI STRAS I 

FIGURE I : LOCATION AND ADMINISTRATIVE BOUNDARIES 

Jalan 

Jalan kereta api 

Sungai/Anak Sungai 

Kota/Pemuk iman 

Batas Kabupaten 

Batas Propinsi 

1 : 1000 000 

10 20 30 

106°00' 

r 

106°30' 

I. Propinsi Lampung 

A : Kabupaten Lampung Selatan. 

B : Kabupaten Lampung Tengah. 

C : Kodya Bandar Lampung 

II. Propinsi Jawa Barat 

A : Kabupaten Serang.

6°00' 

GAMBAR 2 : RELAIBILITAS PETA 

FIGURE 2 : MAP RELIABILITY 

Jalan 

Jalan kereta api 

Sungai/Anak Sungai 

Kota/Pemukiman 

1 : 1000 000 

10 20 30 

106°00' 106°30' 

L A U T J A W A 

TINGKAT RELAIBILITAS 

Tinggi 

•V'.2".*» bedang 

Rendah

Uraian u m u m berasal dari 

penyederhanaan semua pengamatan pada 

seluruh satuan peta, termasuk analisis 

laboratorium dari profil yang lain. 

Parameter yang disimpan berisi s e mua 

informasi yang diperlukan untuk 

penilaian evaluasi lahan (lihat 

Laporan Teknis No 13a -Balsem & Buurman, 

1989). Uraian satuan lahan dari 

semua satuan peta yang terdapat dalam 

lembar peta ini disajikan pada Lampiran 

1. 

2.6.Relaibilitas peta 

Relaibilitas dari peta tergantung pada 

beberapa faktor seperti: kerapatan 

pengamatan, keragaman tanah, kualitas 

dari citra penginderaan jauh, lokasi 

dari titik pengamatan atau daerah 

kunci, ketepatan dari batas tanah 

maupun batas satuan lahan, tingkat 

pengetahuan dan pengalaman surveyor. 

Tidak semua dari faktor faktor ini 

dapat diukur dan karena itu harus 

diperkirakan. 

Berdasarkan faktor faktor tersebut 

diatas, terutama kerapatan pengamatan, 

maka diperkirakan mengenai relaibilitas 

peta, dan untuk itu dibagi 

menjadi 3 grup (Gambar 2). 

1110 - 9 

The general description is derived by 

generalizing information of all observations 

within the mapping unit, including 

laboratory analyses of 

separate profiles. The parameters 

stored contain all the information 

necessary for land evaluation procedures 

(see SDBH Technical Report No. 

13, - Balsem & Buurman, 1989). The 

land unit descriptions of all mapping 

units relevant to the present sheet 

are listed in Appendix 1. 

2.6. Map reliability 

The reliability of a map depends on 

many such factors as observation density, 

soil homogeneity or complexity, 

quality of the remote sensing imagery, 

the location of sample/key areas, accuracy 

of soil units and soil boundaries, 

the level of education and the 

amount of experience of the soil surveyor. 

Not all of these can be 

measured and so they have to be estimated. 

Based on the above factors, but mainly 

on observation density, three classes 

of map reliability have been established 

(Figure 2).

3. LOKASI DAERAH PETA DAN SUMBER 

INFORMASI 

3.1.Lokasi dan Bâtas Administras! 

Secara geografik daerah peta Tanjungkaç'ang 

(1110) ( terletak antara 

105°00 dan 106°30 Bujur Timur dan 

antara 

Selatan. 

5°00' dan 6°00' Lintang 

Secara adminitratif daerah peta termasuk 

Propinsi Lampung yang meliputi 

Kabupaten Lairmiin

GAMBAR 3 : INDEKS PETA TOPOGRAFI DAN JALUR TERÜANG POTRET UDARA 

FIGURE 3 : INDEX OF TOPOGRAPHIC HAPS AND FLIGHT LINES OF AERIAL PHOTOGRAPHY 

105°00' 15' 30' 45' 106°00' 

5°00' 

6°00' 

JJ 

OÏ 

M 

S 

œ 

77 

R62/8282 

61-77 

: Nomor jalur terbang 

: Nomor foto udara 

(54) 

f54) : Nomer lemrjai 

peta topografi 1 : 50 000 

106°30'

105°00' 

5°00' 

6°00' 

GAMBAR 4 : INDEKS CITRA RADAR STAR-I DAN LANDSAT 

FIGURE

GAHBAR 5 : INDERS LAPORAN SURVEI DAN PEMETAAN TANAH 

FIGURE 5 : INDEX OF SOIL SURVEY REPORTS 

105°D0 1O6°0O' 106°30' 

Toboali - Kesuji 

Pusat Penelitian Tanah, 1986 

Pusat Penelitian Tanah, 1981 

Propinsi Iêpung 

Lenbaga Penelitian 

Tanah, 1%S 

LAUT J A W A 

DAS Sekanpung Atas 

Leibaga Penelitian Tanah, 1971 

'î "^ Seka«pung Bavah 

&A Letóaqa Penelitian Tanah, 1972 

«s»

GAMBAH 6 : PKTA GEOLOGI SAGAN 

FIGURE 6 : GEOLOGICAL SKETCH HAP 

105 Off BT 

Kuarier 

LAUT J A W A 

Pratersier 

Sedlmen cut PTw 

Sumbar : GeologfelembarTeniung Karang. Geological Research and Development Centre, 1978 

106 30' ET 

6 00' LS 

0 5 10 16 Km

6°00' 

GAMBAR 7 : GRUP FISIOCRAFI LEMBAR TANJUNGKARANG 

FIGURE 7 : PHYSIOGRAPHIC GROUPS OF THE TANJUNGKARANG SHEET 

0 106°30 

Grup M\i\i\a\iAlluviat Group 

Grup Mann/Manne Group 

Grup Dataran Tuf Masam / Acid Tuff Plain Group 

Grup Dararan/PlainGroup 

Grup Volkan/Volcanic Group 

Grup Perhukitan/W/y/y Group 

Grup Pctjununqan/Mountain Group 

Grup Aneka Bentuk / Miscellaneous Group

Tersier 

Dari batuan Tersier, batuan yang mempunyai 

penyebaran luas hanyalah dasi t 

dan liparit forraasi Tmda (ïerriary 

-middle - da cite) dan ba tuan volkan an - 

desit tua formasi Tov (Tertiaryolder-volcanics). 

Bat uan-batuan ini 

teiah mengalarai perubahan hidroterraal 

dan deformasi tektonik. Batuan Tov 

umumnya berkoraposisi andesitik. 

Batuan-batuan Tersier non-volkan sangat 

jarang dijumpai pada lembar peta 

Endapan Kuarter dapat dibagi dalam empat 

grup utama : 

(a) Tuf Lanipung (Qlv) 

(b) Basal Sukadana (Qb) 

(c) Batuan andesit muda (Qhv) 

(d) Endapan aluvial dan marin (Qal) 

a. Tuf Lampung vang menutupi bagian 

terluas di timur dan utara lembar peta 

ini raerupakan endapan ignimbrit yang 

sebagian besar diendapkan dalam 

1ingkungan marin dan setempat-setempat 

secara er at bercampur dengan endapan 

marin halus. Tuf raempunyai komposisi 

da s i t i k sampa i liparitik dengan kada r 

t inggi gelas dan batuapung. Karena 

diduga pusat erupsi berada di Teluk 

Lampung, maka keadaan tuf dari endapan 

berangsur berkurang kearah utara. 

b. Basal Sukadana membentuk jalur 

lebar (lebar Ik. 25 km) dengan arah 

tenggara-baratlaut di bagian timur 

lembar peta ini. 

Basal ini mempunyai umur hainpir same 

dengan Tuf Lampung. Batuan ini 

sebagian besar basai olivin. Fade 

pi a to basal terdapat sejumlah krucut 

sinder kecil-kecil aan muds. 

c. Sebagian besar batuan volkan andesitik 

muda termasuk dalam tiga pusat 

erupsi utaina : Vol kan Ra iai , Betung 

dan Rajabcsa. 

Beberapa pusat erupsi rua dan kecil 

juga dit emukan. misalnya di bagiar 

barat1aur 1embar peta in: Serempatsetempat 

bahat: volkar muds merupakan 

lapisan penutup tipis di atas batuan 

tua seperti Tuf Lampung. misalnya di 

baratlauï; kompleks Ra jabasa . 

1110 - lfa 

d. Aluvium marin dan sungai dijumpai di 

sepanjang sungai-sungai utama dan pantai. 

Cekungan aluvial utama adalah 

sungai Sekampung (Rawa Sragi ) . 

Pantai- timur sebagian besar terdiri 

dari dataran pasang surut dan kompleks 

beting pantai; beting-beting pasir dan 

beting-beting karang kecil ditemukan 

sepanjang pantai di barat dan selatan 

Tanjungkarang. 

Te ra s sungai seterapat-setempat dijumpai 

di atas Tuf Lampung, te tapi 

teras-te ras ini bel um dikemukakan 

dalam peta eeoloei vanc arin ceL-ai-atin 

4.2 Fisiografi 

Lembar peta Tanjungkarang dapat dibagi 

dalam tujuh grup fisiografi utama: 

grup Pegunungan, Perbukitan, Volkan, 

Dataran, Dataran Tuf Masam, Marin. 

Aluvial dan Aneka Bentuk. (Gainbar 7). 

Pegunungan 

Bentang a lam yang terraasuk dalam grup 

ini terdapat di bagian sudut baratdaya 

lembar peta ini dan sedikit terdapat 

di timurlaut Tanjungkarang- Pegunungan 

ini termasuk daiam punggung/blok 

lipatan (block faulted) Pegunungan 

Barisan. namun karena terdapat di 

bagian ujung rangkaian pegunungan, 

maka kurang terpengaruh deformasi. 

Pegunungan ini sebagian besar terdiri 

dari batuan volkan tua (basal, andesit, 

dasit) Sub grup yang dijumpai 

adalah: 

M*.2.2: Pegunungan berlereng curam 

sampai sangar curam 

M*.2.3; Pegunungan beriereng sangat 

curam sekali 

Tingkat torehannya berkisar antara 

sangat tertoreh sampai sangat tertoret 

sekali (kelas 3 dan 4). 

Perbuki tan 

Bt-ntang alair vanj., t ermasuk dalanï grup 

perbuki tan berdampingan pada si si 

pegunungan Perbedaan utaraa terdapat 

dalau! arapl ltudonya dimana perbukitan 

lebih kecii l

esar terbentuk dari bahan yang sama 

dengan pegunungan, tetapi beberapa 

perbukitan terdapat pada batuan 

Intrusif (granit) dan batuan metamorfik 

(skis, gneis)..Subgrup yang dijumpai 

adalah: 

H*:l. 2 : Perbukitan dengan pola random 

dan lereng cukup curam 

H*.l. 3:Perbukitan dengan pola random 

. dan lereng curam 

H*.1.5:Lahan bergelomang dengan bukitbukit 

kecil 

H*.1.6:Bukit-bukit kecil berpola 

wilayah bergelombang. 

H*.4.4: Pelembahan tektonik 

Semua satuan ini mempunyai tingkat 

torehan agak tertoreh hingga sangat 

tertoreh sekali. 

Grup Volkan 

Grup ini dibagi lebih lanjut dalam dua 

subgrup: Kerucut Volkan dan bagianbagiannya 

(V*.1) dan dataran volkan, 

plato serta volkan tua tererosi 

(V*.2). 

Dua kompleks volkan utama: Rajabasa 

dan Ratai/Betung tergolong dalam grup 

V*.l; plato Sukadana dan dataran 

volkanik kecil di perbatasan barat 

lembar peta ini termasuk dalam grup 

V*.2. Kerucut volkan terutama dibagi 

lebih lanjut menurut keadaan 

lerengnya, sedangkan satuan-satuan 

volkan lainnya dibagi menurut morfologi 

umum. Sub grup yang dijumpai 

dalam lembar peta ini adalah: 

V*.1.2 :Lereng atas volkan (>30%) 

V*.1.3 :Lereng tengah volkan (16-50%) 

V*.1.4 :Lereng bawah volkan (

sampai bergelombang 

I*.5: Dataran tuf masam bergelombang 

I*.8: Dataran tuf masam bergelombang 

• dengan bukit-bukit kecil. 

S e mua satuan ini dibagi lebih lanjut 

menurut tingkat torehannya. 

Marin 

Grup ini meliputi jalur sempit sepanjang 

pantai timur dan luasan-luasan 

kecil sepanjang pantai selatan. Di 

timur, jalur sempit yang terdiri dari 

beting pantai dan cekungan antar 

beting pantai dipi s^Vikar. n^ri jcl-r 

pantai sekarang oleh dataran mangrove 

dan rawa belakang pantai bervegetasi 

rendah. Dataran lumpur estuarin (nipah 

dan vegetasi campuran) terdapat sepanjang 

beberapa sungai. Jalur beting 

pantai dan cekungannya berbatasan 

dengan lahan atasnya, namun kerapkali 

terpisah dari lahan ini dengan rawa 

belakang payau -bervegetasi hutan rawa 

campuran. 

Di pantai selatan dataran lumpur tidak 

dijumpai dan disini grup ini dicirikan 

oleh dataran pantai dan karang yang 

sempit. Subgrup berikut ini dijumpai 

pada lembar peta ini: 

Bfq.1.1:Kompleks beting pantai dan 

cekungan antar beting 

Bfq.1.2 :Kompleks beting pantai 

tererosi dan cekungannya 

Bf .4.3:Dataran pasang surut bervegetasi 

bakau 

Bf.4.4 :Dataran estuarin 

Bf.5.1 :Rawa belakang dipengaruhi air 

asin bervegetasi rumput-rumputan 

Bf.5.2:Rawa belakang dipengaruhi air 

asin bervegetasi hutan campuran 

Bcq.7 : Endapan marin tak dibedakan 

Aluvial 

Grup ini dicirikan oleh endapan sungai, 

endapan di lembah tertutup, endapan 

sungai melebar (braided) dan endapan 

kipas. 

Yang luas penyebarannya adalah endapan 

sungai Sekampung, yang membentuk 

dataran aluvial luas dengan rawa-rawa 

yang menjulur di bagian tenggara lembar 

peta ini. Rawa-rawa ini terbentuk 

1110 - 18 

di belakang garis pantai dan mungkin 

disebabkan oleh gradien sungai yang 

rendah dan pembendungan sungai-sungai 

oleh deposit marin. Endapan volkan 

menyebabkan terbentuknya beberapa 

cekungan tertutup, yang dijumpai di 

perbatasan barat lembar peta dan di 

plato Sukadana. Kipas tersebar luas di 

daerah bergunung dan berbukit di barat 

daya peta. Subgrup yang dijumpai 

adalah: 

Au.1.1.1 :Rawa dari dataran aluvial 

luas 

Af . 1. 2.1 :Jalur meander dari lembah 

aiuvial luas 

Au.1.3: Pelembahan sempit (erosif) di 

daerah upland 

Au.2.2: Kipas aluvial dan koluvial 

Au.3.2: Cekungan/lembah tertutup 

Aq.5 : Dataran banjir sungai melebar 

Aneka Bentuk 

Di daerah bergunung terdapat lembahlembah 

sungai yang terjal (X.1). Disebélah 

tenggara Sukadana dijumpai 

danau (X3) 

4.3. Hidrologi 

Daerah lembar peta Tanjungkarang mempunyai 

ketinggian antara Om (pantai) 

sampai 1.700m dpi (Gunung Ratai). 

Topografinya menurun ke arah timur 

membentuk dataran/ dataran rendah yang 

diselingi daerah plato dari basai 

Sukadana. 

Sungai-sungai utama di daerah ini a.l. 

Way Sekampung, W.Kambas, W.Penet yang 

bermuara di Laut Jawa dan beberapa 

sungai kecil yang mengalir ke arah 

utara. 

W.Sekampung merupakan sungai terbesar 

dan terpanjang, berasal dari mata air 

di sekitar volkan Ratai dan Betung. 

Sungai ini mula-mula mengalir ke arah 

timur/timurlaut. Plato basai Sukadana 

menyebabkan aliran sungai ini terbendung 

dan alirannya beralih ke arah 

tenggara. Akibat pembendungan ini terbentuk 

daerah-daerah banjir dan rawa 

yang luas seperti rawa Selapan, rawa 

Keramat/Subud dan rawa Sragi. 

Bentukan morfologi, jenis batuan,

proses-proses geomorfik serta keadaan 

tata air di daerah int sangat menentukan 

keadaan pola drainasenya. 

Daerah pegunungan dan perbukitan yang 

pada umumnya mempunyai gradient yang 

cukup besar membentuk pola drainase 

dendritik, sedang di daerah dimana 

proses tektonik nyata mempunyai pola 

drainase rectangular (structural 

control). 

Daerah volkan dengan bentukan-bentukan 

kerucut yang masih utuh membentuk pola 

radial di daerah puncak dan lereng 

atas, sedang di lereng- tengah dan 

bawah paralel atau sub-paralel. 

Basai Sukadana yang banyak mempunyai 

rekahan dan dengan sifat tanahnya yang 

porous, mempunyai drainase internai 

sangat baik yang banyak menghasilkan 

mata air di kaki sekeliling plato 

(spring). Danau Jepara di utara plato 

diduga merupakan bekas kawah yang 

telah mati, membentuk danau yang merupakan 

sumber air utama di daerah 

ini. 

Daerah tuf Lampung umuimya mempunyai 

pola drainase dendritik sedang 

sesetempat dimana dijumpai bentukan 

lahan yang memanjang dijumpai pola 

drainase paralel. 

W. Sekampung yang mempunyai pola 

aliran meandering, di dataran rendah 

membentuk dataran banjir/rawa yang 

cukup luas dengan pola drainase tidak 

nyata (sesetempat meandering). Rawa 

Sragi merupakan daerah rawa terluas 

yang sedang direklamasi guna dijadikan 

areal pertanian. 

5. SATUAN LAHAN 

5.1. Satuan lahan dan tanah. 

Secara garis besar satuan lahan lembar 

peta Tanjungkarang (1110) dapat 

dikelompokkan kedalam 8 (delapan) grup 

yaitu: Grup Aluvial (A), Marin (B), 

Dataran Tuf Masam (I), Dataran (P), 

Volkan (V), Perbukitan (H), Pegunungan 

dan Plato (M) serta Aneka Bentuk 

(Gambar 7). Pada setiap satuan lahan 

umunya diketemukan lebih dari satu 

satuan tanah (pada tingkat Great 

Group), dan agar memudahkan pembacaannya 

maka setiap satuan tanah yang 

1110 - 19 

dijumpai pada setiap satuan lahan 

ditentukan luas penyebarannya secara 

kwalitatif, yaitu: 

- Sangat dominan: apabila penyebarannya 

>75% dari luasan satuan lahan. 

- Dominan: apabila penyebarannya antara 

50-75% dari luasan satuan 

lahan. 

- Cukup: apabila penyebarannya antara 

25-50% dari luasan satuan lahan. 

- Sedikit: apabila penyebarannya 10- 

25% dari luasan satuan lahan. 

- Sedikit sekall: apabila penyebarannya 

nya berasosiasi dengan lingkungan 

air/basah, antara lain Tropaquepts 

(telah berkembang), Fluvaquents dan 

Hydraquents (belum berkembang), serta 

Tropohemists yang merupakan tanah organik 

di daerah berawa. Didaerah 

tanggul sepanjang sungai atau 

peralihan ke dataran dijumpai jenis 

tanah Dystropepts/Eutropepts berpenampang 

dalam, bertekstur halus sampai 

sedang, drainase baik. 

Tanah berpenampang dalara dengan 

tekstur bervariasi dari halus sampai 

kasar, kadang-kadang berlapis-lapis . 

Drainase pada umumnva rortumi.;; ca.-pai 

sangat terhambat. Tingkat kesuburan 

tanahnya sangat tergantung pada bahan 

di daerah sekitarnya dan daerah dari 

mana bahan itu berasal. Umumnya unsur 

hara di daerah ini sedang sampai 

sangat rendah, diraana lapisan atas 

lebih baik daripada lapisan bawah. 

Dengan pengendalian air yang baik 

terutama untuk daerah rendah di tiraur 

lembar peta daerahnya mempunyai 

potensi yang besar sebagai daerah persawahan, 

seperti halnya daerah rawa 

Sragi di sekitar aliran W.Sekampung 

yang telah direklamasi. Penghambat 

utama adalah genangan air permanen, 

banjir dan kandungan unsur hara. 

Grup Marin (B) 

Merupakan dataran rendah yang memanjang 

dari utara ke selatan sepanjang/ 

sejajar pantai timur lembar peta yang 

sebagain besar daerahnya dipengaruhi 

pasang surut. Terletak pada ketinggian 

O-25m dpi., berupa dataran pasang 

surut berlumpur yang diselingi oleh 

beting-beting pasir pantai (beach 

ridges') dan cekungan-cekungan antar 

beting (swales). Bentuk wilayahnya 

datar, datar agak cekung, sedang 

beting pasir pantai umumnya datar agak 

cembung dengan lereng 0-3% . Meliputi 

luas 45.070 ha (6.30%). 

Vegetasi dan penggunaan lahan utamanya 

berupa hutan mangrove, rawa pasang 

surut, sawah, kebun kelapa, tambak dan 

daerah pemukiman. 

Jenis tanah utama di daerah ini adalah 

Hydraquents, Sulfaquents dan Fluv- 

1110 - 20 

aquents yang merupakan tanah-tanah 

belum berkembang di daerah cekungan 

sepanjang pantai yang selalu tergenang 

air. Sulfaquents merupakan jenis tanah 

yang mengandung sulfat tinggi yang 

bila muncul di permukaan dalam jumlah 

di atas ambang toleransi tanaman akan 

sangat membahayakan. Ketiga jenis 

tanah ini berpenampang dalam, tekstur 

umumnya halus bercampur bahan organik, 

drainase sangat terhambat, hampir 

sepanjang tahun daerahnya tergenang 

Di daerah pasir pantai muda di iumpai 

Tj-upoyùaiiuueni:s, yang merupakan tanah 

belum berkembang, bertekstur kasar/ 

pasir, drainase cepat. Tropohumods dan 

Tropaquods merupakan tanah yang telah 

berkembang, dijumpai di daerah beting 

pasir pantai tua yang terletak lebih 

kepedalaman. Daerah ini terutama 

sepanjang pantai berpotensi baik 

sebagai daerah tambak, tanpa melupakan 

kelestarian alam antara lain perlunya 

hutan mangrove sebagai buffer zone 

disepanjang pantai. Beting pasir pantai 

cocok untuk perkebunan kelapa 

sedang pelembahan antar beting untuk 

persawahan dengan jenis padi yang 

lebih toleran terhadap air asin. 

Penghambat utama berupa genangan air/ 

banjir, tanah sulfat masam (cat clay), 

tekstur kasar di daerah beting pasir 

serta unsur hara tanaman (kesuburan 

tanah) yang rendah. 

Grup Dataran Tuf Masam 

Merupakan daerah terluas yang menyebar 

dari arah tenggara-baratdaya terutama 

di baglan tengah dan utara lembar 

peta. Bentuk wilayahnya datar, berombak 

sampai bergelombang dengan diselingi 

oleh cekungan-cekungan. Bahan 

pembentuknya berupa tuf masam bersusunan 

dasit/ignimbrit sebagai hasil 

aktivitas volkan. Aliran abu masam ini 

sangat tebal dan luas mencapai >1000 

km . Tuf masam ini membentukkan 

dataran rendah di pantai tiraur. Terletak 

pada ketinggian 10-100m dpi. 

dengan variasi lereng 0-25% . Meliputi 

luas 288.130 ha (40,15%). 

Vegetasi dan penggunaan lahannya

adaiah pertanian lahan kering (ladang 

dan tegalan), persawahan, kebun campuran, 

kebun karet, semak belukar dan 

padang alang-alang. 

Jenis tanah utamanya antara lain 

Kanhapludults dan Dystropepts, berpenampang 

sedang sampai dalam, tekstur 

umumnya halus, drainase baik. 

Kesuburan tanahnya rendah sampai 

sangat rendah demikian pula kandungan 

bahan organiknya. Dystropepts mempunyai 

kandungan hara yang relatif 

leblh baik. Sebagian besar jenis tanah 

Kanhapludults mempunyai sifat fisik 

yang jelek disebabkan banyak terdapatnya 

lapisan kedap air (lapisan dengan 

kandungan kongkresi besi dan mangan 

tinggi). 

Di lain pihak adanya lapisan kedap air 

ini mempunyai dampak positif untuk 

daerah persawahan karena tidak membutuhkan 

air terlalu banyak disamping 

dapat menyimpan air. Di cekungan 

cekungan dan pelembahan (dataran rendah) 

dijumpai jenis tanah Tropaquepts, 

berpenampang sedang, tekstur halus, 

drainase terhambat. Dengan pengendalian 

air yang baik (perbaikan dan 

pengàturan air) daerahnya berpotensi 

baik untuk persawahan, sedang daerah 

berombak sampai bergelombang untuk 

pengembangan perkebunan terutama 

kelapa sawit dan karet dan pertanian 

lahan kering. 

Penghambat utama antara lain kandungan 

hara tanaman rendah (miskin), fisik 

tanah jelek dàn kekurangan air di 

daerah bergelombang. 

Grup Dataran 

Dataran ini merupakan daerah peralihan 

antara dataran tuf masam dan daerah 

perbukitan/pegunungan. Bahan pembentuknya 

berupa batuan intrusi masam 

terutama granit dan batuan metamorfik 

(skis). Penyebarannya terutama di 

sebelah timur Bandar Lampung dan di 

sebelah barat Natar dengan bentuk 

wilayah berombak sampai bergelombang 

dengan bukit-bukit kecil. Terletak 

pada ketinggian antara 50-125m dpi., 

dengan variasi lereng antara 3-25%, 

meliputi luas 49.075 ha (6,85%). 

1110 - 21 

Jenis tanah utama yang dijumpai di 

daerah ini adalah Kanhapludults, 

Dystropepts, Hapludults dan Tropaquepts 

. 

Kanhapludults dan Hapludults menempati 

lereng tengah atau punggungan, berpenampang 

dalam, tekstur bervariasi 

dari halus sampai sedang. Di lereng 

atas dan daerah berbukit kecil dijumpai 

Dystropepts, berpenampang dalam, 

tekstur bervariasi dari halus sampai 

kasar, drainase baik. Tropaquepts 

dijumpai di daerah pelembahan/cekungan, 

berpenampang sedang sampai dalam, 

tekstur bervariasi, drainase terhambat 

. Kandungan unsur hara tanaman 

(kesuburan) dari tanah-tanah tersebut 

umunya rendah sampai sangat rendah, 

kandungan bahan organik juga rendah. 

Kecuali daerah pelembahan/cekungan, 

daerah ini tidak cocok untuk persawahan. 

Tanaman pertanian lahan 

kering dapat dikembangkan di daerah 

berombak, berombak agak bergelombang, 

sedang perbukitan kecil hendaknya 

dihutankan untuk menjaga kondisi air 

di daerah bawahnya. Penghambat utama 

antara lain hara tanaman yang rendah 

keadaan topografi/erosi di daerah bergelombang 

agak berbukit. 

Grup Volkan (V) 

Grup volkan dapat dibagi menjadi subgrup 

volkan muda dan subgrup basal 

Sukadana. Grup volkan muda terdiri 

dari stratovolkan Rajabasa, Betung dan 

Ratai menyebar di bagian selatan lembar 

peta. Puncak-puncak pegunungan 

tersebut terletak pada ketinggian 

1.282m (Rajabasa), 1.300m (Betung) dan 

1.681m dpi. (Ratai). Lereng atas dan 

tengah telah mengalami pengikisan Ianjut, 

berlereng curam sampai sangat 

curam dengan lereng >30%, sedang 

lereng bawahnya berlereng

lahan kering, semak belukar dan persawahan. 

Jenis tanah utama di lereng atas dan 

tengah terutama Dystrandepts , Dystropepts 

dan Troporthent yang 

merupakan tanah-tanah muda. Sedang di 

lereng bawah dijumpai Dystropepts dan 

Humitropepts dengan kandungan bahan 

organik tinggi. Jenis-jenis tanah tersebut 

berpenarapang dalara, tekstur 

halus sampai agak kasar di lereng 

atas, agak halus sampai halus di 

lereng tengah dan bawah dengan 

drainase baik. Di lereng bawah banyak 

dijumpai batuan besar (h.iHOr\ y-r.~ 

berasal dari lereng atas/tengah. 

Kesuburan tanahnya sedang sampai 

tinggi di daerah dataran rendah sampai 

sangat rendah. Diperkirakan adanya 

tutupan bahan lain di daerah ini. 

Dengan memperhatikan tindakan konservasi 

tanah, lereng-lereng bawah berpotensi 

sebagai pengembangan 

perkebunan kopi, lada, cengkeh dan 

pertanian lahan kering sedang di 

daerah dataran untuk persawahan. 

Lereng atas dan tengah hendaknya tetap 

sebagai hutan 1indung/hutan tutupan. 

Penghambat utama adalah lereng, erosi 

dan batuan besar di lereng tengah dan 

bawah. 

Plato basal Sukadana terdapat di 

sebelah timur lembar peta, menyembul 

di atas dataran tuf masam dengan bentuk 

wilayah berombak-bergelombang, 

berlereng melandai, terdapat pada 

ketinggian antara 50-100m dpi. 

Puncak-puncaknya yang berupa kerucutkerucut 

volkan (cindercone) dan leher 

volkan (volcanic neck) mencapai 

ketinggian 250m dpi. Meliputi luas 

106.420 ha (14,80%). Daerah transisi 

ke dataran berupa lereng terjal yang 

merupakan batas antara lapisan atas 

lava basal yang porous dan lapisan tuf 

masam yang kedap air, dimana terdapat 

banyak mata air. 

Jenis tanah utama adalah Hapludalfs, 

Eutropepts dan Humitropepts berpenampang 

dalam, tekstur agak halus sampai 

halus, drainase baik, kandungan unsur 

1110 - 22 

haranya sedang sampai tinggi dengan 

kandungan bahan organik rendah sampai 

sedang. Di beberapa tempat di bagian 

selatan terdapat hamparan lava di permukaan 

dengan lapisan tanah yang tipis 

dari jenis Troporthents. 

Daerahnya mempunyai potensi yang 

tinggi terutama untuk perkebunan kopi, 

cengkeh dan lada serta pertanian lahan 

kering/tegalan. Sedang daerah perbukitannya 

hendaknya dipertahankan 

sebagai hutan lindung. Kecuali batu 

dipermukaan daerah ini hampir tidak 

mempunyai penghambat. Erosi di daerah 

ir.i l.owupii. u-Lüctk iiampaK Karena sifat 

tanahnya yang sangat mudah menyerap 

air/"internal drainage"nya baik. 

Grup Perbukitan (H) 

Daerahnya terbentuk karena aktivitas 

tektonik, terletak di lereng pegunungan 

dan volkan terutama di bagian 

selatan lembar peta. Bahan perabentuknya 

berupa bahan volkan (tuf dan 

batuan andesit), batuan sedlmen, 

batuan plutonik masam (granit) dan 

batuan metamorf, sesetempat ditempati 

oleh bahan tuf masara Lampung. Terletak 

pada ketinggian 15-375m dpi, dengan 

perbedaan tinggi (amplitudo) 16% . Meliputi luas 50.975 ha 

(7.10%). 

Vegetasi dan penggunaan lahannya 

berupa hutan sekunder, kebun karet, 

kelapa, pertanian lahan kering (ladang 

dan tegalan) sedang di pelembahan 

berupa persawahan. 

Di lereng atas perbukitan dijumpai 

jenis tanah Dystropepts, di lereng 

tengah Hapludults dan Kanhapludults, 

sedang di lereng bawah dijumpai 

Humitropepts. 

Tanah umumnya berpenampang dalam, 

tekstur agak halus sampai halus. 

Kesuburan tanahnya rendah sampai 

sedang untuk yang berkembang dari 

bahan volkan, rendah sampai sangat 

rendah untuk yang terbentuk dari bahan 

lainnya.

GAMBAR 8 : SATDAN LAHAN, BLOK DIAGRAM DAN PENAMFANG KELINTANG LEMBAR TANJUNGKARANG 

FIGURE 8 LAND UNITS, BLOCK DIAGRAH AND CROSS SECTION OF THE TANJUNGKARANG SHEET 

T:;::;: 

":'„:: 

JS'ÔA 

•A. t , î 

Su.f«,,.n« 

'Too e's') 

•"•"••" 

...• 

,At.li,l 

1V0.Î.Ï ti 

JUb S.S.2! 

, 8*6.11 IB;I 

r,...,n 

1110 - 23 

„«,111 N«.J,1) i,M.s.ai

Kecuali lereng bavah yang dapat 

digunakan sebagai Lahan pengembangan 

pertanian lahan kering dengan meraperhatian 

konservasi tanah. lereng 

atas dan tengah hendaknya digunakan 

sebagai hutan. Perabatas utaraa berupa 

lereng, erosi dan kekurangan air. 

Grup Pegunungan dan Plato (M) 

Terletak antara ketinggian antara 

500-1.225m dpi, berlereng curam sampai 

sangat curam, dengan lereng >30% . 

Bahan perabentuknya berupa bahan volkan 

Tersier, tetapi keadaan morfologinya 

Lidak iiieinperiinatKan morroiogi volkan 

yang jelas. Terletak di bagian selatan 

daerah peta yang merupakan bagian 

paling selatan dari pegunungan Barisan 

yang membujur sejajar Pulau Sumatera. 

Meliputi luas 39.990 ha (5.55%). 

Vegetasi dan penggunaan lahannya 

berupa hutan lindung, semak belukar. 

Sedang di lereng bawah berupa 

perkebunan kopi, cengkeh, lada dan 

pertanian lahan kering (ladang dan 

tegalan). 

Jenis tanah utamanya adalah 

Dystropepts yang menempati lereng 

atas. Hapludults inenempati lereng 

tengah sedang di lereng bawah ditempati 

Humitropepts dan Eutropepts. 

Tanah berpenarapang dalam, berteks tur 

halus sesetempat di lereng atas bertekstur 

sedang dengan drainase baik. 

Kandungan unsur hara tanainan dari 

tanah-tanah tersebut umumnya rendah 

sampai sangat rendah, sedang di lereng 

bawah dengan lereng

6. DAFTAR PUSTAKA 

Balsem, T., & P. Buurman, 1989. 

Guidelines for Land Unit Description. 

Soil Data Base Management 

Project Technical Report No. 13, 

Version 2. Soil Data Base Management, 

Center for Soil Research, 

Bogor 

Balsem, T., P. Buurman & U. Wood- 

Sichra, 1988. Penggunaan kode komputer 

untuk data lapangan. Proyek 

Pengelolaan Data Base Tanah, Laporan 

Tehnis No. 5a, Versi 1.1. Pusat 

Penelitian Tanah, Bogor 

Buurman, P., 1988. Sifat-sifat kimia, 

fisika, dan mineralogi untuk data 

base tanah. Proyek Pengelolaan Data 

Base Tanah, Laporan Tehnis No. 7a, 

Versi 2.0. Pusat Penelitian Tanah, 

Bogor. 

Buurman, P., T. Balsem & H.G.A. van 

Panhuys, 1988. Klasifikasi satuan 

lahan untuk survey tingkat tinjau 

Sumatera. Proyek Pengelolaan Data 

Base Tanah, Laporan Tehnis No. 3a, 

Versi 1.2. Pusat Penelitian Tanah, 

Bogor. 

Desaunettes, J.R., 1977. Catalogue of 

landforms for Indonesia. FAO/UNDP 

Land Capability Appraisal Project 

Working Paper No. 13, Soil Research 

Institute, Bogor 

FAO/UNESCO, 1977. Guidelines for soil 

description. Rome 

Gallup, D.L., 1981. Proposed coding 

system for pedon data for trial by 

the Center for Soil Research, Bogor. 

AGO/INS/78/006, Manual 3. Bogor 

GRDC (Geological Research.and Development 

Center), 1978. Geologic map of 

the Tanjungkarang quadrangle, 

Sumatra, scale 1:250,000. 

Kips, P.A., D. Djaenudin & Nata 

Suharta, 1981. The land unit approach 

to land resources surveys for 

land use planning, with particular 

ref.erence to the Sekampung 

watershed, Lampung province, 

Sumatra, Indonesia. 

Muslihat, A., U. Wood-Sichra & P. 

Buurman, 1989. Soil sample analysis 

data base - User Manual and Technical 

Manual. Soil Data Base Management 

Project, Technical Report No. 

17, Version 1.0. Center for Soil 

1110 - 25 

Research, Bogor. 

PPPG - see GRDC 

RePPProT (Regional Physical Planning 

Programme for Transmigration), 1985. 

Review of Phase IB results Cenmtral 

Kalimantan. Ministry of Transmigration, 

Jakarta. 

RePPProT (Regional Physical Planning 

Programme for Transmigration), 1988. 

Review of Phase I results Sumatra. 

Ministry of Transmigration, Jakarta. 

SCS (Soil Conservation Service), 1978. 

Pedon coding system for the National 

Cooperative Soil Survey. USDA, 

Washington D.C. 

Soil Survey Staff, 1987. Keys to Soil 

Taxonomy. SMSS (Soil Management Support 

Service) Monograph 6. US Dept. 

of Agriculture. • 

Laporan pemetaan tanah 

(Nomor adalah nomor laporan dalam file 

SUMREP) 

84. Laporan 1 updating peta tanah tinjau 

daerah Tanjungkarang - Mesuji. 

Pusat Penelitian Tanah, 1986. 

86. Survei dan Pemetaan Lahan dengan 

Sistem Land Unit di DAS Sekampung 

untuk tuJuan evaluasi lahan. Pusat 

Penelitian Tanah, 1981. 

184. Survei dasar dalam rangka pembangunan 

pertanian" Lampung. Lembaga 


340. Survei dan Pemetaan Tanah Tinjau 

DAS Sekampung Atas. Lembaga 


341. Survei dan Pemetaan Tanah Tinjau 

DAS Sekampung Bawah. Lembaga 

Penelitian Tanah, 1972.

LAMPIRAN 1. URAIAN SATUAN LAHAN 

APPENDIX 1. LAND UNIT DESCRIPTIONS 

1110 - 26

LAUD nur REPORT LREP-SDHM, CSE-BŒOR 

MF IMAGE: 

1. LAUD OBIT: Au.1.1.1 

4. «»»3IUHM-K by PRuviHUE 

5. STATUS IDENTIFIERS 

6. LARD OHIT DESCBIPTIOH 

7. SATELLITE SCEBES 

8. AERIAL PHOTOGRAPHS 

g. BADAR 

10. PAREBT MATBBTÀI. 

a. Weathering 

b. Litbology 

c. Formation 

12. MATER a. Quality 

13. FISHERIES 

b. Source 

14. RIVERS a. Floodrisk 

b. Inundation 

15. VBSEIATIGH/LAHD USE 

Area used 

16. ACCELERATED EBOSICH 

a. Occnrence 

b. Evidence 

17. SOIL GSEAT OOOP 

Doainant >50I 

Associated 1 

Associated 2 

Lampung: 99% 

CBQ5S SBCXIOH: 

A.2.2.1 

m 

A.I.I .1 

2. MAP SHEET: 1110 3. AREA: 168 km2 

Updated by: DR edit date: 29/05/89 Status: Final 

A.l.2.1 

Marshes of broad alluvial plains with open low vegetation, mixed 

sediments, slopes 0-3%. 

123/64/14/11/84 

1:100.000 62 /8282-071, 62 /8282-065 

Star-I/250/88/1110-2,3 

Slight 

clay, sand, peat 

Qal 

Fresh 

Perennial River,. Shallow wells 

Rawa (swamp) 

High 

Permanent 

11. R0Œ OOTCKOP: X 

, swamp (rawa) including sedges, tidal wetland rice (pasang surut) 

60 X 

None 

32. wy-fuFSiggTATinv. PROFILES: 

Classification 

hydraquents 

fluvaquents 

tropohemists 

eqw/ /341-71 /72/IS/1110/23/ /16 / 

het/ /341-20 /72/SK/1110/23/ /59 / 

1110 - 27 

Z of area 

60 Z 

30 X 

10 X 

Lab. checked 

yes 

yes 

yes 

eqv/ /86-18 /81/SR/1110/44/ /03 /

18. SOIL CHABACTEBISnCS 

Properties 

a. Texture: topsoil 

subsoil 

b. Depth: peatsoil 

mineralsoil 

c. Drainage: 

d. Ezch. K: topsoil 

subsoil 

e. Total K2O: topsoil 

subsoil 

topsoil 

subsoil 

g. Total P: topsoil 

subsoil 

b. CEC pH 7 topsoil 

subsoil 

i. Soil Reaction:topsoil 

subsoil 

j. Al Sat. topsoil 

subsoil 

k. Al toxicity : 

1. Acid sulph. pot.: 

a. Salinity : 

n. Other Toxicity: 

o. Boot obstr. layer : 

p. Organic Matter : 

q. TEB : 

r. Total observations: 

19. ALTITUDE: 

20. PLAH/IKQFILE: 

21. L.D. DBAQUGE: 

22. SLOPE: 

23. SLOPE DISTB.: 

24. BELIEF AMPU.: 

25. TEOTATB- 

26. CREST/BIDGES: 

27. VALLET FLOOR: 

28. LAND FACETS: 

29. FBASffiBTATIOH: 

30. BKI.TAim.TTY: 

10.b : 2 12.a: 2 

18.d-q: 2 19: 2 

31. ADDITIOHAL •DIES: 

Dominant > 501 

fine 

fine 

— 

very deep 

Very poorly drained 

-- 

-low 

medium 

Olsen 

very high 

low 

very high 

low 

-- 

-strong 

acid 

moderately acid 

125 cm 

13.5 

0.0 

1 

Associated 1 

fine 

fine 

— 

extremely deep 


very high 

high 

very low 

-- 

-very 

high 

medium 

very high 

very high 

strong acid 

strong acid 

200 cm 

23.1 

26.5 

3 

Associated 2 

organic 

organic 


-- 

Very poorly dr 

— 

— 

medium 

very low 

Olsen 

very high 

high 

very high 

medium 

— 

— 

slightly acid 

slightly acid 

100 cm 

68.4 

0.0 

1 

15 m 

Dominant: No pronounced highs/lows 

Included: 

5 m 5 m 

a. Pattern: 

b. density: 

c. Variability: 

a. Steepness:flat 

\ 

b. Variability: Low 

c. Length: 

e. Curvature: straight 

ValleybottoBs: 100 Z 

d. Variability: 

Interfluves : 0-8Z.-0 Z, 9-251: 0 Z 25-551: 0 

a. Asciitode: very low 


Flat, slope

LAHD R£PGRT LREP-SDBf, CSR-BOGCR 

1. LAHD OHIT: Af.1.2.1 

«. OyaiHtaCE by FBCWIBCE 

5. STATUS IDEfflFTERS 

6. LAHD «HIT DESCKIFTIOH 

7. SATELLITE 

8. AERIAL EBOTOGKAFB5 

9. PAT1AP 

10. PARERT MATERTAT. 

MAP IMAGE: CSDSS SECTIOH: 

. a. Heathaxins 

b. Litfaolossr 

c. Fomtion 

12. HATER a. Quality 

13. FISHERIES 

b. Source 


IS. VEGETATIOB/LAHD OSE 

16. 

17. SGII> 

32. 

iqt/ 

ity/ 

Area used 

a. Occuxence 

b. Evidence 

Damnant >5OI 

Associated 1 

Associated 2 

A.l.2.2 

tMdtsvaip 

Y/ S\ older subsoil 

A.1.2.1 A.l.2.2 

*Mn*T »ar promit rivw 


Lampung : 992 

Updated by: DR edit date: 29/05/89 ' Status: Final 

Meanderbelts of broad alluvial valleys fine sediments, slopes 

0-3Ï 

123/64/14/11/84 

1:100.000 62 /8282-071, 60 /8295-015, 61 /8344-197 

Star-I/250/88/1110-2,3 

Slight 

clay 

Qal 

Fresh 

Perennial River, Shallow wells 

Rawa (swamp) 

High 

11. ROCK OUTCROP: X 

Seasonal • 

bush, swamp (rawa) including sedges, shifting cultivation, 

rainfed wetland rice, deepwater rice (lebak), rubber (karet) 

50 I 

None 

Classificatie 

tropaquepts 

fluvaquents 

dystxopepts 

/341-18 /72/SK/1110/44/ /50 / 

/184-05 /68/IS/1110/51/ /60 / 

1110 - 29 

X of area 

55 X 

35 X 

10 X 

Lab. checked 

yes 

yes 

yes 

eqv/, /341-68 /72/IS/1110/23/ /ll /

IS. 

Properties 


subsoil 


mineralsoil 

c. Drainage: 

d. Exch. K: topsoil 

subsoil 

e. Total K2O: toosoil 

subsoil 

£. Avail. F: method 

topsoil 

subsoil 

g. Total F: topsoil 

subsoil 

h. CEC pH 7 topsoil 

subsoil 


subsoil 


subsoil 



m. Salinity : 


o. Root obstr. layer : 


q. TEB : 


19. ALTITUDE: 

20. FIAH/PBOFILE: 

21. L.U. DRAIBâGE: 

22. SLOPE: 

23. SLOPE DISTR.: 

24. RELIEF AMPU.: 

25. TERRAIN: 

26. CREST/RIDGES: 


28. LARD FACETS: 

29. FRAGMENTATION: 

30. RELIABILITY: 

10.b : 2 12.a: 

18.d-q: 1 19: 

31. ADDITIOHAL HOTES: 


moderately fine 


deep 

Poorly drained 

verv hieh 

medium 

Olsen 

very high 

very high 

very high 

very high 

slightly acid 

slightly acid 

100 cm 

1.6 

0.0 

4 

Associated 

fine 

fine 

deep 

Moderately 

very low 

Olsen 

very high 

very low 

high 

medium 

1 

well 

very strong acid 


80 cm 

4.7 

0.0 

1 

60 m Minimum: 5 n 


Included: 

a. Pattern: meandering 

c. Variability: low 


c. Length: 


Valleybottoms: 90 X 

Interfloves : 0-8Z:10 X, 9-2SZ: 0 X, 

a. Amplitude: very low 

Flat, slope

LAHD UHIÏ REPORT 

MAP MAGE: 

1. LAHD IJHIT: Au.1.3 

4. maiKKHKE by PRUNIMUK: 

5. STATUS IDEHTHTERS : 

6. LAHD DUIT DESCBXFnOH: 

7. SATELLITE HCKUKS • : 

8. ABHTAT. FBOTCG8AEBS : 

9. RADAR : .Star-I/250/88/1110-2,6 

10. BAREST MATERIAL 

a. Weathering : 

b. Lithology : clay, sand, 

c- Formation : 

12. NATES a. Quality : 

b. Source : Perennial River 

13. FISHERIES : Rawa (swamp) 

14. RIVERS a. Floodrisk : High 

b. Inundation: 

15. VEGETATICH/LAHD USE : 

Area used : 

16. ACCELERATED EROSION 

a. Occnrence : None 

b. Evidence : 

17. SOIL GREAT GROUP 

REPR 

Donnant >SOZ 

Associated 1 

Associated 2 

1.3.2 

LBEP-SDBM, CSR-BOSOR 

CSOSS SECnGH: 

X.1.3 


Lampung: 99! 

1.2.1 

Updated by: OR edit date: 29/05/89 Status: Final 

Narrow valley bottoms,mixed sediments,slopes 0-3Ï. 

123/64/14/11/84 

1:100.000 62 /8282-75 

Slight 

Qal 

Fresh 

Seasonal 

11. BOCK OOTCBaP: 

, swamp (rawa) including sedges, deepwater rice (lebak) 

30 Ï 


tropaquepts 

fluvaquents 

eutropepts 

iqt/ /341-18 /72/SK/1110/44/ /50 / 

ite/ /341-70 /72/IS/1110/23/ /15 / 

1110 - 31 

X of area 

65 Z 

30 Z 

5 Z 

Lab. checked 

yes 

yes 

yes 

1.4.2

18. SOIL CHARACTERISTICS 

Properties 


subsoil 


mineralsoil 

c. Drainage: 

d. Excb. K: topsoil 

subsoil 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 

i. Soil Reaction: topsoil 

subsoil 


subsoil 



m. Salinity : 




q- TEB : 


19. ALTITUDE: 

20. FLAH/ÎBQFILE: 

21. L.O. DRAIHAGE: 

22. SLOPE: 


24. RELIEF AMPLI.: 

25. TESBAIH: 

26. CfiESTVRlDGtS: 


28. LAHD FACETS: 

29. FRAGMEHTATIGH: 


lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 




-deep 


— 

-- 

medium 

Olsen 

very high 

very high 

very high 

very high 

-- 

-slightly 

acid 

slightly acid 

1.6 

0.0 

0 

Associated 1 

fine 

fine 

Shallow 



low 

low 

medium 

low 

— 

— 

medium 

medium 

strong acid 

strong acid 

0.0 

0.0 

0 

Associated 2 

moderately coarse 


-extremely 

deep 

Well drained 

law 

low 

- - • 

— 

— 

-very 

low 

very low 

-- 

— 

slightly acid 


1.8 

0.0 

1 

40 m Minimum: 10 m Range: 30 m 


Included: 

a. Pattern: 


b. density: 



c. Length: 

e. Curvature: concave 

Valleybottoms: 95 % 


InterCloves : 0-81:5 X, 9-25X: 0 X, 25-55Z: 0 X 

a. Amplitude: very low b. Variability: Low 

Flat, slope

LAHD UIXT REFQBT LREP-S0BM, CSR-BOGOR 

MAP IMAGE: CSOSS SECTIOH: 

1. LAID OBIT: Au.2.2.1 2. MAP SHEET: 1110 3. AREA: 113 km2 

4. UaaiKtWKK by HtUVlKVE: Lampung: 99X 

5. STATUS IDENTIFIERS : Updated by: OR edit date: 29/05/89 Status: Final 

6. LAHD UHXI DESCBIPTIOH: Slightly dissected alluvial and colluvial fans,mixed sediments, 

slopes 3-8X 

7. RATgf-l-ITK sa'WfUfK : 123/64/14/11/84 

8. AERIAL PHOTOGRAPHS : 1:100.000 58 /8292-67 , 58 /8292-6S 

9. RADAR : Star-I/250/88/1110-1,3 

10. BARER! M»Ti«T*T- 11. ROCS OUTCROP: X 

a. Weathering : Slight 

b. Lithology : clay, sand 

c. Formation : Qal 

12. HATER a. Quality : Fresh 

b. Source : Perennial River, Medium wells 

13. FISHERIES : Sungai (river) 

14. RIVERS a. Floodrisk : Low 

^^ • XonnQftbioQ" iiOxiô 

15. VBGETAIIGH/LABD USE : bus'h, alang-alang, shifting cultivation, upland crops, rainfed 

wetland rice, irrigated wetland rice (irigasi), coconut (kelapa) 

Area used : 60 X 

a. Occurence : Localised 

b. Evidence : Various 

17. SOIL 68EAX G8OHP : 

Classification X of area Lsb. checked 

DfÎTwmt >50X eutropepts 70 X yes 

Associated 1 tropaquepts 30 X yes 

Associated 2 X 

32. REPRESENTATIVE PROFILES: 

ite/ / /87/ER/1010/33/ /17 / 

1110 - 33

is. son. 

Properties 


subsoil 


MÏ nnrai «/»i 1 

c. Drainage: 


subsoil 

e. Total S2O: tonsoil 

subsoil 

t. Avail. F: aethod 

topsoil 

subsoil 


subsoil 

h. CEC pB 7 topsoil 

subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FLAB/PROFILE: 

21. L.O. DRAWGE: 

22. SLOPE: 



25. TiynATW- 




29. FRAGMEHTATIOn: 


lO.b : 2 12.a: 2 

18.d-q: 2 19: 2 

Damnant > 501 

medium 

medium 

-very 

deep 

Well drained 

medium 

low 

mpHi im 

low 

Bray I 

very high 

low 

low 

very low 

high 

very high 


strong acid 

very low 

low 

— 

-- 

— 

-- 

102 cm 

3.8 

94.4 

0 

Associated 1 

coarse 


— 

very deep 


-- 

— 

1 

very low 

-- 

-low 

very low 

medium 

medium 

strong acid 


— 

-- 

— 

— 

— . 

-- 

— 

0.0 

0.0 

0 

Associated 2 

0.0 

0.0 

0 

100 m Minimum: s m Range: 40 m 

Dominant: linear and random > 60Z of area flat-topped 

Included: 

a. Pattern: distributary 

c. Variability: medium 

b. density: Low 

a. Steepness:gently sloping b. Variability: Low 

c. Length: moderate 


ValleybottOBs: 20 X 

Interfluves : 0-81:80 X 

a. A^plitode: very low 

Undulating 2- 8Ï, 0-50 m 

a. Shape: no crests 

d. Width: 

a. Width: 

9-25X: 0 

b. Length: 

e. Variability: 

b. Variability: 

-1- Fan head & mid fans, eutropepts, 70Ï 

-2- Toe & valley bottoms, tropaquepts, 30% 

-3- 

-4- 

Valleys: Small blocks Interduves: Medium blocks 

1= reliable, 2° probable, 3= tenable, 

14.a: 1 14.b: 1 17: 2 18.a: 2 

22: 2 23: 2 24: 2 28: 3 

d. Variability: Medium 

X, 25-55X: 0 X 


4= plausible 

18.b: 2 18.c: 

29: 2 


31. ADDITIORAL HOTES: Tropaquepts extrapolation based on RePPProt Land System KNJ.Repres 

entative profiles for Eutropepts is extrapolated from other LU. 

1110 - 34

LAHD UHIT REPORT LREP-SDBH, CSR-BOGOR 

1. 

4. 

5. 

e. 

7. 

8. 

9. 

10. 

12. 

13. 

14. 

15. 

16. 

17. 

MAP IMAGE: CROSS SECTIG8: 

LAHD UHIT: Au. 3 .2 

niiiukwiJ Ky nxvnrt 

SIAIDS IDjtainritKö 

LABD UHIT DÜÜLXIFIIIJH 

SATELLITE SCEHES 

ABPTAT- PHOTOGRAPHS 

RADAR 

BAREST MATERIAL 

a. Weathering 

b. Lithology 

c. Fonation 

HAIER a. Quality 

b. Source 

FISHERIES 

RIVERS a. Floodrisk 

b. Inundation 

VEGETATIOH/LAHD OSE 

Axea used 

inrnnitTin rgrnjrî 

a. Occurence 

b. Evidence 

SOIL G8EAT GSOOF : 

Dominant >50Z 

Associated 1 

Associated 2 

B.l.3.3 

volcanic rods 

V.2.2.1 

A.3.2 

savais savahs 

swamp 

alluvial sediments 

V.2.2.1 


Lampung: 99X 


Tolcanic rodcs 

V.l.4.2 

Closed basin/depression^mixed sediments, slopes 0-3Ï. 

123/64/14/11/84 

1:100.000 61 /8344-195, 57 /8292-81 , 57 /8292-79 

Star-I/250/88/1110-4 

11. ROCK OUTCH3P: % 

Slight 

clay, sand 

Qal 

Fresh 


Rawa (swamp) 

Low 

Seasonal 

, swamp (rawa) including sedges, rainfed wetland rice, irrigated 

wetland rice (irigasi) 

90 % 

None 


tropaquepts 

eutropepts 

X of area 

80 X 

20 X 

X 

Lab. checked 


iqt/ /340-12 /71/SK/1110/41/ /35a/ ite/ /340-22 /71/DN/1010/ / /60 / 

1110 - 35 

yes • 

yes

18. SOIL CHARACTEKISTICS 

Properties 


subsoil 


mineralsoil 

c. Drainage: 


subsoil 


subsoil 

£. Avail. P: nethod 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PIAH/PHDFILE: 

21. L.D. DBAIHAGE: 

22. SLOPE: 

23. SLOPE DISTE.: 

2«. HFITTO AMPLI.: 

25. TEgPATTB- 

26. 

27. VALLEY FLOCK: 

28. LAID FACETS: 

29. FBAGMEaTATICH: 


lO.b : 2 12.a: 2 

18.d-q: 2 19: 2 

31. ADDITIONAL HOTES: 

Dominant > SOX 


fine 

very deep 

Irrigated 

low 

low 

low 

very low 

medium 

medium 

high 

very high 

slightly acid 

moderately alkaline 

105 cm 

1.3 

31.5 

2 

Associated 1 


fine 

moderately deep 

Well drained 

very high 

high 

verv hieh 

high 

high 

medium 

high 

high 

strong acid 

slightly acid 

65 cm 

1.4 

26.6 

1 

150 m Minium: 100 m 


Included: 

a. Pattern: 



c. Length: 


Valleybottons: 100 X 

Range: 

Associated 2 

0.0 

0.0 

0 

125 m 

b. density: 



Interflnves : 0-81:0 X, 9-25X: 0 X. 25-551: 0 X 

a. «»ym-~»~- very low 


Flat, slope = probable, 3= tenable, 

14.a: 2 14.b: 2 17: 2 18.a: 2 

22: 2 23: 2 24: 2 28: 2 

1110 - 36 

4= plausible 

18.b: 2 18.c: 

29: 2

LAUD QUIT BEEOBT IBEP-SDBM, CSR-BOGGS 

1. LAND DIBIT: Aq.5 

4. OCCUREHCE by PHOVIHCE: 

5. STATUS XDEHTIFIEBS : 

6. LAKD QUIT DESCRIFTICH: 

7. SATELLITE «l^lHmgt : 

8. AERIAL EBOTOGKAPHS : 

9. BADAR : 


MAP IMAGE: CSOSS SECTIOH: 


b. LAthology : 

c. Formation : 

12. WATER a. Quality : 

b. Source : Perennial River, Shallow wells 

13. FISHERIES : 

14. RIVEBS a. Floodrisk : High 

b _ Immdatxan : Seasonal 

15. VEGETATIGH/LAHD USE : 

Area used : 

16. ACCELERATED EBGSIGH 

a. Occurence : 

b. Evidence : 

17. SOU. GBEAT GBCOP 

Dominant >50I 

Associated 1 

Associated 2 

32. REPHESEHTATIWE PROFILES: 


Lampung: 99% 

updated by: DR edit date: 29/05/89 Status: Final 

Fioodplain of braided rivers,coarse sediment,slopes 0-3%. 

123/64/14/11/84 

1:100.000 57 /8292-73 , 58 /8292-67 

Star-I/250/88/1110-3,4 

Slight 

sand 

Fresh 

Sungai (river) 

, bush, upland crops, tea (ten) 

20 % 

None 


tropaquepts 

tropofluvents 

dystropepts 

iqt/ / /87/SR/1010/44/ /44 / 

ity/ / /87/HJ/1010/24/ /46 / 

1110 - 37 

Z of area 

60 % 

30 % 

10 % 

11. ROCK OUTCROP: % 

Lab. checked 

yes 

no 

yes 

evt/ /87/SR/1010/ /43

is. son. CHARACTERISTICS 

Properties 

a. Textare: topsoil 

subsoil 


•Ancrai «"*!1 

c. Drainage: 


subsoil 


subsoil 

£. Avail. F: aethod 

topsoil 

subsoil 

8- Total P: topsoil 

subsoil 

b. CXC pH 7 topsoil 

subsoil 


subsoil 


subsoil 

k. Al taxicity : 

1. Acid salpb. pot.: 

B. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FLAH/ÏROFILE: 

21. L.0. DRAIHAGE: 

22. SLOPE: 

23. SLOPE DISTE. : 


25. TEPBAT». 


27. VALLEY FLOOR: 


29. FRACMEBTATIGH: 

Donnant > SOX 

fine 

fine 

very deep 


low 

very low 

low 

very low 

Bray I 

very low 

very low 

low 

very low 

very high 

very high 



very low 

very low 

120 cm 

3.3 

25.5 

0 

Associated 1 

0.0 

0.0 

0 

Associated 2 


fine 

very deep 

Moderately well 

high 

low 

y,* eu 

medium 

Bray I 

high 

very low 

very high 

medium 

high 

high 

strong acid 


very low 

very low 

120 cm 

2.0 

11.9 

0 

100 m Minisa: 5 m Range: 40 m 

Included: 

a. Pattern: braided 




b. Variability: Medium 

c. Length: short 




Interfloves : 0-81:0 X, 9-251: 0 Z, 25-551: 0 X 

a. Anplitade: low 

Undulating 2- 8Z, 0-50 m 


a. Shape: no crests b. Length: 


d. Width: e. Variability: 

a. Width: 

-1- 

-2- 

-3- 

-4b. 

Variability: 

Valleys: Interflaves: 

30. Hn.TABTT.TTY: 1= reliable, 2= probable, 3= tenable, 4- plausible 

lO.b : 2 12.a: 2 14.a: 2 14.b: 2 17: 2 18.a: 2 18.b: 2 18.c: 2 

lS.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 29: 

31. ADDITIOSAL BOXES: Representative profiles are extrapolated from sheet Kotaagung 

1110 - 38

LARD DHIT REPORT LREP-SDBM, CSR-BOGOR 

MAP IMAGE: CBOSS SECTICH: 

(old) 

1. 1AHD UUT: Bfq.1.1 

4. I113IUHHÜH. Ky PBfWTWTK 

5. STATUS utaaxxjjjfa 

6. LAID DHIT DKaUtLPTllH 

7. SATELLITE Mf-WiiBt 

8. AERIAL FBOTOGSAFBS 

9. BADAR 

10. PARERT M*TCTTÄI- 


13. FISHERIES 

a. Heatharing 

b. Litbology 

c. Foxution 

b. Source 


15. U HJHTATTf /I *T> (JSE 

Area used 

16. »rr-FU3»ATin ynfipT rl H 

a. Occurence 

b. Evidence 

17. SOU« CPBAT GSODP 

Dominant. >SOX 

Associated 1 

Associated 2 

(young) 

B.S B.I.2 B.4.2 

.4» o, J-" 

B.1.1 B 

4.1 

(old, flattened (young) 

eroded) 


Lampung: 99% 


Complex of beach ridges and swales,fine and coarse sediments 

(unripe) 

123/64/14/11/84 

. 1:100.000 

Star_I/250/88/1110-4 

sand, clay 

Qal 

Brackish 

Rain 

Laut (sea) 

Low 

32. BEHiESEKTATIVE PROFILES: 

None 

11. BOCK ODTCSOP: X 

coastal forest on beaches, bush, coconut (kelapa) 

60 I 

None 


tropopsanments 

fluvaquents 

Z of area 

85 Z 

15 I 

X 

Lab. checked 

est/ /341-7 /72/SK/1110/24/ /09 / eqv/ /341-5 /72/SK/1110/24/ /07 / 

1110 - 39 

yes 

yes 

s 

Sea

Properties 

a. Texfcoxe: topsoil 

subsoil 


• SOX 

coarse 

coarse 

— 


Excessively drained 

— 

low 

Olsen 

low 

low 

low 

low 

— 

-neutral 

slightly alkaline 

— 

-- 

— 

-- 

— 

-- 

40 cm 

0.2 

0.0 

1 

Associated 1 

fine 

fine 

-very 

deep 


very high 

very high 

Olsen 

medium 

very low 

low 

very low 

— 

-slightly 

acid 

neutral 

— 

-- 

— 

-- 

— 

-- 

100 cm 

2.6 

0.0 

1 

Associated 2 

0.0 

" 0.0 

0 

5 m Minim»: 1 m Range: 2 m 

Dominant: linear and parallel > 60% of area flat-topped 

Included: 

a. Pattern: parallel b. density: Very 




e. Curvature: convex 

Valleybottoms: 15 I 

InterCLuves : 0-8Z:85 X, 9-251: 0 X, 

a. A^litude: low 

Flat, slope

LABD DHIT BERST L8EP-SDBM, CSB-BOBCR 

MftF IMAGE: CSOSS SECTIGH: 

(old) (young) (old, flattened (young) X' 

eroded) 

1. LAID OBIT: Bfq.1.2 2. MAF SHEET: 1110 3. AREA: 149 km2 

4. OCCŒEBCE by PHUV1BUE: Lampung: 99% 

5. STATUS IDENTIFIERS : Updated by: DR edit date: 29/05/89 Status: Final 

6. LAHD UNIT DESCB1PTIGH: Complex of eroded beach ridges and filled in swales, fine and 

7. SATELLITE SCEBES : 123/64/14/11/84 

8. AERIAL PHDrOGSAPBS : 1:100.000 

coarse sediments (partly ripened) 

9. BADAR .: Star-I/250/88/1110-2,4 

10. BABEHT MATEBTAT. 11. BOX OOICSOP: X 


b. Litbology : clay, sand 


12. HATER a. Quality : Brackish 

b. Source : Rain, Perennial River 

13. FISHERIES : Laut (sea) 

14. RIVERS a. Floodrisk : Low 

b. Inondation: None 

15. VBGEIATIOB/LAHD OSE : coastal forest on beaches, bush, alang-alang, irrigated wetland 

Area used : 60 X 

16. ACCELERATED Fnn^yr» 

rice (irigasi), rainfed wetland rice, coconut (kelapa), towns, 

villages 

a. Occorence : None 

b. Evidence : 

17. SOIL GREAT GBOUP : 

Classification X of area Lab. checked 

Dominant >50I tropopsanments 70 X yes 

Associated 1 tropaquepts 25 % yes 

Associated 2 tropohumods 5 Z yes 

— — — — — — — — — — — — -._ — — — ____ ______ _______ ______ _______________________.-«_ — — — — __ — — — -• — — — _____________ 

32. BERESEnATIVE PROFILES: 

est/ /341-98 /72/IS/1110/51/ /62 / iqt/ /184-6 /68/IS/1110/24/ /63 / 

sht/ /341-4 /72/SK/1110/24/ /06 / 

1110 - 41

18 

Properties 

à. Textaxe: topsoil 

subsoil 


•ïneralsoil 

c. Drainage: 


subsoil 

subsoil 

t. Avail. P: nethod 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 

k. À1 toxicity : 


•. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FLAH/ÎBQFHJE: 

21. L.ü. DRAUttGE: 

22. SLOPE: 


24. RELIEF AMPU.: 

25. TERRAS: 

26. C8EST/RIDSES: 


28. LAUD FACETS: 

29. FRAGMEHIATIGH: 


lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 

31. ADDITIGHAL BOIES: 

Donnant > SOX 

coarse 

coarse 

— 

deep 

Somewhat excessively 

— 

— 

low 

Olsen 

very low 

very low 

low 

very low 

— 

— 

strong acid 

strong acid 

— 

-- 

— 

— 

— 

— 

100 cm 

1.8 

0.0 

3 

Associated 1 

fine 


— 



-- 

nisn 

medium 

X. 9-25Z: 0 

— 

-very 

high 

medium 

— 

— 



— 

-- 

— 

— 

— 

— 

80 cm 

2.1 

0.0 

1 

Associated 2 

coarse 

coarse 

very deep 


low 

very low 

Olsen 

low 

very low 

low 

very low 


strong acid 

110 cm 

1.5 

0.0 

1 

25 m Minium: 5 m Range: 15 m 

Dominant: linear and parallel > 60Z of area flat-topped 

Included: 

a. Pattern: parallel b. density: Very low 






Interflows : 0-81:75 


Flat, slope

LAUD OBIT REPORT 

12. 

13. 

14. 

15. 

16. 

17. 

LREP-SDBf, CSH-BOGCB 

MAP IMAGE: CSOSS SECTICH: 

a. Heatherins 

b. Litfaology 

c. Fora&txon 

HATER a. Quality 

b. Source 

FISHERIES 


b. Immdation 

VEGETATICH/LAHD DSE 

Area used 

ATT-FIVBATFn tq^lKIIW 

a. Occorence 

b. Evidence 

SOIL GREAT GSODF 

B.5.1 X.3 4.5 

B.4.4 B.4.2 B.4.3 B.4.1 Sea 

1. LAUD OBIT: Bf .4.3 


4. 

Lampung: 991 

5. STATUS IDEHIir.LEK2> Updated by: DR edit date: 29/05/89 Status: Final 

6. LAHD UBIT DESCXIPTIGH Tidal flats with mangrove vegetation,fine sediments(unripe). 

7. SATELLITE MMHMHM 123/64/14/11/84 

8. ABBT*T- PHOTOGRAPHS 1:100.000 

9. RADAR 

Star-I/250/88/1110-2,4 

10. PAREBT M»TEBT»T. 

11. BOCK OGTCHaP: % 

Dominant >50I - 

Associated 1 

Associated 2 

32. REPRESEHTATIVE PROFILES: 

clay 

Qal 

Saline 

Rain 

Laut (sea) 

None 

Permanent 

mangrove forest (bakau), swamp (rawa) including sedges, fishponds 

(tambak) 

20 X 

None 


hydraquents 

sulfaquents 

eqw/ /184-8 /68/IS/1110/52/ /67 / 

1110 - 43 

Z of area 

90 X 

10 X 

X 

Lab. checked 

yes 

yes


Properties 


subsoil 


wi VM»i-stl *ni 1 

c. Drainage: 


subsoil 

e. Total K2O: tonsoil 

subsoil 

£. Avail. P: method 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/ÏROTTLE: 

21. L.U. DRAIHAGE: 

22. SLOPE: 

23. SLOPE DISTR. : 


25. TERRAIH: 


27. VALLET FLOCK: 


29. fRAGMEHTATIOB: 


lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 

DoBinant > SOX 


fine 

— 



— 

-- 

1 nu 

low 

— 

— 

medium 

very low 

— 

-strong 

acid 


-- 

-- 

— 

— 

-- 

— 

— 

6.4 

0.0 

0 

Associated 1 

fine 

fine 

very shallow 



very high 

very high 

very high 

medium 

high 

low 

medium 

low 

medium 

slightly acid 

slightly acid 

-- 

-- 

-very 

shallow 

saline 

-- 

— 

0.0 

0.0 

0 

2 m MinixuB: 1 

Drainant: No pronounced highs/lows 

Included: 

a. Pattern: reticular 


a. Sbeepness:flat 

c. Leqgth: short 


Valleybottcms: 100 Z 

Interfluves : 0-8X:0 X. 9-25X: 0 X, 


Flat, slope

LAHD OBIT REPORT LREP-SDHM, CSR-BOGOR 


B.4 .2 

logged lunciroTe 

unjroe 

K 

nlpah 

^ ^ 

B.4.4 

tidal îlly 

nipah 

UKjrove 

B.4.2 

locked unçrovs 

X X A. 

1. LAHD DHIT: Bf.4.4 


4. iMaaiitHMiat by PRCWIBCE: Lampung: 99! 

5. STATUS IDEHTIFIEBS : Updated by: DR edit date: 30/05/89 Status: Final 

6. LAHD DHIT DESCHIPTICH: Estuarine flat along rivers with nipa vegetation,fine sediments 

(unripe) 

7. SATELLITE 

8. ABPTAT. PHOTOGRAPHS 

g. RADAR 

10. PAREHT MATERIAL 

a. Heatfaering 

b. Litbology 

c. Formation 


13. FISHERIES 

b. Source 


123/64/14/11/84 

1:100.000 

b. TffT^ftt-i ori: 

Permanent 

IS. VEGETAIIOH/LAHD OSE 

Area used 

IK irrnniiTm vnretrcm 

a. Occurence 

b. Evidence 

17. gun. G8EAT GSOOP 

Daainant >SOX 

Associated 1 

Associated 2 

Star-I/250/88/1110-2,4 

: clay 

: Qal 

: Brackish 

: Rain 

: Laut (sea) 

: High 

: nipah forest (nipah). 

including sedges 

: 0 X 



hydraquents 

fluvaquents 

sulfaquents 


heath forest (kerangas), bush, swamp (rawa) 

X of area Lab. checked 

80 X yes 

15 X yes 

5 X yes 

eqw/ /184-8 /68/IS/1110/52/ /67 / eqv/ /341-5 /72/SK/1110/24/ /07 / 

1110 - 45 

1

is. son. 

Proparties 

a. TtiQEfcŒO z topsoi.1 

sabsoil 


minorai «nil 

c. Drainage: 


sabsoil 

o. Total ran- *«~»»-ÎI 

sabsoil 

t. Avail. F: -atfaod 

topsoil 

sabsoil 


sabsoil 


sabsoil 


sabsoil 


sabsoil 


1. Acid salph. pot.: 




p. Organic Hatter : 

q. TEB : 


Donnant > SOI 


fine 

— 



— 

1er: 

low 

medium 

— 

very low 

— 

-- 

strong acid 


— 

-- 

— 

-- 

— 

-- 

50 cm 

6.4 

0.0 

0 

Associated 1 

fine 

fine 

-- 

vsrv desD 


— 

— 

very mgn 

very high 

Olsen 

medium 

very low 

low 

very low 

— 

-- 

slightly acid 

neutral 

— 

-- 

— 

— 

— 

-- 

100 cm 

2.6 

0.0 

3 

Associated 2 

fine 

fine 

— 

very deep 


very high 

very high 

very high 

very high 

medium 

high 

low 

medium 

low 

medium 

slightly acid 

slightly acid 

-- 

-- 

shallow depth 

saline 

19. ALTITUDE: Mari—: S m Mini«: 1 m Range: 3 m 

20. PLAH/reOFTLE: Dominant: No pronounced highs/lows 

Included: 

21. L.D. DRAIHAGE: a. Pattern: none b. density: Very low 


22. SLOPE: a. Steepness:flat b. Variability: Low 

c. Length: very short d. Variability: Low 


23. SLOPE D1STR-: Valleybottons: 100 1 

Interflnves : 0-8Z:0 X, 9-25Z: 0 Z, 25-55X: 0 X 

24. RELIEF AMPLI.: a. Hmyi i I mln very low b. Variability: Low 

25. TBBPATM- Flat, slope

LARD DHIT REPGBÏ IHEP-SDBM, CSR-BOGGR 

MAP HUGE: CSOSS SBCTIOB: 

1. LAHD OHTT: Bf. 5.1 2. MAP SHEET: 1110 3. AREA: 92 km2 

4. OOCÜREHCE by PB0VIHCE: Lampung: 99% 

5. STAIDS IDEHTIFIERS : Updated by: DR edit date: 30/05/89 Status: Final 

6. UHD DHIT DESCBIPTIOH: Saline b ackswamps with grass vegetation ,fine sediments (unripe) 

7. SATELLITE 

8. AERIAL PBDTOGBAPHS 

9. BADAR 


a. Weathering 

b. Lithology 

c. Formation 

12. HATER a. Quality : Saline 

b. Source : Rain 


14. BIVEBS a. Floodrisk : None 

b. Inundation 

15. VEGETATICH/LftHD USE : 

Area used : 

16. ACCELERATED EBOSICH 

a. Occoxence : 

b. Evidence : 

17. SOIL GSEAI GSOOP 

Dominant >SOZ 

Associated 1 

associated 2 

: 123/64/14/11/84 

: 1: .000 

: Star-I/250/88/1110-2,4 

: clay 

: Qal 

Permanent 

0 X 

32. BEESESEHIATIVE PROFILES: 


hydraquents 

sulfihemists 

sulfaquents 

eqw/ /184-8 /68/IS/1110/52/ /67 / 

eqi/ /84-1 /86/F /1110/53/ /15 / 

swamp (rawa) including sedges 

1110 - 47 

Z of area 

60 X 

30 X 

10 X 

11. SOCK OUTCROP: 

Lab. checked 

yes 

yes 

yes 

hei/ /112-12 /79/P /1110/53/F18/12 /


Properties 


subsoil 


c. Drainage: 

d. Erch. K: topsoil 

subsoil 

e. Total K2O? t^wKsi? i 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/ÏHQETLE: 

21. L.D. DRAIBA0E: 

22. SLOPE: 



25. TTOPHTW- 




29. FRAGMEHTATIOB: 

30. RELJABILITÏ: 

lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 

Donnant > 501 


fine 

-moderately 

deep 


— 

-- 

1 

low 

-- 

— 

medium 

very low 

-- 

— 

strong acid 


-- 

— 

— 

50 cm 

6.4 

0.0 

2 

Associated 1 

organic 

organic 


— 


high 

high 

-- 

— 

-- 

— 

-very 

high 

very high 


excessive acid 

very low 

low 

shallow depth 

salt free 

— 

47.5 

40.6 

0 

5 m Minimum: 1 m 


Included: 

a. Pattern: none 



c. Length: long 


Valleybotton»: 100 Z 

Interfluves : O-8Z:0 Z, 

a Ampli hula, »ory 1 r\xn 

9-25X: 0 Z, 25-551: 0 

b. 

Flat, slope

LAU) OBIT REPORT 

1. LAHD OHIT: Bf.5.2 

LBEP-SDBM, CS&-BOBGR 

MAP IMAGE: CSOSS SBCTIOH: 

4. OOCOREBCE by PROVIKE: Lampung: 99% 

1.2.1 

B.S.2 

^ . «*. 

5. STATOS IDEHTIFIERS : Updated by: DR edit date: 30/05/89 Status: Final 

6. LAID OMIT DESCRIPnOH: Saline backswamps with mixed forest,fine sediments (unripe) 

7. S*Tgl-f-1TH ^'fjflKK ; 123/64/14/11/84 

8. ABHTAT- PBOEQG8APBS : 1: .000 

9. RADAR : Star-I/250/88/1110-2,4 

10. PAREBT MATERIAL 


b. Litbology : clay 

c. Forant" ï rai : Qal 

12. HATER a. Quality : Saline 


Laut (sea) 

14. RIVERS a. Floodrisk : 


15. VEGEIATiaR/LABD OSE : peat swamp forest (gambut), swamp (rawa) including sedges 

Area used : 0 I 

16. ACCELERATED EROSIGH 

a. Occnrence : None 

b. Evidence : 

17. SOIL CSEAT GROUP 

Doainaat >50Z 

Associated 1 

Associated 2 

Permanent 

B.S.1 

B.1.2 



sulfihemists 

hydraquents 

X of area 

65 Z 

35 Z 

11. ROCK OOTCSOP: X 

Lab. checked 

yes 

32. unMtiu.iurr*Tiw|r PBQFILES: 

hei/ /112-1 /79/P /1111/53/Fol/Ol / eqw/ /112-11 /79/P /1111/53/F16/11 / 

1110 - 49 

yes 

B.1.1 

sea

IR a m ntAWktrTVBTsrr11*n 

Properties 


subsoil 


w^ TMkrjk l if*** 1 

c. Drainage: 


subsoil 

a. Total K2O: tonsoil 

subsoil 

f. Avail. P: nethod 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 




n. Other Taxicity: 



q. TEB : 


19. ALTITUDE: 

20. PLAH/PB0FILE: 

21. L-U. DRADUGE: 

22. SLOPE: 


24. RELIEF «MFLI. : 

25. TETOATM- 

26. ŒEST/RIDGES: 



29. FKAGHEflTATICH: 


lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 

Doainant > SOX 

organic 

organic 


__ 


very high 

high 

-- 

— 

very high 

-- 

— 

-- 

very high 

very high 



very low 

medium 

— 

shallow depth 

-- 

-- 

120 cm 

55.2 

44.5 

0 

Associated 1 


fine 

— 

very deep 


very low 

very low 

-- 

— 

high 

— 

-- 

— 

-- 

very high 



very low 

very high 

— 

very deep 

moderately 

-- 

120 cm 

22.3 

26.4 

0 

5 m MiniMsa: 1 m 





c. Length: 


ValleybottOBS: 100 Z 

Intarfluves : 0-8Z:0 X. 9-2SZ: 0 X. 25-551: 0 Z 

Associated 2 

0.0 

0.0 

0 

Range: 2 m 

b. density: 


d. Variability: Low 

a. flax»! i I mill very low b. Variability: Low 

Flat, slope

LAHD UBIT REPORT IKEP-SDBM, CSR-BOSOR 

1. UND DHIT: Bcq.7 

MAP IMAGE: CBOSS SECTIGH: 

sea 

B.7 

__-- urine sediients 

V.l.3.3 

v.1.4.2 ; i 

^.V/TOlcaic rocte * l '- 

4. OCCUREHCE by PROVIBCE: Lampung: 99% 

5. STATUS IDEHTIFIERS : Updated by: DR edit date: 30/05/89 Status: Final 

6. USD OBIT DESCRIPTIGH: Undifferentiated marine deposits,calcareous and coarse sediments, 

slopes 0-3X. 

7. SATELLITE SCERES : 

8. AERIAL PHOTOGRAPHS : 

9. KAOAR : 



b. Lithology : gravel, sand 


12. HATER a. Quality : Brackish 

b. Source : Rain, Not known 


14. RIVERS a. Floodrisk : None 

b. Inundation: Seasonal 

13. VBGETATIGH/LAHD OSE : mangrove forest (bakau), bush, alang-alang, coconut (kelapa), 

Area used : 



a. Occurence : None 

b. Evidence : 

Dominant >50I 

Associated 1 

Associated 2 

2. MAF SHEET: 1110 3. AREA: 75 km2 

123/64/14/11/84 

1:100.000 59 /8292-19 , 60 /8295-05 , 61 /8344-207 

Star-I/250/88/1110-1,3 

towns, villages 

90 X 


troporthents 

tropopsamments 

Z of area 

80 Z 

20 % 

X 


Lab. checked 

32. REPSESEHTATIVE PROFILES: 

eot/ / /88/SR/1010/44/ /48 / est/ /184-15 /68/IS/1110/43/ /95 / 

1110 - 51 

yes 

yes

18. SOU. CHARACTERISTICS 

Properties 


subsoil 


c. Drainage: 

mineralsoil 


subsoil 

e. Total K2Or tnnsnii 

subsoil 

f. Avail. F: method 

topsoil 

subsoil 


subsoil 

b. CEE pH 7 topsoil 

subsoil 


subsoil 



subsoil 


m. Salinity : 


o. Boot obsfcr. layer : 


q. TEB : 


19. ALTITUDE: 

20. FLAH/FBQFILE: 

21. L.D. DRAIHAGE: 

22. SLOPE: 



25. TFPBATW- 




29. FRAGMEHTATIOH: 

30. PFI.TABTI.TTT- 

10. b : 2 12.a: 2 

18. d-q: 2 19: 2 


coarse 

coarse 



very low 

very low 

low 

Olsen 

very low 

very low 

high 

high 

very low 

very low 

strongly alkaline 

strongly alkaline 

very low 

very low 

75 cm 

3.4 

22.5 

0 

Associated 1 

fine 

coarse 



-- 

-- 

low 

high 

high 

-- 

— 

-- 

-- 


neutral 

-- 

-- 

70 cm 

3.4 

0.0 

1 

Range: 

10 m Minium: 1 


Included: 






Valleybottoms: 20 Z 

Interfluves : 0-8Z:80 Z. 9-251: 0 


Flat, slope

LATO UBIT REPORT LREP-SDBM, CS8-BOOCK 

MAF IMAGE: CSOSS SECTIOH: 

Idij.1.1 

valley bottoi valley bottoi 

-, interfluve 1 

ft > L .. CO i 

dacitc (Iqniibrite) 

coarse felsic sedinentary rocks 

interfluve 

1. LAHD UHIT: Idq.1.1 


4. OCCŒEHCE by PROVTTCE: Lampung: 992 

5. SIAinS IDENTIFIERS : Updated by: DR edit date: 30/05/89 Status: Final 

6. LARD DBIT DESCRIPTIOH: Slightly dissected flat acid tuff plain,acid tuffs and felsic 

7. SATELLITE 

123/64/14/11/84 

8. AERIAL PBOTOGKAPBS : 1:100.000 61 /8344-197, 60 /8295-017, 59 /8292-029 

9. RADAR : Star-I/250/88/1110-2.3 

10. PARERT MATERIAL 

a. Weathering : Partial 

11. ROCK OuTCSaP: % 

b. Lithology : 

12. HATER 

c. Formation : Qlv 

a. Quality : Fresh 




b _ Inondation : None 

15. VBSEIATHM/LAHD OSE : 

16. 

17. 

Area used : 

ATXTEMWATED KRnCTKYf 

coarse sedimentary rocks, slopes 0-3X. 

liparite, dacite, sandstone 

, bush, alang-alang, upland crops, rainfed wetland rice, towns, 

villages 

a. Occurence : None 

b. Evidence : 

SOIL GREAT GROUP : 

Dominant >SOZ 

Associated 1 

Associated 2 


90 % 


kanhapludults 

tropaquepts 

dystropepts 

udh/ /84-14 /85/DN/1111/12/ /09 / 

ity/ /184-1 /68/IS/1110/44/ /52 / 

1.110 - 53 

X of area 

60 X 

30 X 

10 X 

Lab. checked 

yes 

yes 

yes 

iqt/ /84-12 /86/DK/1110/53/ /22 /

18. 

Properties 


subsoil 


c. Drainage: 


sobsoil 

t. Avail. P: 

Total P: 

CBC pH 7 

sobsoil 

•ethod 

topsoil 

subsoil 

topsoil 

subsoil 

topsoil 

snbsoil 

Soil Reaction:topsoil 

snbsoil 

Al Sat. topsoil 

snbsoil 

Al taxicity : 

Acid sulph. pot.: 

Salinity : 

Other Toxicity: 

Root obstr. layer : 

Organic Matter : 

TEB : 

Total observations: 

19. ALTITUDE: 

20. FLU/PROFILE: 

21. L.O. 

22. SLOPE: 


2«. PUT-TUP AMPLI. 

25. TBPBAT»- 

26. CHEST/RIDGES: 

27. VALLET FUXS: 

28. IAD FACETS: 

29. nUEMB*TAXICB: 

Doeinant > SOX 


fine 

very deep 

Well drained 

low 

low 

very low 

Bray I 

very low 

very low 

very low 

very low . 

low 

low 



very low 

medium 

salt free 

1.8 

1.9 

0 

Associated 1 

fine 

fine 



low 

low 

v ery J.OW 

very low 

Bray I 

medium 

low 

very high 

very high 

high 

high 


neutral 

very low 

very low 

salt free 

60 cm 

0.9 

18.2 

1 

Associated 2 

medium 


very deep 

Imperfectly drained 

medium 

very low 

low 

very low 



salt free 

120 cm 

2.7 

0.0 

3 

60 m Ifiniam: 40 m - Range: 50 m 

t: non-linear and random > 60X of area flat-topped 

Included: 

a. Pattern: dendritic b. density: Low 


a. Steepness:flat b. Variability: Low 

c. Length: extremely d. Variability: Low 


Valleybottoas: 10Z 

Interzlnves : 0-8Z: 85%, 9-251: 5 X. 25-551: 0 X 

a. »til 11 mil low b. Variability: Low 

Flat, slope

Ulli QHIT BEFOBI LREP-SDBM, CSR-BOGOR 

1. LARD IffllT: Idq.2.1 

H&P DKGE: SECTIOM: 

4. «TfflRHWT by PROVHICE 

5. STATUS IDENTIFIERS 

Idq.2.1 

valley bottoi 

interfltjve I interfluve 

I""* I dacite (igniibrite) 

!*•••) coarse felsic seditentiry rocks 

2. MAP SHECT- 1110 3. AREA: 792 km2 

Lampung: 99% 

Updated by: DR edit data: 30/05/89 Status: Final 

6. LARD O H DESCHIPTICH: Slightly dissected flat to undulating acid tuff plain, acid tuffs 

7. SATELLITE 

8. AEBIAL PHDTOGKAFHS 

9. BAtiAP 

10. IWRGHT MftTTITTftT 

a. Heatharing 

b. Lithology 

c. Fonnation 


13. FISHERIES 

b. Source 


b. Inondation 

15. VBÊTATIGH/LAHD USE 

16. 

Area used 

a. Occurence 

b. Evidence 


Devinant >SOZ 

Associated 1 

Associated 2 

and felsic coarse sedimentary rocks, slopes 0-8X 

123/64/14/11/84 

1:100.000 62 /8282-061, 60 

Star-I/250/88/1110-2,4 

High 

dacite, liparite, sandstone 

Qlv 

32. ^ nfuBRBMTAT 111 If PROFILES: 

Fresh 



None 

None 

/8295-013 

11. ROCK OOTCSaP: X 

, bush, alang-alang, upland crops, mixed gardens of fruit trees, 

rainfed wetland rice, coconut (kelapa), towns, villages 

90 % 

Localised 

Various 


kanhapludults 

tropaquepts 

dystropepts 

udh/ /86-33 /81/SR/1110/43/ /26 / 

ity/ /340-6 /71/SK/1110/41/ /19 / 

1110 - 55 

Z of area 

60 % 

25 % 

15 I 

Lab. checked 

yes 

yes 

yes 

iqt/ /86-36 /81/DK/1110/23/ /04 /

ia srm. nuauurmof^rrrrs 

Properties 


subsoil 


•dmeralsoil 

c. Drainage: 


sobsoil 

e. Total ren- «-~~~^J 

sobsoil 

f. Avail. P: method 

topsoil 

sobsoil 


sobsoil 

fa. CSC pH 7 topsoil 

sobsoil 

i. Soil Beaction:topsoil 

subsoil 


sobsoil 


1. Acid snlph. pot. : 

m. Salinity : 


o. Boot obstx. layer : 


q. TJEB : 


19. ALTITUDE: 

20. PLAR/PBQFILE: 

21. L.O. 

22. SIOPE: 


24. RELIEF AMPLI. 

25. TPPHftTH- 

26. mcai/H 



29. FRAGKERATIOI: 

Dcadnant > SOZ 

medium 

fine 

— 

very deep 

Well drained 

low 

low 

1 

very low 

— 

— 

very low 

very low 

medium 

low 

strong acid 

strong acid 

— 

-- 

— 

— 

— 

-- 

138 cm 

1.4 

2.8 

1 

Associated 1 

medium 

medium 

-- 



low 

"low 

very iow 

very low 

-- 

-very 

low 

very low 

very low 

very low 



-- 

-- 

— 

— 

— 

-- 

75 cm 

0.8 

1.4 

4 

Associated 2 


fine 

— 

deep 

Well drained 

— 

— 

— 

-- 

— 

-low 

very low 

— 

— 

neutral 

neutral 

-- 

-- 

— 

-- 

— 

-- 

90 cm 

2.1 

0.0 

9 

60 m MüninoB: 10 m Range: 40 m 

: non-linear and random > 60X of area flat-topped 

a. Pattern: dendritic 


a. Steepness:gently sloping 



Valleybottcas: 10 Z 

Intarflnves : 0-81:85 Z, 9-25Z: 5 Z, 25-551: 

a. Aaplitode: low b. 

Undulating 2- 8Z, 0-50 m 


d. Hidth: e. Variability: 

a. Hidth: very narrow b. Variability: Low 

-1- Interfluves. kanhapludult-.s, fin* 

—2- Depression on interflu, tropaquepts, 15Z 

-3- Valley bottoms, tropaquepts, 10Z 

-4- Interfluves, dystropepts, 15Z 

Valleys: Interxlnves: Large blocks 




0 Z 

Variability: Low 


30. RELUBnjR: 1« reliable, 2- probable, 3= tenable, 4- plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITIOSAL BOTES: 

1110 - 56

UHD IH1T LREP-SDBM, CSR-BOSOR. 

1. LABD ÜHTT: Idq.3.1 

IMF THEES: CBDSS SECTICB: 

4. CCCORESCE by HttJVlMIE: 

5. STATUS IIIHWTI kI WIR ; 

6. LARD DKIT DESCKOTTCS: 

7. ifTBT-f-TTB 

(igniiDrite) 

coarse feisic sedinentuy rods 

1: (undif f) top 2: slope 3: valley bottoi 

8. AESIAL FBOTOGSAFBS : 1:100.000 59 /8292-29 , 59 /8292-27 , 60 /8295-19 

9. BADftR : Star-I/250/88/1110-5 

10. MREHT MtTBPTÄT. 

a. Weathering : High 

11. ROCK ODTCSOF: Z 

b. Litbology : liparite, dacite, sandstone 

c. Formation : Qlv 

12. H&IE& a. QuaUty : 

Fresh 


13. gTjaraPTTcs : 

M. BIVEBS a. Floodxisk : 

b. Inondation: 

Not known 

None 

None 

15. VBSEtATIGH/tAHD OSE : , alang-alang, upland crops, mixed gardens of fruit trees, irrigated 

Area used : 

16. ACCELERATED EROSICH 

a. Occorence : 

b. Evidence : 

17. SOIL GREAT GROOF 

Donnant >50I 

Associated 1 

Associated 2 

32. REE8ESESIATIVE PROFILES: 


Lampung: 99Z 


Slightly dissected undulating acid tuff plain,acid tuffs and 

feisic coarse sedimentary rocks, slopes 3-8Ï 

123/64/14/11/84 

wetland rice (irigasi), towns, villages 

95 X 

Localised 

Various 


kanhapludults 

dystropepts 

tropaquepts 

udh/ /184-14 /68/IS/1110/43/ /92 / 

iqt/ /86-16 /81/NS/1110/42/ /25 / 

1110 - 57 

Z of area 

65 X 

30 X 

5 X 

Lab. checked 

yes 

yes 

yes 

ity/ /341-90 /72/IS/1110/44/ /52 /

IH srrn. rnA»Af-rreT

LAUD (OTT REPORT IREP-SDBi, CSR-BOBOR 

1. LARD OBIT: Idq.3.2 

MAP IMAGE: CBDSS SECTIOH: 

• . OOCUBEHCE by PRuvjjftv£: 

5- STATUS IDEHTIFIERS : 

6. LAID miT DESCHIFTIOH: 

7. SATELLITE 

8. ATOTAT.. CH0TQG8AFBS 

9. BAllAP 

10. VàBEBI MATBPTAI. 

a. Weathering 

b. Litfaolos7 

c. Formation 

12. H&TER a. Quality 

13. FISHERIES 

b. Source 

14. HIVEHS a. Floodrisk 

b. T TWg Ty^*"-'i op 

15. VBraXATIOH/LASD OSE 

16. 

Area used 

a. Occorence 

b. Evidence 

17. SOIL GREAT GBOOP 

32. 

udh/ 

iqt/ 

Dominant >30Z 

Associated 1 

Associated 2 

/184-14 

/341-58 

flattop 

1 

> 

2 

savabs 

3 

2 

jMq.3.2 

ï 

2 

Jr 

1 

12 

flat top 

1 

rt - ~ 

coars« felsic sedioentary rocks 

1: top 2: slope 3: valley bottoi 


Lampung: 99% 


Moderately dissected undulating acid tuffs plain,acid tuffs and 

felsic coarse sedimentary rocks, slopes 3-8% 

123/64/14/11/84 

1:100.000 58 /8292"53 , 60 /8295-19 , 62 /8282-61 

Star-I/250/88/1110-3,5 

Partial 


Qlv 

Fresh 

Perennial River, Medium wells 


None 

None 

11. F* M ^ OUTCROP: X 

, bush, alang-alang, mixed gardens of fruit trees, upland crops, 

irrigated wetland rice (irigasi), towns, villages 

90 % 

Common 

Gulleys 


kanhapludults 

dystropepts 

tropaquepts 

/68/IS/1110/43/ 

/72/DR/1110/53/ 

/92 / 

/63 / 

1110 - 59 

X of area 

60 X 

30 X 

10 X 

Lab. checked 

yes 

yes 

yes 

ity/ /86-28 /81/SR/1110/51/ /16 /

IA «arm numanrvBTSTTCs 

Properties 


subsoil 


•riiMrfll *ni 1 

c. Drainage: 


subsoil 

a. Xi*i#o£. AM/: 'iiupsoix 

subsoil 

f. Avail. F: nethod 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 

k. AI toxicity : 

1. Acid solph. pot. : 





q. TEB : 



fine 

fine 

— 

deep 

Well drained 

— 

— 

medium 

very low 

-- 

-low 

very low 

-- 

— 

strong acid 

strong acid 

-- 

-- 

— 

— 

— 

-- 

85 cm 

2.2 

0.0 

1 

Associated 1 





low 

low 

very low 

very low 

very low 

very low 

very low 

very low 



180 cm 

1.0 

2.1 

4 

Associated 2 

medium 

medium 

deep 


-- 

— ' 

low 

very low 

medium 

low 

very stro.ng acid 

strong acid 

100 cm 

1.5 

0.0 

2 

19. ALTITUDE: Hmriim»- 60 m Minions: 20 m Bange: 40 m 

20. PLAH/PBUFILE: Dominant: non-linear and random > 60% of area flat-topped 

Included: 

21. L.U. nPATMCT. a. Pattern: dendritic b. density: Moderate 


22. SLOPE: a. Steepness:gently sloping b. Variability: Medium 

c. Length: long d. Variability: Low 


23. SLOPE DISTR.: Valleybottoms: 10 X 

InterCluves : 0-8X:75 X, 9-25X: 15 2, 25-55X: 0 X 

24. RELIEF AMPLI.: a. Amplitude: low b. Variability: Medium 

25. TBBBATW- Undulating 2- SX, 0-50 m 

26. CREST/RIDGES: a. Shape: Level b. Length:Moderately long c. Variability: Low 

d. Width: moderate e. Variability: Low 

27. VALLEI FLOOR: a. Width: very narrow b. Variability: Low 

2B iJti F4CÏTS: -1- Flat top/upper sldyaa, kanhapluduits, ouï 

—2- Mid & lower slopes, dystropepts, 30X ' 

-3- Valley bottoms, tropaquepts, 10X 

-*- 

29. FRêCMEHTATIOH: Valleys: Intarfloves: Medium blocks 

30. RELIABILITY: 1= reliable, 2> probable, 3= tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITICHAL BOIES: 

1110 - 60

MftP DOGE: 

1. UU) OBIT: Idq.4.2 

4. uniun/f-Ç by ÏBDVIBCE: 

5. S1A1QS TnwiTI vI HIS ; 

6. UD m i DESCHIPTIOH: 

7. SATELLITE SCEHES : 

8. AWITAT. IHJ HI ijBAPHg ; 

9. BADAS : 

10. MEERT tiftTTHTM 



c. Fonation : 

12. HATER a. Quality : 

b. Source 

14. KIVEBS a. Floodrisk : 

b. Immd&'U.osi: 

15. VBGEIATICB/LAHD USE : 

16. 

Area osad 

a. Occnrence 

b. Evidence 

17. SOIL (SEAT GSOOP 

>5OZ 

Associated 1 

Associated 2 

Lampung: 99Z 

2 

Idq.4.2 

l 

2 

..... Vj/- • 

I 

(tacite (igniitrite) 

U.J 

12 2 

/• • 

.) cou» felsic sediKnUry recta 

41.4.2 

1: top 2: slope 3: valley botten 



Moderately dissected undulating to rolling acid tuff plain, acid 

tuffs and felsic coarse sedimentary rocks slopes 3-15Z 

123/64/14/11/84 

1:100.000 60 /8295-011, 60 /8295-019, 58 /8292-057 

Star-I/250/88/1110-2,5 

High 


Qlv 

32. BEfBESBRAIIVE PBOFILES: 

Fresh 


None 

None 

None 

11. BOCK OOTCBDP: Z 

, bush, alang-alang, shifting cultivation, upland crops, rainfed 

wetland rice, rubber (karet), towns, villages - 

90 Z 

Common 

Gulleys 


kanhapludults 

dystropepts 

tropaquepts 

ity/ Z86-25 /81/SR/1110/51/ /13 / 

iqt/ /341-15 /72/SK/1110/43/ /43 / 

1110 - 61 

Z of area 

55 Z 

35 Z 

10 Z 

1 

Lab. checked 

yes 

yes 

yes 

udh/ /84-19 /85/US/1111/14/ /09 / 

2

is. son. i EKISUCS 


subsoil 


•ttneralsoil 

c. Drainage: 

d. Each. K: topsoil 

Subsoil 

a. Total ran- »«~-i' 

subsoil 

f. Avail. P: Method 

topsoil 

subsoil 


subsoil 

h. CSC pH 7 topsoil 

subsoil 


subsoil 


subsoil 

k. Al texlcity : 

1. Acid solpb. pot.: 





q. TEB : 


19. ALTITUDE: 


21. L.Ü. DRAIHAGE: 

22. SLOPE: 


24. RELIEF AMFLI.: 

25. TBBBATW- 



28. LAB) FACETS: 

29. FRéGMEHTATIGH: 

Ooadnant > 50X 

fine 

fine 

— 

very deep 

Well drained 

low 

low 

vr-- I-;; 

very low 

Bray I 

very low 

very low 

very low 

very low 

low 

very low 

strong acid 


very high 

very high 

yes 

not relevant 

— 

— 

125 cm 

1.0 

0.4 

1 

A«itr1 Html 1 



— 

very deep 


high 

low 

uieaium 

very low 

• — 

-low 

very low 

low 

very low 



-- 

-- 

— 

— 

— 

— 

150 cm 

1.0 

1.7 

3 

Associated 2 

medium 

medium 

— 

deep 

Well drained 

— 

— 

medium 

very low 

Olsen 

low 

very low 

medium 

low 

-moderately 

acid 


-- 

-- 

— 

-- 

-- 

100 cm 

1.6 

0.0 

3 

100 m Minjfi: 10 m Range: 70 m 

Donnant: non-linear and random 40-60Z of area flat-topped 

Included: 

a. Pattern: dendritic b. density: Moderate 


a. Stn»ijiniss:sloping 



ValleybottoBB: 10 Z 

InterCLoves : 0-81:55 Z 

a. ABplitade: medium 

Rolling 9-15%, 0-50 m 

a. Shape: Level 

d. Width: moderate 

a. Width: very narrow 

•"•l* Crest/uppßT* Rlop?s, ~_n!?«pludulw3, 55Z 

-2- Mid & lower slopes, dystropepts, 35Z 


-4- 

Valleys: Intarflaves: Large blocks 



9-251: 35 Z, 25-551: 0 Z 


b. Length:Moderately long 

e. Variability: Low 


30. RELIABILITY: 1- reliable, 2« probable, 3- tenable, 4- plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 1 18.b: 1 18.c: 1 

18.d~q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

c. Variability: Low 

31. AUMTiUHAL KITES: Representative profile for Kanhapludults is extrapolated from sheet 

Menggala (Idq.4.2). 

1110 - 62

LAHD UH1T LKEP-SDBM, CSR-BOSOR 

1. 

4. 

MAP IMAGE: C8OSS SECTICB: 

OBIT: Idq.5.2 

ilWK by 

5. SIAIOS IDBHT 

6. LAHD DUIT DESCRIFTIOB: 

7. SATELLITE 

8. AEBIAL PHOTOGRAPHS 

9. BADAR 

10. « m t H&XEBIAL 

13. FISHERIES 

16. 

a. Weathering 

b. LAthology 

c. Fomatian 

b. Source 

b. Inundationi: 

None 

Area used 

«nrtintnn vamjrm 

a. Occurence 

b. Evidence 


Daainant >50I 

Associated 1 

Associated 2 

Lampung: 99X 

1 " 1J - : I "" i ""*lüff'7coarse~sedïiientary rocks 



Moderately dissected rolling acid tuff plain,acid tuffs and felsic 

coarse sedimentary rocks, slopes 8-15X. 

123/64/14/11/84 

1:100.000 59 /8292-025, 60 /8295-015, 82 /8282-73 

Star-I/250/88/1110-2.4 

: Partial 

: dacite, liparite, 

: Qlv 



: Perennial River, Medium wells 

: Sungai (river 1 

sandstone 

11. BOCK OUTCROP: X 

15. VEGETATIOH/LAHD USE : , bush, alang-alang, upland crops, mixed gardens of fruit trees. 


: 90 X 


: Common 

: Gulleys 


kandiudults 

dystropepts 

eutropepts 

udk/ /86-26 /81/SR/1110/42/ /14 / 

ite/ /341-28 /72/DR/1110/23/ /09 / 

1110 - 63 

X of area 

60 X 

30 X 

10 X 

Lab. checked 

yes 

yes 

yes 

ity/ /341-81 /72/IS/1110/42/ /35 /


Properties 


subsoil 


c. Drainage: 


subsoil 

a Totj.1 net- »—i' 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 





o. Boot obsfcr. layer : 


q. TEB : 


19. ALTITUDE: 


21. L.D. «ADAGE: 

22. SLOPE: 


24. BELIEF AMPLI.: 

25. TEPBATH- 


27. VALLEI FLOOR: 


29. FRAGMEHTATIOH: 

30. SELIABILITÏ: 

lO.b : 1 12.a: 2 

18.d-q: Z 19: 2 

31. ADDITIGHAL BOTES: 




-very 

deep 

Well drained 

low 

low 

- 

very low 

-- 

-low 

very low 

low 

very low 

strong acid 


-- 

-- 

— 

— 

— . 

-- 

125 cm 

1.4 

1.7 

3 

Associated 1 

medium 

medium 

-deeo 

uos r 

Well drained 

-- 

-very 

low 

very low 

Olsen 

very low 

very low 

very low 

very low 

-- 

— 

strong acid 

strong acid 

-- 

-- 

— 

— 

— 

-- 

100 cm 

0.8 

0.0 

2 

70 m Minlra: 40 m Bange: 50 m 

Dominant: non-linear and random 40-60% of area flat-topped 

Included: 



a. Steepness:sloping 




Interfluves : 0-8Z:30 %. 9-25X: 65 

a. Amplitude: medium 

Rolling 9-15Z, 0-50 m 

a. Shape: Undulating 

d. Width: moderate e. Variability: Medium 

a. Width: very narrow. b. Variability: Low 

-1- Crest/urmer slnno;] tsiîdiudults, SCS 

-2- Middle slopes, dystropepts, 30Ï 

-3- Lower slopes, eutropepts, 10X 

-4- 

Valleys: Interfluves: Medium blocks 

Associated 2 

medium 

medium 

— 

modératelv deen 


— 

-high 

very high 

Olsen 

medium 

very low 

low 

very low 

— 

-neutral 


-- 

-- 

— 

— 

— 

-- 

55 cm 

1.3 

0.0 

1 

b. density: Moderate 



Z, 25-551: 0 % 


b. Length:Short c. Variability: Medium 

1= reliable, 2= probable, 3= tenable, 4= plausible 

14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 

22: 2 23: 2 24: 2 28: 2 29: 2 

1110 - 64

UHIT BEFORT IREP-SDEM, CSR-BOGQR 

1. LABD UHIT: Idq.8.3 

IMF IMAGE: CSOSS SECTIGH: 

4. OOCDREHCE by ÏKCWHCE: 

5. STATUS IDEfiTIFIEBS : 

6. LAHD HOI DEStXIFTIOB: 

7. SATELLITE 

8. ATOTAI. FBOTOGSAPSS 

9. RADAR 

10. EftHEBT H»TFHTAT. 

a. HeatbexiH8 

b. Litbology 

c. Foimatian 

12. HUXR a. Quality 

13. FISHERIES 

b. Source 


b - TT—Ty^wfri OB 

15. VEEXTATICH/LARD USE 

16. 

Area used 

a. Occorence 

b. Evidence 

17. SOIL GREAT GBDOP 

Dominant >SOX 

Associated 1 

Associated 2 

Lampung: 992 



Strongly dissected rolling acid tuff plain with hillocks,acid 

tuffs and coarse felsic sedimentary rocks,slopes 8-25%. 

123/64/14/11/84 

1:100.000 62 /8282-075 

Star-I/250/88/1110-3 

Partial 


Qlv 

32. REERESEHTATIVE PROFILES: 

Fresh 

Perennial River 


None 

None 

, bush, grazing land, upland crops 

20 % 

Extensive 

Gulleys 


troporthents 

' eutropepts 

X of area 

80 X 

20 X 

X 


Lab. c 

yes 

eot/ /86-3 /81/NS/1110/23/ /04 / ite/ /86-35 /81/DK/1110/23/ /03 / 

1110 - 65 

yes

18. SOIL CBÀKACTERISnCS 

Properties 


subsoil 


mineralsoil 

c. Drainage: 


subsoil 

~. T^ttL * r ***" > - iij^.11 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 

J. Al Sat. topsoil 

subsoil 


1. Acid sulph. pot. : 

m. Salinity : 




q. TEB : 


Dominant > 50Z 

medium 


-mod. 

shallow 

Well drained 

high 

high 

Lie'" 

high 

-- 

-- 

very low 

very low 

low 

low 


slightly acid 

-- 

-- 

-- 

— 

— 

-- 

32 cm 

1.5 

6.5 

1 

Associated 1 

medium 

medium 

— 



low 

very low 

xow 

low 

low 

— 

-- 

very low 

high 

high 


strong acid 

-- 

-- 

— 

-- 

-- 

50 cm 

1.0 

22.9 

2 

Associated 2 

19. ALTITuDE: Mmrinrai: 70 m Minim: 25 m Bange: 40 m 

20. PLAH/PKOFIXE: Dominant: non-linear and random > 60% of area crested/peaked 

TTW-IUHPH- non-linear and random < 40% of area flat-topped 

21. L.D. DBATWGE: a. Pattern: dendritic b. density: Mod. high 

c. Variability: high 

22. SLOPE: a. Steepness:sloping b. Variability: High 

c. Length: short d. Variability: Medium 


23. SLOPE DISTB. : Valleybottans: 5 Z 

Interfluves : 0-81:10 X, 9-251: 75 %, 25-55Z: 10 X . 

24. BELIEF AMPLI.: a. Amplitude: medium b. Variability: Medium 

25. TFTOATW- hillocKy >16Ï, 0-50 m 

26. CREST/BTDSES: a. Shape: Irregular b. Lengtb:Short c. Variability: Medium 

d. Width: narrow e. Variability: Medium 

27. VALLEI' FLOCK: a. Width: very narrow b. Variability: Low 

28. LAUD FACETS: -1- Crest.s, nr> ft m.id slcpc, trcpcrthsnts, COS 

—2- Lower slopes, eutropepts, 20Ï 

-3- 

-4- 

29. FBAGMEBTATIOH: Valleys: Interfluves: Small blocks 

30. RELIABHJTÏ: 1= reliable, 2= probable. 3= tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 3 

31. ADDITIONAL SOXES: 

1110 - 66 

0.0 

0.0 

0

LAHD UU.I HMIff IXEP-SBm, CSR-BOGOR 

1. 

4. 

5. 

HftP IMAGE: CROSS SECTIOH: 

6. LAHD OBIT DESCRIPTIOH 

7. SATEIJ.TTE 

SCEHES 

8. ABHTA1. FflOTOSRAFBS 

9. PAPlAP 

12. HATER 

13. FISHESjjjS 


15. W KKKTÂT 11 W /J APP OSE 

16. 

LAHD DlŒT: 

Ftn.3.2 

«Jt by PROVINCE 

SIATDS xunrrLrj-Eic» 

10. BAKER MATERIAL 

a. Heathering 

b. Littaology 

c. Formation 

a. Quality 

b. Source 

tl TlHMMiartii em 

Area used 

HATW» HMftrUll 

a. Occurence . Localised 

b. Evidence . Gulleys 

17. SOIL 6BEAT 

G800P : 

Dominant >50Z 

Associated 1 

Associated 2 

32. REERESEfflATIVE EB0FILES: 

2. MAP SHEET: 1110- 3. AREA: 158 km2 

Lampung: 99X 


Moderately dissected undulating plain,metamorphic rocks, slopes 

3-8X 

123/64/14/11/84 

1:100.000 57 /8292-85 , '59 /8292-23 , 60 /8295-11 

Star-I/250/88/1110-5 

High 

schists, gneiss 

PTse 

Fresh 


None 

None 

None 


, bush, alang-alang, upland crops, rubber (karet) 

60 X 


kanhapludults 

dystropepts 

tropaquepts 

udh/ /340-52 /71/SD/1010/62/ /14 / 

iqt/ /86-41 /81/DK/1110/42/ /10 / 

1110 - 67 

Z of area 

60 X 

30 X 

10 X 

Lab. checked 

yes 

yes 

yes 

ity/ /341-13 /72/SK/1110/42/ /36 /

18. SOIL 

Properties 


subsoil 

b. Depth: ] peatsoil 

mim sralsoil 

c. Drainage: 


subsoil 

*—'I 

subsoil 

t. Avail. P: •othocl 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 

k'. Al taxicity : 

1. Acid sulph. . pot.: 

B. Salinity : 


o. Root obstx.. layer : 


q. TEB : 


19. ALTITUDE: 

20. PLAa/PROFILE: 

21. L.U. 

22. SLOPE: 


24. RELIEF «PLI. 

25. TEBBAT»- 

26. 



29. fKAGHEHTATICH: 

30. REUABHIR: 

lO.b : 2 12.a: 1 

18.d-q: 2 19: 2 




— 

very deep 

Well drained 

-- 

-- 

! — • : 

low 

— 

-low 

very low 

— 

— 

slightly acid 


• 

— 

- - 

— 

- - 

110 cm 

2.1 

0.0 

0 

- - 

Associated 1 

medium 

medium 

— 

mod. shallow 

Well drained 

-- 

-- 

low 

Olsen 

medium 

very low 

medium 

low 

— 

— 

slightly acid 

slightly acid 

— 

-- 

-- 

— 

-- 

40 cm 

3.0 

0.0 

1 

Associated 2 

moderately coaxse 

medium 

— 

very deep 


low 

low 

very low 

-- 

-very 

iow 

very low 

very low 

very low 


strong acid 

— 

-- 

— 

-- 

-- 

-- 

150 cm 

1.0 

3.3 

2- 

100 m Minima: 50 m Range: 70 m 

Dominant: non-linear and random 40-60% of area flat-topped 

Included: 




c. Length: moderate d. Variability: Low 


Valleybottoas: 10 % 

Intarfluves : 0-81:90 %, 9-2SZ: 0 Z, 25-551: 0 X 

a. Amplitude: low b. Variability: Medium 

Undulating 2- 8%, 0-50 m 

a. Shape: Level b. Length:Moderately long c. Variability: Low 

d. Hidth: moderate e. Variability: Low 

a. Width: very narrow b. Variability: Low 

-1- Interfluves, kanhapludults, 60% 

-2- Interfluves, dystropepts, 30Ï 

-3- Valley bottoms, tropaquepts, 10% 

-4- 

Valleys: Small blocks Interfluves: Medium blocks 

1- reliable, 2= probable, 3- tenable, 

14.a: 1 14.b: 1 17: 2 18.a: 1 

22: 2 23: 2 24: 2 28: 2 

4= plausible 

18.b: 2 18.c: 1 

29: 2 

31. ADDITIONAL BOXES: Representative profile for Kanhapludults is extrapolated from sheet 

1010 (Ptn.4.2). 

1110 - 68

1. LARD OBIT: Pg.4.2 

HAP WSE: GBOSS SBCTICB: 


4. OOCDREKX by PB0VIKE: Lampung: 99% 

5. SMIQS IDEHXIFIERS : Updated by: DR edit date: 30/05/89 Status: Final 

6. LAUD Œil DESCRICTICB: Moderately dissected undulating to rolling plain,acid plutonic 

rocks, slopes 3-15% 

7. 

8. 

9. RADAR 

10. 

13. 

16. 

17. 

SATKfJ.ITK ^J'HllfK 

AERIAL PHOTOGRAPHS 

PARER HftTERTAI. 

a. Heathering 

b. Lithology 

c. Formation 

Area used 

VTVf fiBATVn «MgtW 

a. Occorence 

b. Evidence 

wfi| |r uuifAT G800P 

IVTrinmrt >SOX 

Associated 1 

32. HhmB^HHIATXVK PROFILES: 

: 123/63/14/11/84 

: 1:100.000 57 /8292-83 , 57 

: Star-I/250/88/1110-4,5 

: High 

: granite 

: Kgr 

: Fresh 



: Not known 

: 90 % 

: Common 

: Gulleys 


dystropepts 

hapludults 

Associated 2 tropaquepts 

Z of area Lab. checked 

65 % yes 

30 

5 

/8292-85 

11. ROCK UUTUfliP: X 


b. Inmdatioil: 

None 

15. VESEIAZIQH/LAHD OSE : , bush, alang-alang, shifting 

villages 

cultivation, upland crops, towns. 

ity/ / /88/ER/lOlO/ / /42 / 

iqt/ /341-11 /72/SK/1010/42/ /34 / 

1110 - 69 

% yes 

Z yes 

uda/ /86/AH/1010/ / /7a /

18. SOIL CHABâ SISTICS 

Proparties 

a. Texture: topsoil • 

subsoil 


•ineralsoil 

c. Drainage: 


subsoil 


subsoil 


topsoil 

subsoil 

8. Total P: topsoil 

subsoil 


subsoil 


subsoil 


subsoil 





o. Hoot obstr. layer : 


q. TEB : 


19. ALTITUDE: 

20. PLAH/PHOFTLE: 

21. L.O. DBADttGE: 

22. SLOPE: 

23. SLOPE DISTK.: 

24. BELIEF AHPU.: 

25. TBUBATW- 

26. CHEST/ 

27. VALUY FLOCK: 


29. FBAGMEHTATIOH: 

30. BELIABUJTY: 

10.b : 1 12.a: 2 

18.d-q: 3 19: 2 

Donnant > 50Z 

fine 

fine 

very deep 

Well drained 

medium 

medium 

medium 

medium 

Bray I 

very low 

very low 

low 

low 

medium 

medium 



very low 

very low 

120 cm 

2.9 

6.9 

0 

Associated 1 

fine 

fine 

deep 

Well drained 

medium 

medium 

medium 

medium 

Bray I 

very low 

very low 

very low 

very low 

low 

medium 



high 

very high 

no 

98 cm 

1.6 

3.3 

0 

Associated 2 

medium 

medium 

very deep 

Well drained 

low 

very low 

Olsen 

low 

very low 

low 

very low 

very high 



80 cm 

1.9 

0.0 

0 

125 m »»

UHXT LREP-SDBM, CSR-BOGGR 

1. LARD HUIT: Ftn.4.2 

MAP DMCE: CSGSS SECTIGH: 

4. OCCOHEHCE by PBOVITCE: 

5. STAIDS IDEBTIFTERS : Updated by: DR edit dat«: 30/05/89 Status: Final 

6. LARD URIT DESCHIPTIOB: Moderately dissected undulating to rolling plain,metamorphic 

rocks,slopes 3-15X. 

7. SATELLITE SCEflES : 

8. AERIAL FHOTOGHAFHS : 

9. "Aru>p : 

10. BAKERT WTERTAI. 


b. Litbology : 






b _ Inondation: None 

15. VB5EIAII0H/LAID USE : 

16. 

Area used 

a. Occorence 

b. Evidence 

17. SOIL GSEAT G8O0P 

Damnant >5OI 

Associated 1 

Associated 2 

2. MAP SHEET: 1110 3. AREA: 129 kmZ 

Lampung: 99X 

123/64/14/11/84 

1:100.000 57 /8292-085, 57 /8292-083 

Star-I/250/88/1110-5 

gneiss, schists 

PTse 

Fresh 

11. BOCK OOTCHOP: X 

, bush, alang-alang, upland crops, mixed gardens of fruit trees, 

rubber (karet), coconut (kelapa) 

60 X 

32. KKHHKSmtAIXVE IBQFILES: 

Localised 

Gulleys 


kanhapludults 

dystropepts 

tropaquepts 

udh/ /340-52 /71/SD/1010/62/ /14 / 

iqt/ /340-07 / O/SK/1110/41/ /20 / 

1110 - 71 

Z of area 

60 X 

35 X 

5 X 

Lab. checked 

yes 

yes 

yes 

ity/ /184-12 / 0/IS/1110/43/ /86 /

10 OrtTT ÛDA^TvBTCffTPC 

• ^^ ^*^ • • • • ^^^m^m^mm m ^r^m m -^ • • • —» 

Pi.opm.tieg 


subsoil 


•riimral «oil 

c. Drainage: 


subsoil 

e. Totjii r^n- »^—-£1 

subsoil 

f. Avail. P: aethod 

topsoil 

subsoil 


subsoil 


sobsoil 


subsoil 


subsoil 



B. Salinity : 

n. Other Toxicity; 



q. TES : 


19. ALTITUDE: 

20. PLAH/PHOFILE: 


22. SLOPE: 

23. SLOPE DISTB. : 


23. TEOTAT»- 

26. C8EST/RXDGES: 



29. FBAQŒBTATI0H: 

Damnant > 501 



— 

very deep 

Well drained 

le:: 

low 

low 

— 

-- 

-- 

-- 

very low 

-- 

-- 

slightly acid 


-- 

-- 

-- 

— 

— 

-- 

110 cm 

2.1 

0.0 

0 

Associated 1 

medium 


-mod. 

shallow 

Well drained 

medium 

low 

low 

-- 

-- 

— 

-- 

very.low 

neutral 

— 

-- 

slightly acid 

— 

-- 

— 

— 

— 

-- 

40 cm 

2.4 

0.0 

1 

Associated 2 

medium 


— 

mod. shallow 


very low 

very low 

very low 

medium 

.-- 

-- 

very low 

medium 

low 

high 


slightly acid 

— 

-- 

— 

— 

-- 

-- 

30 cm 

0.4 

11.4 

1 

125 m Minis«: SO m Range: 80 m 

Dominant: non-linear and random 40-602 of area flat-topped 

Included: 



a. Steepness:gently sloping b. Variability: Medium 



Valleybottoas: S Z 

Interfiles : 0-8Z:70 X, 9-251: 25 X. 25-551: 0 X 

a. Aaplitode: low b. Variability: Low 

Undulating 2- 8%, 0-50 m 

a. Shape: Undulating b. Length:Short c. Variability: Medium 


a. Width: very narrow b. Variability: 

-1- Interfluves.. kanhaplndults, SO* 

-Z- Interfluves, dystropepts, 35Ï 

-3- Valley bottoms, tropaquepts, 5X 

-4- 


30. REU ABILITY: 1= reliable, 2= probable, 3= tenable, *- plausible 

10.b : 1 12.a: 2 l*.a: 1 14.b: 1 17: 2 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 7.2- 2 23: 2 24: 2 28: 3 29: 2 

M ADDITIGHAL KITES: r.ttpreEenta' ive profile for Kanhapludults is extrapolated from Sheet 

IC/.' O ;.n. • .2) . 

i no -

1. LUD DUT: Pg.8.2 

MAP IMAGE: SECIÏGH: 

4. I«IIIBW:W by rBOTOCB: 

5. STATUS IDEHTIFIERS : 

6. um ran DESCSIPTICH: 

7. SATELLITE 

8. AERIAL PBOIOGRAPBS 

10. PARE« MATERIAL 

a. Weathering 

b. Lithology 

c. Formation 


13. FISHERIES 

b. Source 


b. 

13. VBGEIATIOH/LAHD OSE 

16. 

Area used 

a. Occorence 

b. Evidence 

17. SDH. GSEAI GSOOP 

32. ••«*•«•« 

Dominant >SOZ 

Associated 1 

Associated 2 

ity/ /86-43 

iqt/ /341-H 

Lampung: 991 

2. MAP SHEET: 1110- . 3. AREA: 119 km2 

Updated by: DR ' edit data: 01/06/89 Statos: Final 

Moderately dissected rolling plain with hillocks,acid plutonic 

rocks, slopes 9-25X. 

123/64/14/11/84 

1:100.000 60 /8295-009, 57 /8292-87 

Star-I/250/88/1110-3 

High 

granite 

Kgr 

PROFILES: 

Fresh 



None • 

None 

11. ROCK OUTCROP: 5 X 

, alang-alang, shifting cultivation, upland crops, rubber (karet), 


80 X 

Common 

Gulleys 


dystropepts 

hapludults 

tropaquepts 

/81/DK/1110/42/ 

/72/SK/1110/42/ 

/12 / 

/34 / 

1110 - 73 

X of area 

65 I 

30 Z 

5 X 

Lab. checked 

yes 

yes 

yes 

uda/ /86/AH/1010/ / /7a /

IS. SOIL CHARACTERISTICS 

Properties 


subsoil 


c. Drainage: 


subsoil 


subsoil 

t. Avail. P: Method 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 


1. Acid sulpb. pot.: 

m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/PBOFILE: 

21. X..U. DBAUIAGE: 

22. SLOPE: 

23. SLOPE DISTS.: 


25. 

26. 


Z8. LAHD FACETS: 

29. FHAGMOnaTICB: 



medium 

very deep 


low 

low 

low 

low 

-- 

— 

very low 

very low 

low 

very low 

slightly acid 

neutral 

— 

-- 

-- 

125 cm 

0.6 

4.0 

5 

Associated 1 

fine 

fine 

deep 

medium 

marJi .im 

-- 

medium 

medium 

Bray I 

very low 

very low 

very low 

very low 

low 

medium 



high 

very high 

no 

98 cm 

1.6 

3.3 

0 

Associated 2 

medium 

medium 

very deep 

Well drained 

— 

- 

low 

very low 

Olsen 

low 

very low 

low 

very low 

— 

— 



-- 

— 

-- 

80 cm 

1.9 

0.0 

2 

100 m Miniana: 50 m Range: 75 m 

Donnant: non-linear and random 40-60Z of area flat-topped 

Tnclnded: 




c. Length; moderate 


Valleybottoas: 10 X 

InterCLnves : 0-81:20 





9-251: 50 X, 25-55X: 10 Z, >55X: 10 Z 


a. Shape: Irregular b. Length:Short c. Variability: Medium 


a. Width: very narrow b. Variability: Low - 

-1- Upper •+• lower slopes, dystropepts, 651 

-2- Middle slopes, hapludults, 30Z 


-4- 

Valleys: Interfluves: Small blocks 

30. RELIABILITY: 1° reliable, 2- probable, 3- tenable, 4» plausible 

lO.b : 2 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 U.b: 2 18.c: 2 

18.d-q: 2 19: 1 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITTOSAL BOTES: Representative profile for Hapludults is extrapolated from Sheet 

1010 (Hg.1.2.2). 

1110 - 74

USD DUT REPORT LREP-S0BM, CSR-BOBGR 

1. LAHD CHIT: Vab.1.2.3 

BLOCK DIAGRAM: CSDSS SBCT1OH: 

4. GCCOREICE by tSOTOCE: 

5. STATUS IDENTIFIERS : 

6. LAHD OBIT DESCRIPTIOH: 

7. RATFf _T. I TV. 

8. ABBTAI- FBOTOG8ACBS : 

9. BADAR : 

10. FARERT MATBBTAT- 

a. Heathexing : 

b. Litfaology : 

c. Fazaatian : Qhv 






15. VEGEIATIOH/LAHD USE : moist primary submontane forest, bush 

Area used : 

16. ACCELERATED EROSIGB 

a. Occnrence : Extensive 

b. Evidence : Gulleys 

17. SOU. G8EAI GBOOP 

Doadnant >SOZ 

Associated 1 

Associated 2 

32. REESESEHATIVE PROFILES: 


Lampung: 99Ï 


Strongly dissected upper slopes of volcanoes,intermediate and 

mafic tuffs and lavas, slopes >30%. 

123/64/14/11/84 

1:100.000 61 /8344-20 , 58 /8292-061 

Star-I/250/88/1110-1,3 

Partial 

andesitic tuffs, andesitic lavas, 

None 

0 Z l 


dystrandepts 

troporthents 

humitropepts 

iny/ / /88/HJ/1010/ / /30 / 

ith/ /340-26 /71/H /1110/43/ /60 / 

1110 - 75 

Z of area 

50 Z 

30 Z 

10 Z 

11. ROCK UUTLSUP: 10 X 

Lab. checked 

yes 

no 

yes

18. SOIL CBABACTERISTICS 

Properties 


subsoil 


c. Drainage: 


subsoil 

e. Total KZO: topsoil 

SUDSOll 


topsoil 

subsoil 

8. Total F: topsoil. 

sobsoil 


subsoil 

x. Soil Reaction:topsoil 

subsoil 


subsoil 


1. Acid snlph. pot.: 

m. Salinity : 



p. Orsanic Matter : 

q. TEB : 


19. ALTITUDE: 

20. PLAH/IBOFILE: 

21. L-D. DBAIHAGE: 

22. SLOPE: ' 

23. SLOPE OISTB. : 


25. TBgrarr- 

26. C8EST/BISGES: 

27. VALLET FLCKK: 

28. TABn FACETS: 

29. FBAEMERATIGH: 


medium 

medium 

very deep 

Well drained 

medium 

very low 

medium 

very low 

Bray I 

very low 

very low 

high 

medium 

high 

low 


strong acid 

very low 

very low 

150 cm 

11.3 

3.0 

0 

Associated 1 Associated 2 


fine 

0.0 

0.0 

0 

•: 1800 m Minima: 

Damnant: non-linear and random 

Included: 

a. Pattern: radial 


a. Steepness:Steep 




Well drained 

high 

very low 

medium 

very low 

high 

high 

high 

medium 



70 cm 

5.9 

1.8 ' 

1 

750 m Range: 1150 m 

> 60Z of area crested/peaked 

b. density: Mod. high 


d. Variability: High 

ValleybottoBS: % 

Inter£lmves : 0-81:0 X 9-251: 5 Z, 25-551: 40 X, >55X: 55 % 

a. Amplitude: very high 


Mountainous >16X, >300m 



a. Width: b. Variability: 

-1- Middle parts, dystrandepts, 50X 

-2- Crsst/upper paiLs, Lruporthents, 3ÜÏ 

—3- Lower parts, humitropepts, 10Z 

-4- 

Valleys: Interflnves: Small blocks 

30. RELIABILITY: 1= reliable, 2= probable, 3- tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 2 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. AMM.IJ.OHAL BOIES: Representative profile 

1010 (Vab.1.2.3). 

for Dystrandepts is extrapolated from Sheet 

1110 - 76

IAHD DDT KEHRT LBEP-SDBM, CSR-BOQGR 

BLOCK DIAGRAM: CSOSS SECTICH: 

'A 

*>30t A i 

v '\l 

V.l.3.3 

-


Properties 


subsoil 


c. Drainage: 


subsoil 


subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 


1. Acid snlpb. pot.: 

a. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAB/rSOFILE: 

21. L.V. DRATKAGE: 

22. SLOPE: 


2«. RELIEF AMPLI.: 

25. TERRAO: 




29. FRAGMEHTATIOB: 

Damnant > 501 

fine 

fine 

very deep 

Well drained 

high 

very low 

low 

very low 

very high 

very high 

high 

low 

medium 

low 

slightly acid 

strong acid 

130 cm 

11.9 

2 

Associated 1 

medium 


very deep 

Well drained 

medium 

low 

low 

very low 

very low 

medium 

low 

medium 

low 

slightly acid 

slightly acid 

very low 

low 

0.0 

0.0 

0 

Associated 2 

fine 

fine 

deep 

Well drained 

low 

Olsen 

very high 

very high 

very high 

very high 



90 cm 

5.8 

0.0 

2 

750 m MULÜBOB: 250 m Range: 500 m 

DoBinant: linear and random 40-60% of area crested/peaked 

Included: linear and random < 40% of area flat-topped 

a. Pattern: radial 





ValleybottoBs: % 

InterfLuves : 0-81:5 %, 

a. Aa^litode: high 

Mountainous >16%, >300m 

a. Shape: Irregular 




9-251: 35 I, 25-551: L0 X 


b. Length:Short 



-1- Upper part, dystropepts, 50% 

-2- Middle part, dystrandepts, 25% 

-3- Lower part, humitropepts, 10% 

-4- 


30. RELIABILITY: 1= reliable, 2= probable, 3= tenable. *= plausible 

lO.b : 1 12.a: 2 14.a: 1 l*.b: 1 17: 1 18.a: 1 13.b: 2 13.c: 

18.d-q: 2 19: 2 22: 2 23: 2 24: 7. 23: 3 29: 2 

31. ADDITIC8AL BOTES: 

1110 - 78 

c. Variability: Medium

BEBST ÎMBP-SBm, CSR-BOGCK 

1. LARD HUIT: Vab.1.4.2 

BLOCK DIAGRAM: C8DSS SECTIOB: 

4. OCCHBH9CE by PRCV1KCE: 

5. STATUS IOESTIFXXSS : 

6. LAHD OTIT DE3CHIPTICH: 

7. SATELLITE 

8. AESIAL PBOTOGBAFHS : 

9. RADAR : 

10. BAREST mTBBTAI. 



c. Formation : Qhv 

12. HtTER a. Quality : 


13. FISHEBIES : 

14. RIVERS a. FLoodrisk : 

b_ Inundation: 

15. VEGETATIGH/LAHD USE : moist primary lowland forest, bush, alang-alang, shifting cu 

Area used 

16. ACCELERATED EROSIG8 

a. Occurence 

b. Evidence 

17. SOU- i-SUHAT GBODP 

Donnant >SOZ 

Associated 1 

Associated 2 

Lampung: 99Ï 


Opdated by: DR edit date: 01/06/89 Status: Final 

Moderately dissected lower slopes of volcanoes,intermediate and 

mafic tuffs and lavas, slopes 8-15%'. 

123/64/14/11/84 

1:100.000 57 /8292-077, 58 /8292-063, 61 /8295-207 

Star-I/250/88/1110-2,3 


Fresh 

None 

11. BOCK OOTCSOP: 20 X 

ltivation, upland crops, irrigated wetland rice (irigasi), coffee 

(kopi), clove (cengkeh), rubber (karet), towns, villages 

80 % 

Localised 

Gulleys 


dystropepts 

hapludults 

humitropepts 

Z of area 

- 40 X 

30 X 

10 X 

Lab. checked 

yes 

32. BEEBESESTAIXVE PROFILES: 

ity/ /86-4 /81/NS/1110/21/ /05 / uda/ /341-59 /72/IS/1110/21/ /01 / 

1110 - 79 

yes 

no

1« SOX 


fine 

— 

very deep 

Well drained 

high 

low 

very high 

medium 

— 

-high 

low 

medium 

medium 

strong acid 

strong acid 

_. 

-- 

-- 

— 

-- 

-- 

120 cm 

1.8 

6.9 

4 

Associated 1 


fine 

-deep 

Well drained 

-- 

— 

verv hieh 

high 

Olsen 

medium 

low 

medium 

medium 

-- 

-neutral 

slightly acid 

- - 

- - 

- - 

100 cm 

1.7 

0.0 

1 

— 

- - • 

- - 

Associated 2 

0.0 

0.0 

0 

S00 m Miniana: 20 m Bange: 200 m 

Dominant: linear and parallel 40-60% of area flat-topped 

Included: 

•a. Pattern: parallel b. density: Moderate 


a. Steepness:gently sloping b. 

c. Length: long d. 


ValleybottOMs: 10 % 

Interdîmes : 0-81:80 2, 9-251: 10 %, 25-551: 

a. Amplitude: medium b. 

Rolling 9-15Î, 0-50 m 

a. Shape: Level b. Length:Moderately long 


a. Width: narrow b. Variability: Low 

-1- Upper & lower part, dystropepts, 40Ï 

-2- Middle part, hapludults, 30Z 

-3- Valleys, humitropepts, 10X 

-4- 

Valleys: Small blocks InterCLuves: Medium blocks 

1° reliable, 2= probable, 3° tenable, 4» plausible 

14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 

22: 2 23: 2 24: 2 28: 2 29: 2 

1110 - 80 

Variability: Medium 


0 % 


c. Variability: Low

LAHD OMIT BEFGST IBEP-SDBM, CSR-BOGQR 

V. 1.4.2 / 

-> 

BLOCK DIAGRAM: fMSS SECTICH: 

V.l.3.3 ^> 

1. LAHD EHIT: Vab.2.1.1 

^"" N 1.8 .3 

4. i»»aium;g by IBUV1NU£: 

s. siams roarruieas : 

6. IABD OBIT DE3CB1PTICH: 

7. SATELLITE 

8. ATOTAT- PHOTOGRAPHS : 

V.2.1. 

\ 

N 

.2.2.2 

9. RADAR : Star-I/250/88/1110-2 

10. PAREU! MATERIAL 

a. Hnnthnring : High 

b. Litbology : andesitic tuffs, basalt, 






b _ Tut »TMât-i on ; 

15. VESETATHB/LAHD OSE : 

(irigasi), coconut (kelapa), towns, villages 

Area used : 90 % 

16. ACCELERATED ERGSIOS 

17. SOIL GSEAT GSOOP 

a. Occnrence : Localised 

b. Evidence : Landslips 

Dominant >50I 

Associated 1 

Associated 2 

32. PKWifj%yjTATirg|B; 


Lampung: 99% 


Slightly dissected flat volcanic plain,intermediate and mafic 

tuffs and lavas, slopes 0-3Ï. 

123/64/14/11/84 

1:100.000 62 /8282-075 

None 


, upland crops, rainfed wetland rice, irrigated wetland rice 


hapludalfs 

tropaquepts 

Z of area 

80 X 

20 X 

X 

Lab. checked 

ada/ /341-61 /72/IS/1110/21/ /03 / ity/ /341-66 /72/IS/1110/23/ /08 / 

1110 - 81 

yes 

yes


Proporties 

a. Textare: topsail 

subsoil 


mineralsoil 

c. Drainage: 

d. Ercb. K: topsoil 

subsoil 

e. Total K2O: toosnil 

subsoil 


topsoil 

subsoil 


subsoil 

h. CEE pH 7 topsoil 

subsoil 


subsoil 

j. AI Sat. topsoil 

subsoil 

k. Al toxlcity : 


m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/IB0FILE: 

21. L.D. DBAIBAGE: 

22. SLOPE: 

23. SLOFE DISTR.: 

24. RELIEF AMFLI.: 

25. TEBRAIB: 

26. CREST/HEDGES: 


28. LABD FACETS: 

29. FBAGMEflTATIOH: 


medium 


deep 

Well drained 

1 nu 

low 

Olsen 

very low 

very low 

low 

low 


slightly acid 

100 cm 

1.4 

0.0 

1 

Associated 1 


fine 



i «~* 

very low 

Olsen 

low 

very low 

low 

very low 


slightly acid 

80 cm 

2.1 

0.0 

4 

Associated 2 

0.0 

0.0 

0 

125 m Minimal: 50 m Range: 75 m 

Dominant: linear and random > 60% of area flat-topped 




c. Length: extremely 






Interfiles : 0-81:80 X, 9-25Z: 0 X, 25-551: 0 X 

a. Arçtlitode: low 


Flat, slope

LAHD ÖHIT BEPCRT LHEP-SDBM, CSR-BOGGR 

1. LftHD EHBXT: Vb.2.1.1 

BLOCK DIAGKAM: SECTICH: 

4. OCCOREBCE by PBGWIBCE: 

5. STATUS HJEHTIFIEBS : Bpdated by: DR edit date; 01/06/89 Status: Final 

6. LAID HHIT BESCRIFTICH: 


8. AERIAL FHOTOGSAPHS : 

9. BABAK : 



b. Ldtfaology : 


12. KATES a. Quality : Fresh 




b. Inundation: None 

15. VEGETATIGH/LARD USE : 

Aroa 


a. Occurence 

b. Evidence 

17. SOIL G8EAI G8COP 

Dominant >SOZ 

Associated 1 

Associated 2 

0 2. MAP SHEET: 1110 3. AREA: 52 km2 

Lampung: 99Ï 

Slightly dissected flat volcanic plain,intermediate and mafic 

lavas, slopes 0-3% 

12.3/64/14/11/84 

1:100.000 62 /8282-65 , 62 /8282-63 

Star-I/250/88/1110-4,5 

High 

basalt 

Tov 

32. REFRESEBTATIVE PROFILES: 

11. BOCK OOTCSaP: 0 X 

, upland crops, irrigated wetland rice (irigasi), clove (cengkeh), 


100 X 

Localised 

Landslips 


hapludalfs 

dystropepts 

tropaquepts 

ada/ /341-56 /72/DR/1110/51/ /56 / 

iqt/ /341-91 /72/IS/1110/51/ /53 / 

1110 - 83 

X of area 

60 % 

20 X 

20 X 

Lab. checked 

yes 

yes 

yes 

ity/ /341-21 /72/SK/1110/51/ /62 /

Properties 

a. Textaro: topsoil 

subsoil 


•imral «*tï 1 

e. Drainage: 

dV Brch. K: topsoil 

subsoil 

e. Total K2O: tonsoil 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 

i. Soil Eeaction:topsoil 

subsoil 


subsoil 


1. Acid solph. pot.: 

m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAB/PBQFXLE: 

21. L.U. DBAIBBSE: 

22. SLOPE: 



25. TEBBAXB: 

26. 



29. FBAGMEBTATIOS: 


medium 

fine 

— 

mod. shallow 

Well drained 

-vprv 

hi oh 

very high 

Olsen 

high 

medium 

high 

high 

-- 

-neutral 

neutral 

-- 

-- 

— 

-- 

— 

-- 

50 cm 

4.7 

0.0 

0 

Associated 1 

fine 

fine 

deep 


very low 

Olsen 

very low 

very low 

high 

high 

strong acid 


100 cm 

1.9 

0.0 

0 

Associated 2 

medium 

medium 

very deep 


medium 

Olsen 

medium 

low 

very high 

very high 

strong acid 


125 cm 

18.7 

0.0 

0 

60 m Mini—: 25 m Bange: 40 m 

Dominant: linear and random > 60% of area flat-topped 

Included: 






Valleybottans: 20 7, 

Interfloves : 0-81:80 X 

a. Aaplitode: low 

Flat, slope

LAUD DIBIT BEPOST LREP-SDSM, CSR-BOGCB 

BLOCK DIAG8AM: CSDSS SECTION: 

1. LAHO MBIT: Vab.2.2.1 

4. nrnnnnBTF by PK0VXBCE: 

V.l.4.2 

50I 

Associated 1 

Associated 2 

Lampung: 99% 


Slightly dissected undulating volcanic plain intermediate and 

mafic tuffs and lavas, slopes 3-8X. 

123/64/14/11/84 

1:100.000 58 /8292~57 , 57 /8292-81 

Star-I/250/88/1110-1,3 

andesitic tuffs, basalt, 

11. BOCK GOTCBaP: X 

, bush, alang-alang, irrigated wetland rice (irigasi), towns, villages 

95 I 

: Localised 

: Landslips 


dystropepts 

hapludults 

tropaquepts 

ity/ /184-9 /68/IS/1110/41/ /77 / 

iqt/ /341-45 /72/DR/1110/41/ /33 / 

uda/ /184-10 /68/IS/1110/41/ /79 / 

1110 - 85 

Z of area 

60 l 

30 X 

10 ï 

Lab. checked 

yes 

yes 

yes

Properties 

a. Twiljiror 

strfisoil 


•in 

e. Drainage: 

d. Enrh. K: topsoil 

a. Total K3W- 

£. Avail. F: 

8- Total P: 

h. CSC pH 7 

topsoil 

subsoil 

sid] soil 

•ethod 

topsoil 

subsoil 

topsoil 

sobsoil 

topsoil 

subsoil 


subsoil 


subsoil 

k. Al toaticity : 

1. Acid salph. 

pot.: 

m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAS/FfiOFILE: 

21. L.0. DBAHAGE: 

22. SLOPE: 

23. SLOPE DISTK.: 

24. BELIEF AHFLI.: 

25. irraPAT«- 

26. CTEST/BIDGES: 

27. VAIXET FIDOS: 

28. tjii» FACETS: 

29. 

Damnant > 501 

medium 


-moderate*ly 

deep 

Well drained 

— 

— 

-cdivlow 

— 

-medium 

low 

-- 

-moderately 

acid 


— 

-- 

-- 

-- 

— 

-- 

70 cm 

0.9 

0.0 

1 

Associated 1 

fine 

fine 

— 

deep 

Well drained 

— 

_ 

lw.. 

low 

— 

-low 

very low 

-- 

— 



-- 

— 

-- 

-- 

— 

-- 

100 cm 

1.6 

0.0 

2 

Associated 2 

medium 

medium 

-- 

vôrv dsaiD 

» w Jh J S4 w w ^f 


— 

-very 

low 

very low 

Olsen 

low 

low 

very low 

very low 

— 

— 



— 

-- 

-- 

-- 

-- 

120 cm 

1.6 

0.0 

2 

175 m ttLnira: 100 m Bange: 125 m 

Damnant: non-linear and random > 60% of area flat-topped 

Included: 




a. Steepness:gently sloping b. Variability: Medium 





Interfloves : 0-8Z:90 %, 9-25Z: 0 I, 25-551: 0 X 

a. Aqalitode: low 

Undulating 2- 8Ï, 0-50 m 






-1- Interfluves. dvstropepts. 60Z 

-2- Interfluves, hapludults, 303; 

-3- Valleys bottoms, tropaquepts, 10X 

-•- 

Valleys: Small blocks Interflaves: Medium blocks 

30. KU.TAHn.TIY: 1= reliable, 2» probable, 3= tenable, 4° plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITIOBAL HOTES: 

1110 - 86

LAM) UUT REKBÏ LREP-SDHM, CSR-BOGGR 

1. LAS) UMT: Vb.2.2.1 

BLOCK DIAGRAM: CROSS SECTIGB: 

4. umiKMBlE by ISUVIKE: 

5. STATUS ŒEBTIFIERS : 

6. LAB) DBTT DESCROTIOH: 

7". 

8. 

9. 

10. BABOrr M«TFI»TATa. 

»feathering 

b. Littoology 

c. Formation 


13. FISHERIES 

b. Source 


IS. VBSETATHH/LABD USE 

16. 

17. 

Area used : 

AflTKl-HiATfin ÜROÎH 


b. Evidence : 

SOU. C8EAI GROOP : 

Doainant >SOX 

Associated 1 

Associated 2 

V.2.10.2 

V.2.2.1 

aruc rpcks/>.J "ƒ< \» 


Lampung: 99Z 


V.2.6.2 

Slightly dissected undulating volcanic plain,intermediate and 

mafic lavas, slopes 3-8Z 

123/64/14/11/84 

1:100.000 61 /8344-195, 61 /8344-191, 62 /8282-069 

Star-I/250/88/1110-4,5 

Partial 

basalt 

Qb 

32. REfSESESTATIVE ÏWHTLES: 

Fresh 



None 

None 

11. ROCK OOTCSOP: X 

, bush, alang-alang, upland crops, rainfed wetland rice, tea 

(teh), coffee (kopi), towns, villages 

90 % 

Localised 

Landslips 


hapludalfs 

dystropepts 

tropaquepts 

ada/ /341-56 /72/DR/1110/51/ /56 / 

iqt/ /3A1-.93 /85/IS/1110/51/ /53 / 

1110 - 87 

X of area 

60 Z 

30 Z 

10 Z 

Lab. checked 

yes 

yes 

yes 

ity/ /341-21 /72/SK/1110/51/ /62 /

IB. SDU. GHABêCTÜRlSIlCS 

a. Iitluie: topsoil 

subsoil 


c. Drainage: 


subsoil 

a. Total K2O: topsoil 

subsoil 

£. Avail. P: Method 

topsoil 

subsoil 


subsoil 


subsoil 

i. Soil Beaction:topsoil 

subsoil 


subsoil 

k. Al toacicity : 


m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAI/PBOFILE: 

21. L.O. 

22. SLOPE: 


24. BELIEF AMPLI. 

25. 

26. 

27. VALLET FLOCB: 


Donnant > SOX 

medium 

fine 

— 

mod. shallow 

Well drained 

-- 

-very 

high 

very high 

Olsen 

high 

medium 

high 

high 

-- 

— 

neutral 

neutral 

— 

— 

— 

-- 

— 

-- 

50 cm 

4.7 

0.0 

1 

Associated 1 

fine 

fine 

-deep 


— 

medium 

very low 

Olsen 

very low 

very low 

high 

high 

-- 

— 

strong acid 


— 

-- 

— 

-- 

— 

-- 

100 cm 

1.9 

0.0 

1 

75 m Minis«: 25 m Bange: 40 m 

: non-linear and random > 60Ï of area flat-topped 

9. Pattern: dendritic 


a. Steepness:gently sloping 

c. Langte: extremely 


ValleybottoBs: 10 X 

InterflnVBS : 0-81:90 

a. lea.il i I mln low 


Associated 2 

medium 

medium , 

— 

very deep 


— 

— 

medium 

medium 

Olsen 

medium 

low 

very high 

very high 

-- 

— 

strong acid 


— 

-- 

— 

-- 

— 

-- 

125 cm- 

18.7 

0.0 

1 



X. 9-2SZ: 0 X, 25-551: 0 Z 


Undulating 2- 8X, 0-50 m 



d. Hidth: e. Variability: 

a. Hidth: very narrow b. Variability: Low 

-1- Interfluves, hapludalfs, 60X 

-2- Interfluves, dystropepts, 30X 

-3- Valleys, tropaquepts, 10X 

-4- 

Valleys: Small blocks Interfluves: Medium blocks 

30. BEUABUJCT: 1- reliable, , - âbable, 3= tenable, 4° plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. AODITIGBAL KITES: 

1110 - 88

LAÜD UUT LREP-SDBH, CSK-BOGOB 

1. LAID HUT: Vab.2.2.2 

BLOCK DIAGRAM: CSOSS SECTIOH: 

4. ODCORÈSCE by P&OtHBCE: 

5. SIATDS IDEBTIFIEBS : 

6. LAID tffllT DESCRIPTIGH: 

7. 

8. 


Lampung: 992 


Moderately dissected undulating volcanic plain,intermediate and 

mafic tuffs and lavas, slope 3-8Z. 

9. RADAR 

10. PAREHT MUTTOTAT 

: Star-I/250/88/1110-2 

a. Woathnring : Partial . 



16. 

RATET J.ITIE MiÜWWK ; 

AERIAL PBOTOGBAPBS : 



Area used : 

a. Occnrence : Localised 

b. Evidence : Landslips 

17. SOIL GREAT GROUP : 

Destinant >50Z 

Associated 1 

Associated 2 

123/64/14/11/84, 

1:100.000 61 /8344-205, 62 


Qhv 

13. FISHERIES : Not known 


h Tnmi«1atirm- None 

15. VBSETATI08/LARD USE : , upland crops, mixed gardens < Df fruit trees, rainfed wetland 

rice, clove (cengkeh), < ;oconut (kelapa), towns, villages 

32. REHtESERTATTVE PROFILES: 

100 X 


dystropepts 

hapludults 

tropaquepts 

ity/ /184-9 /68/IS/1110/41/ /77 / 

iqt/ /341-45 /72/DR/1110/41/ /33 / 

1110 - 89 

Z of area i 

60 X 

30 X 

10 X 

/8282-77 

, 62 /8282-75 

11. ROCK OtnXSOP: X 

Lab. checked 

yes 

yes 

yes 

uda/ /341-62 /72/IS/U10/ / /04 /

Properties 

ft. Textnxo : topsoiX 

subsoil 


atnanlcnii 

c. Drainage: 


subsoil 


subsoil 


topsoil 

subsoil 


subsoil 

h. CEE pH 7 topsoil 

subsoil 


subsoil 


subsoil 



B. Salinity : 


o. Root obstx. layer : 


q. TEB : 


Daainant > 501 

medium 


— 


Well drained 

-- 

-medium 

low 

— 

-medium 

low 

— 

— 



-- 

-- 

— 

— 

— 

-- 

70 cm 

0.9 

0.0 

0 

Associated 1 

fine 

fine 

very deep 

Well drained 

very high 

high 

Olsen 

very high 

low 

very high 

medium 

slightly acid 


100 cm 

2.1 

0.0 

1 

dated 2 

medium 

medium 

very deep 


very low 

very low 

Olsen 

low 

low 

very low 

very low 



120 cm 

1.6 

0.0 

0 

19. ALTITUDE: Marian: 250 m Miniaa: 10 m Bange: 200 m 

20. PLAH/F8QFILE: Doainant: non-linear and random 40-60! of area flat-topped 

Included: 

21. L.O. DRAIBAGE: a. Pattern: dendritic b. density: Moderate 


22. SLOPE: a. Steepness:gently sloping b. Variability: Medium 



23. SLOPE DISTR. : Valleybottoas: 10 Z 

Interfluves : 0-81:90 X, 9-25Z: 0 Ï, 25-551: 0 X 

24. RELIEF AMPLI.: a. Pill il min: medium b. Variability: Medium 

25. TEBBATM- Undulating 2- 8Ï, 0-50 m 

28. IIWMT/Blimits- a. Shape: no crests b. Length: c. Variability: 


27. VALLET FIDOS: a. Width: very narrow b. Variability: Low 

2S. LSSS ?—-~...- -X- Iui,er£iuves, dysbropepts, ÔÛÏ 

-2- Interfluves, hapludults, 30Ï 

-3- Valley bottoms, tropaquepts, 10Ï 

-4- 

29. IRAGMEnATlUI: Valleys: Small blocks Intarfluves: Medium blocks 

30. RELUBUJTT: 1« reliable, 2= probable, 3° tenable. 4- plausible 

10.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITIONAL BIES: Representative profiles for Dystropepts and Tropaquepts are extrap 

olated from other LU (Vab.2.2.1). 

1110 - 90

LAHD OBIT KEPC8T LREP-SDBM, CSR-BOGGB 

1. LAHD BHTT: Vab.2.3.1 

BLOCK DIAGBAM: C8CSS SECTICH: 

4. 00CDRE8CE by PRCWIBCE 

5. STATUS HJEHTXFIERS 

6. LAHD HUMT DESCRIPTIO8 

7. SATELLITE SCESES 

8. ABPTÀT- PBOTOGKASBS 

9. RADAR 

10. PAREHT tttlEBIAL 

a. Weatfaering 

b. Lithology 

c. Formation 


13. FISHERIES 

b. Source 


b. 

IS. VEGEIAXIOH/LAKD USE 

Area used 


a. Occozemce 

b. Evidence 

17. SOU. G8EAI G800P 

Dcnüaant >SOZ 

associated 1 

Associated 2 

2. MAP SHEET: 1110- ' 3. AREA: 154 km2 

Lampung: 99% 


Slightly dissected rolling volcanic plain,intermediate and mafic 

tuffs and lavas, slopes 8-15Ï. 

123/64/14/11/84, 

1:100.000 58 /8292-59 , 61 /8344-205, 

Star-I/250/88/1110-2,4 

High 


Qhv 

32. REPRESEBTATIVE PROFILES: 

Fresh 


None 

None 

11. ROCK DOTCBOP: % 

, alang-alang, upland crops, mixed gardens of fruit trees, irrigated 

wetland rice (irigasi), rainfed wetland rice, clove (cengkeh), 

coconut (kelapa), towns, villages 

100 X 

Localised 

Landslips 


dystropepts 

hapludults 

tropaquepts 

ity/ /341-44 /72/DR/1110/41/ /32 / 

iqt/ /341-46 /72/DR/1110/41/ /35 / 

1110 - 91 

Z of area 

60 I 

30 Ï 

10 X 

Lab. checked 

yes 

yes 

yes 

uda/ /86-32 /23

18. SOIL CHàRACTEBISnCS 

PmnM"ti es 

a. Tartare: topsoil 

subsoil 


•dneralsoil 

c. Drainage: 


subsoil 


SUDSOXX 

£. Avail. P: aethod 

topsoil 

subsoil 


sobsoil 

h. CSC pH 7 topsoil 

subsoil 


subsoil 


subsoil 



B. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/FKCSTLE: 



fine 

deep 

Well drained 

-- 

-high 

low 

Olsen 

low 

very low 

medium 

low 

— 

-neutral 

neutral 

85 cm 

1.6 

0.0 

1 

Associated 1 

fine 

fine 

very deep 

Well drained 

high 

medium 

medium 

low 

-- 

— 

low 

very low 

low 

low 

strong acid 

strong acid 

125 cm 

2.1 

7.2 

2 

Associated 2 

medium 

fine 

deep 


— 

— 

very low 

very low 

Olsen 

medium 

very low 

medium 

very low 

_- 

_- 

strong acid 

strong acid 

100 cm 

2.6 

0.0 

2 

ISO m mniana: 20 m Range: 100 m 

Dominant: non-linear and random A0-60Ï of area flat-topped 

21. L.U. nPATMiîE- a. Pattern: dendritic b. density: Low 


22. SLOPE: a. Steepness:sloping b. Variability: Median. 

c. Length: long d. Variability: Medium 


23. SLOPE DIST&.: ValleybottOBs: 10 I 

Interflnves : 0-81:60 X, 9-251: 30 X. 25-551: 0 t 

24. RELIEF AMPLI.: a. frill iIi»ln medium b. Variability: Medium 

25. TTMBAT»- Rolling 9-15X, 0-50 m 

26. CREST/RIDGES: a. Shape: no crests b. Length: c. Variability: 


27. VALLET FLOOR: a. Width: very narrow b. Variability: Low 

28. LAID FACETS: -1- Interfluves, dystropepts, 602 

—2— XiitôxfIÜVÖÖ, liapluuulùs, 30X 

-3- Valleys bottoms, tropaquepts, 10X 

-4- 

29. FRAGMHRATICH: Valleys: Small blocks InterfiLnves: Medium blocks 

30. PW-TÄHTTTTV. l- reliable, 2« probable, 3= tenable, 4» plausible 

10.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 18.b: 1 18.c: 2 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 3 29: 2 

31. ADDITICBAL KITES: 

1110 - 92

1. DU© DBIT: Vb. 2. 3.1 

LBEP-SDHtt, CSR-BOSGR 

BLOCK DIAGRAM: CROSS SECTIGH: 

4. OCCDKEBCE by PRGVISCE: 

5. SUniS IDENTIFIERS : 

6. LABD OMIT DESCRIPTIOB: 

7. SATJBTJ-TTE SCEHES : 

8. AERIAL ifHUTUjRAPBS : 

9. RADAR : 



b. Lithology : basalt, 

c. Fomation : Qb 

12. H&IER a. QoaUty : Fresh 



14. RIVERS a. FLoodxisk : None 

b. Imnadafcxan : 

15. VBSEXATIOH/LAHD USE : 

16. 

Area used 

a. Occnrence 

b. Evidence 

17. SOIL G8EAT GROUP 

Dominant >SOZ 

Associated 1 

Associated 2 

32. P^HiiuîJi t*y |U|f 

Lampung: 99Z 

2. MftP SHEET: 1110- 3. AREA: 172 km2 


Slightly dissected rolling volcanic plain,intermediate and mafic 

lavas, slopes 8-15Z. 

123/64/14/11/84 

1:100.000 62 /8282-65 , 62 /8282-67 , 62 /8282-69 

Star-I/250/88/1110-4 

None 

11. ROCK OUTCROP: 5 % 

, alang-alang, upland crops, mixed gardens of fruit trees, coffee 

(kopi), tea (teh), towns, villages 

100 Z 

Localised 

Landslips 


dystropepts 

hapludalfs 

tropaquepts 

ity/ /84-10 /86/DK/1110/51/ /20a/ 

iqt/ /84-12 /86/DK/1110/53/ /22a/ 

1110 - 93 

Z of area 

60 Z 

35 Z 

5 Z 

Lab. checked 

yes 

yes 

yes 

ada/ /341-56 /72/DR/1110/51/ /56 /

u. son. a 

PicoparU.es 

a. Tatar«: 

b. Depth: 

ARACTERISTICS 

topsail 

subsoil 

peatsoil 

c. Drainage: 

d. Ezcfa. K: topsoil 

subsoil 


subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 


1. Acid solpb. pot.: 

m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAS/PfiOFILE: 

21. L.O. nPATM«CB- 

22. SLOPE: 

23. SLOPE OISTB.: 


25. TBBBAT»- 

26. C8ESÏ/BIDGES: 

27. TAUET FLOOR: 

28. LAB) FACETS: 

29. IBAOfDRATIOJ: 

30. BEUABILITT: 

lO.b : 1 12.a: 2 

j: 2 19: 2 

Dominant > SOZ 

fine 

fine 

very deep 

Well drained 

very high 

very high 

very high 

very high 

Olsen 

very high 

low 

very high 

very high 

medium 

medium 

neutral 


very low 

very low 

125 cm 

1.4 

11.3 

1 

Associated 1 

medium 

fine 

mod. shallow 

Well drained 

very high 

very high 

Olsen 

high 

medium 

high 

high 

neutral 

neutral 

50 cm 

4.7 

0.0 

0 

Associated 2 

fine 

fine 

very deep 


very low 

low 

very low 

very low 

Olsen 

high' 

high 

very high 

very high 

high 

high 


neutral 

very low 

very low 

60 cm 

0.9 

18.2 

1 

150 m Miniann: 20 m Bange: 75 m 

: non-linear and random > 60Z of area flat-topped 






Valleybottens: 5 X 

Interfluves : O-8Z:60 % 

a. Anplitode: medium 

Rolling 9-151, 0-50 m 




-1- Interfluves, dystropepts, 60Ï 

—i.- Intertiuves, napludalfs, 35Z 

-3- Valley bottoms, tropaquepts, 5% 

-4- 

Valleys: Intexfluves: Medium blocks 

1= reliable, 2= probable, 3= tenable. 

14.a: 1 14.b: 1 17: 2 18.a: 1 

22: 2 23: 3 24: 2 28: 2 




9-251: 35 Ï, 25-55Z: 0 I 


4= plausible 

18.b: 2 18.c: 

29: 2 


31. ADDITIGBAL BOTES: Representative profile for Hapludalfs is .extrapolated from Vb.2.2.1 

1110 - 94

mo mn REPORT LREP-SDBM, CSR-BOGGR 

1. LARD HOTT: Vb.2.3.2 

B1OCX DIAGRAM: CBCSS SECTION: 

4. OCCQREBCE by PBOVIHCE: 

5. Slams IDESTIFXERS : Updated by: DR edit date: 01/06/89 Status: Final 

6. LAUD OBIT DESCHIPTIGH: Moderately dissected rolling volcanic plain,intermediate and 

7. SATWT X.I TV. 

8. AEBTAI. PHOTOGRAPHS 

9. RADAR 


a. Heatbering 

b. Litbology 

c. Formation 


13. FISHERIES 

b. Source 


b_ Tf •••Hat-ion 

15. VESETAIICH/LABD OSE 

16. 

Area used 

-BBATfBI EROSIOH 

a. Occurence 

b. Evidence 

17. SOU. GSEAT GSOOP 

Damnant >50X 

Associated 1 

Associated 2 

Lampung: 99% 

2. MAP SWEET- 1110- 3. AREA: 151 km2 

mafic lavas, slopes 8-1531 

123/64/14/11/84 

1:100.000 62 /8282-063, 60 /8295-017, 60 /8295-15 

Star-I/250/88/1110-5,6 

Partial 

basalt 

Qb 

32. REPBESEBTATIVE PROFILES: 

Fresh 


None 

None 


, alang-alang, upland crops, mixed gardens of fruit trees, rainfed 

wetland rice, clove (cengkeh), coffee (kopi), towns, villages 

100 X 

Common 

Gulleys 


dystropepts 

hapludalfs 

tropaquepts 

ity/ /86-14 /81/NS/1110/53/ /22 / 

iqt/ /84-11 /86/DK/1110/53/ /21a/ 

1110 - 95 

Z of area 

50 X 

40 X 

10 X 

Lab. checked 

yes 

yes 

yes 

ada/ /341-56 /72/DR/1110/51/ /56 /


Fcoperti.es 


subsoil 


•innrainoil 

c. Drainage: 


subsoil 

«. TUMUL atcu: copsoxx 

subsoil 


topsoil 

subsoil 


subsoil 

fa. ŒC pH 7 topsoil 

subsoil 


subsoil 


subsoil 



m. Salinity : 


o. Root obstx. layer : 


q. TEB : 


19. ALTITUDE: 

20. PLAB/ÏBOFILE: 

21. L.U. TtP*TM«CT- 

22. SLOPE: 

23. SUSE DISTR. : 


25. TEPBATM- 

26. 


in um »irrig. 

29. FRACMERAITOB: 


lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 


fine 

fine 

~ 

very deep 

Well drained 

medium 

low 

mgn 

medium 

— 

-medium 

medium 

low 

low 

strong acid 


— 

-- 

— 

— 

-- 

-- 

-- . 

2.2 

7.5 

1 

Associated 1 

medium 

fine 

— 

mod. shallow 

Well drained 

-- 

— 

very high 

very high 

Olsen 

high 

medium 

high 

high 

-- 

-neutral 

neutral 

— 

-- 

— 

— 

— 

— 

50 cm 

4.7 

0.0 

0 

Associated 2 

fine 

fine 

— 

very deep 

Irrigated 

very low 

very low 

very low 

very low 

Bray I 

very low 

very low 

very low 

very low 

high 

very high 

slightly acid 

slightly acid 

very low 

very low 

— 

— 

— 

110 cm 

0.6 

33.9 

2 

100 m Minim- 25 m Bange: 50 m 

: non-linear and random 40-60Z of area flat-topped 

Included: 









ValleybottOBs: 10 X 

xnterCLoves : 0-81:60 X, 9-2SZ: 30 I, 25-551: 0 X 

a. Aaplitode: medium 


Rolling 9-15X, 0-50 


b. Length:Short c. Variability: Low 



-2- Interfluves, hapludalfs, 40Z 

-3- Valleys, tropaquepts, 10Ï 

-4- 

Valleys: Small blocks Interümves: Medium blocks 

1- reliable, 2° probable, 3- tenable, 

14.a: 1 14.b: 1 17: 1 18.a: 1 

22: 2 23: 2 24: 2 28: 3 

31. ADDITIGBAL KITES: Hapludalfs transpered from Vb.2.2.1 

1110 - 96 

4- plausible 

18.b: 1 18.c: 

29: 2

LARD miT REPOST LBEP-SDBf, CSR-BCGGK 

1. LAND DIBIT: Vb. 2. 6. 2 

BLOCK DIAGRAM: CBQSS SECTI08: 

4. •»i:iiiimrpiql-fi by ÎBEWIBCE: 

5. STATUS XDEHTIPXEBS 

V.2.10.2 

V.2.6.2 V.2.2.1 

6. LAHD OBIT DESC8IPTIQB: Moderately dissected rolling volcanic plain with hillock,intermediate 

7. SATELLITE 

8. AESIAL PH0T0G8APBS : 

9. BADAR : 

10. PAKHOT MUEBIAL 

a. Hn.iUmri ÛIIH : 


c Foiaation : 

12. MâTEH a. Quality : 

b. Source : 

13. FISDEfilES : 

1«. BIVEBS a. Floodrisk : 

b, Innndstion : 

15. WBSEIATICffl/LAHD USE : 

Area used : 

is «n-«T.J!i»»Tinn varszTim 

Lampung: 99% 

2. MAP SHEET: 1110- 3. AREA: 104 km2 • 


and mafic lavas, slopes 8-25Ï. 

123/64/14/11/84 

1:100.000 61 /8344-191, 62 /8282-69 , 61 /8344-193 

Star-I/250/88/1110-6 

High 

basalt 

Qb 

Fresh 


None 

None 

a. Occurence : Common 


17. SOIL G8EAT GBD0P : 

Dominant >50Z 

Associated 1 

Associated 2 

32. REfHESEHI&TIVE FBOFILES: 

11. BOCK GOTCSOP: S Z 

, alang-alang, upland crops, mixed gardens of fruit trees, clove 

(cengkeh), coconut (kelapa) 

100 X 


eutropepts 

hapludalfs 

Z of area 

80 X 

20 X 

X 

Lab. checked 

ite/ /84-9 /86/DK/1110/53/ /19a/ ada/ /341-87 /72/IS/1110/53/ /47 / 

1110 - 97 

yes 

yes

18. SOIL CBABACTERISnCS 


stsbsoïl 


•dneralsoil 

c. Drainage: 


subsoil 


fine 

fine 

deep 

Well drained 

very high 

high 

subsoil high 

t. Avail. F: Method Olsen 

topsoil low 

subsoil very low 

g. Total P: topsoil very high 

subsoil very high 

h. CEC pB 7 topsoil medium 

subsoil medium 

i. Soil Reaction:topsoil neutral 

sobsoil neutral 


sdbsoil 

k. Al tozicity : 

1. Acid snlpb. pot.: 

m. Salinity : 


o. Boot obstr. layer : 78 cm 

p. Organic Matter : 1.4 

q. TEB : 9.2 

r. Total observations: S 

19. ALTITUDE: 

20. PIAW/IBDFTLE: 

21. L.D. IttATMGB: 

22. SLOPS: 


24. RELIEF AMPLI. : 

25. 

26. 


28. IAD FACETS: 

29. 

Associated 1 

fine 

fine 

very deep 


high 

Olsen 

high 

medium 

medium 

high 

moderately alkaline 

neutral 

100 cm 

1.3 

0.0 

1 

Associated 2 

0.0 

0.0 

0 

MaxüaB: 230 m tfinin: 40 m Range: ISO m 

Pnrinmt: non-linear and random 40-601 of area flat-topped 

Included: non-linear and random > 60% of area crested/peaked 






ValleybottOBs: S X 

Interfauves : 0-8Z:60 X, 9-251: 30 

a. Aaplitode: medium 




d. Hidth: moderate e. Variability: Low 

a. Hidth: 


-1- Rounded top/crest, mihrori 

-2- Hillock part, eutropepts, 30X 

-3- Slopping, hapludalfs, 20Ï 

-4- 

Valleys: Interflaves: Medium blocks 

30. RELIABILIT7: 1« reliable, 2- probable, 3° tenable, 

10.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 

31. ADDITIOML BOTES: 

1110 - 98 




X, 25-551: 5 * 


4- plausible 

18.b: 2 18.c: 1 

29: 2 

c. Variability: Low

Lernt mai REPOST IBEP-SD3M, CSB.-BCGQR 

BLOCK DIAGSâM: 

ï. Laan rani: vb.2.9.1 

4. OCOTREKEE by HMWTflCE: 

5. STATUS ŒESTIFIEBS : 

6. LAMB OBIXT DESCKIPTICBI: 

7. 

8. 

Lampung: 99% 

2. MAP SHEET: 1110- 3. AREA 43 km2 


Slightly dissected lahars,intermediate and mafic lavas,slopes 

3-15X. 

9. BADAR 

10. PAHFNT MATKRTAT- 

: Star-I/250/88/1110-5,6 

13. FISHERIES : None 



15. VBSETATIQH/LAHD OSE : , bush, alang-alang, mixed gardens of fruit trees, upland crops 

16. 

SATELLITE âiifuMnjS ; 123/64/14/11/84, 

AERIAL FBDTOG8APBS : .1:100.000 62 /8282-67 


b. Lithology : basalt 

c. Formation : Qb 


b. Source : Rain, Not known 

Area used : 

AfTTTt TOATmn mmîim 

a. Occuremce : 

b. Evidence : 

17. SOIL GSEAT GKOTP : 

Dominant >50Z 

Associated 1 

Associated 2 

10 X 

Localised 

We • - -. 

Classification 'Z of area Lab. checked 

troporthents 

eutropepts 

1110 - 99 

11. BOCK OOTCSOP: 35 X 

55 Z no ' 

10 % no 

X


Properties 

a. Texture: 

b. Depth: 

topsoil 

subsoil 

peatsoil 

c. Drainage: 


subsoil 

f. Avail. P: 

8- Total P: 

h. CEC pH 7 

subsoil 

method 

topsoil 

subsoil 

topsoil 

subsoil 

topsoil 

subsoil 

i. Soil Réaction:topsoil 

subsoil 


subsoil 


1. Acid smlph. pot.: 

n. Salinity : 




q. TEB : 

x. Total observations: 

19. ALTITUDE: 

20. FLAH/ÎBQFILE: 

21. L.O. IBALBflGE: 

22. SLOPE: 


24. RELIEF AHPLI.: 

25. TEBKAIB: 

26. 

27. TAUET FLOOR: 


29. FRAGMESTATIGH: 

Drainant > 501 Associated 1 Associated 2 

0.0 

0.0 

0 

0.0 

0.0 

0 

120 m MiniraraB: 30 m Range: 70 m 

t: non-linear and random 40-60% of area flat-topped 

Included: 




c. Length: short . d. Variability: Low 


Valleybottass: 5 X 

Interflaves : 0-81:60 X, 9-251: 30 X. 25-55X: 0 X. >55Z: 5 X 

a. Amplitude: low b. Variability: Low 

Undulating 2- SX, 0-50 in 

a. Shape: no crests b. Length: c. Variability: 


a. Width: b. Variability: 

-1- Flat & rounded top. trooorthents. 55% 

-2- Gentle sloping, eutropepts, 10% 

"3- Rock outcrops, 35% 

-4- 

VaUeys: Interflaves: Medium blocks 

30. RELIABILITY: 1= reliable, 2° probable, 3= tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 3 18.a: 3 18.b: 2 18.c: 

18.d-ij: 3 19: 2 22: 2 23: 3 24: 2 28: 3 29: 3 

31. ADDITIQBAL BOTES: 

1110 - 100 

0.0 

0.0 

0

LARD OBIT REPORT LREP-SDBM, CSR-BGGGR 

1. LAHD mit: Vb.2.10.2 

BLOCK DIAG8AM: CROSS SECTIC«: 

4. OCCORESCE by PRCVŒCE: Lampung: 99% 

s. STATUS 

6. LARD OBIT 

7. SATELLITE 

8. AFPTA1L W tot MJPAHtK 

9. BADAR 

10. FAREBT MltTIWTAT. 

a. Heathecrng 

b. Litbologjr 

c. Formation 

12. MATER a. Quality 

13. FISHERIES 

b. Source 


b. Iimndati.aii 

15. VEGETATXGH/LAHD OSE 

16. 

Area used : 

AlV'KIIJRDATtqi 1?Rfff>TflflV 


b. Evidence : 

17. SOU. GREAT G8ODP 

Donnant >50t 

Associated 1 

Associated 2 


Opdated by: DR edit; date: 02/06/89 Status: Final 

Moderately dissected eroded volcanoes,intermediate and mafic 

lavas, hilly relief, slopes (15-30Ï). 

123/64/14/11/84 

1:100.000 61 /8344-195 

Star-I/250/88/1110-5 

Partial 

basalt 

Qb 

32. REERESEHTATIVE FKDFTLES: 

Fresh 

Rain 

None 

None 

None 

11. ROCK OOTCSOT: 20 2 

moist primary lowland forest, upland crops, reafforestation, 


40 X 

Common 

Gulleys 


kandiudults 

humitropepts 

Z of area 

60 X 

20 X 

I 

Lab. checked 

udk/ /86-13 /81/NS/1110/51/ /20 / ith/ /341-57 /72/DR/1110/51/ /57 / 

1110 - 101. 

yes 

yes

18. SOIL CBABACTEBISTICS 

Properties 

a. Texture: topsoll 

subsoil 


c. Drainage: 

d. Each. K: topsoll 

subsoil 

e. Total K2O: topsoll 

subsoil 

t. Avail. P: aathod 

topsoil 

subsoil 


subsoil 

h. CBC pH 7 topsoil 

subsoil 

1. Soil Reaction:topsoil 

subsoil 

i. Al Sat. topsoil 

subsoil 







q. TEB : 


19. ALTITUDE: 


21. L.U. 

22. SLOPE: 



25. TEBBATM- 

26. 



29. FfittGMERTATIOfl: 

30. REUABILm: 

lO.b : 2 12.a: 2 

18.d-q: 2 19: 2 

31. ADDTTIOBAL KITES: 

Donnant > SOX 

fine 

fine 

very deep 

Well drained 

very low 

very low 

very low 

very low 

very high 

very high 

low 

low 


strong acid 

1.6 

5.8 

0 

Associated 1 


fine 

deep 

Well drained 

verv hieh 

medium 

high 

high 


neutral 

100 cm 

4.3 

0.0 

0 

0.0 

0.0 

0 

elated 2 

290 m Htoimm: 25 m Range: 203 m 

Donnant: non-linear and random > 60Z of area crested/peaked 

Inclnded: 

a. Pattern: radial b. density: Moderate 




e. Curvatsre: convex 

Valleybottoas: Z 

Interdaves : 0-81:30 Z, 

a. flfl 11 mil» medium 

hillocKy >16Ï, 0-50 ra 


d. Hidtb: moderate 

a. Hidtb: 

b. Variability: High 


9-2SX: 50 Z, 25-55X: 20 Z 



e. Variability: Low 


-1- Upper & middle slopes, kandiudults, 60Z 

-2- Lower slopes, humitropepts, 20Z 

-3- Rock outcrops, 20Z 

-4- 

Valleys: Interxlnves: Small blocks 

1» reliable, 2- probable, 3» tenable, 

14.a: 1 14.b: 1 17: 1 18.a: 2 

22: 2 23: 2 24: 2 28: 3 

1110 - 102 

c. Variability: Medium 

•= plausible 

18.b: 2 18.c: 1 

29: 2

LUD OBIT HEPCRT LREP-SDBM, CSR-BOGOR 

1. LAHD OBIT: H.-.b . 1. 2 . 1 

4. OCCuREHCE by HKXTDCE: 

5. SUIDS IDEHTIFIE8S : 

6. LAHD OBIT DESCRIFTIOH: 

7. SATELLITE SCUTES : 

8. ÀTOTAI. HKJTOGRAPBS : 

9. RADAR : 

10. BARER MATERIAL 

HAP BUGE: CSOSS SECTICS: 

H.I.2.1 H.I.5.2 H.I.6.3 

"volcanic rocks ''* 


b. Lithology : andesitic tuffs, basalt, 






b _ Inundation : None 

15. TEGEIATIOB/LAHD USE : 

Area used : 

16. ACCELERATED ERCGIGH 

17. SOIL GREAT GBODP 

Lampung: 99% 



Dominant >5OI 

Associated 1 

Associated 2 




netaDorphic - 

; rocks 

Slightly dissected hills,intermediate and mafic tuffs and lavas, 

moderately steep slopes (16-30%) 

123/64/14/11/8« 

1:100.000 57 /8292-075, 62 /8282-77 , 60 /8295-05

1« «»ITT. PHAPATTFUTSTT'-'S 

Properties 

Dominant > SOZ 

a. Texture: topsoil fine 

subsoil fine 


-- 

mineralsoil very deep 

c. Drainage: 

Well drained 

d. Erch. K: topsoil »medium 

subsoil low 

e. Total K2O: topsoil medium 


t. Avail. P: method Bray I . 

topsoil very low 


g. Total P: topsoil low 

subsoil low 

h. CSC pH 7 topsoil high 

subsoil high 

i. Soil Reaction:topsoil very strong acid 

subsoil excessive acid 

j. Al Sat. topsoil very low 

subsoil high 


no 


-- 

m. Salinity : 

-- 


-- 

o. Boot obstr. layer : 120 cm 

p. Organic Matter : 1.9 

q. TEB : 

3.1 

r. Total observations: 0 

19. ALTITUDE: 

20. PLAI/PBOFILE: 

21. L.O. 

22. SLOPE: 



23. TWmATW- 




29. FRAGMEBTATIC«: 

Associated 1 

fine 

fine 

— 

very deep 

Well drained 

— 

— 

high 

very low 

Olsen 

low 

very low 

medium 

low 

-- 

— 

slightly acid 

neutral 

-- 

-- 

— 

-- 

-- 

-- 

62 cm 

3.1 

0.0 

1 

Associated 2 


fine 

— 

very deep 

Well drained 

medium 

_.JJ 

low 

medium 

Bray I 

very low 

very low 

medium 

medium 

medium 

high 

strong acid 

strong acid 

very low 

very low 

— 

-- 

-- 

-lio 

cm 

4.6 

9.8 

0 

290 m Mrnixn: 25 m Bange: 75 m 

Dominant: non-linear and random 40-60X of area crested/peaked 

Included: non-linear and random < 40X of area flat-topped 



a. Steepness:mod. steep. 



Vallevbottons: 5 X 

Intarfluves : 0-81:20 X 

a. Amplitude: high 

Hilly >16Z,51-300m 



a. Width: very narrow 

—1- Crests & upper slopes, dystropepts, 75Z 

-2- Middle slopes, hapludults, 20Ï 

-3- Lower slopes/valleys, humitropepts, 5Ï 

-4- 




, 9-25X: 60 X. 25-551: 15 X 



e. Variability: Medium 


30. RELIABILITY: 1- reliable, 2= probable, 3- tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 1 18.b: 1 18.c: 2 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITIOSAL BOTES: Representative profile for Dystropepts and Humitropepts are extrap 

olated from sheet 1010 (Hab.1.3.3). 

1110 - 104

LAUD UHIT REPORT LREP-SDB4, CSR-BOGOR 

1. LftHD UHIT: Htn.1.2.2 

MAP DÜGE: CSGSS SECTIOH: 

4. nrrm»W-E by PROVIHCE: 

5. STATUS IDE9TIFIERS : 

6. LAID DBIT DESCHIPTIOB: 

V.l.4.2 

B.I.2.2 

«etaiiorpbic rocks _ " C *^N 

A.2.2.1 

7. SATELLITE SCEHES 

slopes (16-30%). 

: 123/64/14/11/84, 

8. AERIAL PHOTOGKAPBS : 1:100.000 57 /8292-083, 

9. RADAR : Star-I/250/é8/1110-3 

10. BARER HATERIAL 

a. Heatherins : Partial 

b. Lithology : gneiss, schists, 

c. Formation : Ptse , 







15. VBSETAÏIGH/LAHD OSE : , bush, upland crops, mixed gardens of fruit trees, rubber (karet) 

Area used 

16. ACCELERATED EROSIOH 

: 75 % 

17. SOIL GSEAT G8OUP 



Dominant >50Z 

Associated 1 

Associated 2 

32. REPRESEaTATIVE PROFILES: 


Lampung: 99Ï 


Moderately dissected hills,metamorphic rocks,moderatelly steep 


dystropepts 

kanhapludults 

Z of area 

75 X 

20 X 

X 

Lab. checked 

yes 

ity/ /340-16 /71/DN/1110/42/ /80 / udh/ /340-14 /71/SK/1110/42/ /45 / 

1110 - 105 

yes 

rosï'

18. gnTi CHaBACTEBZSTICS 

Properties 

a. Taxtaxe: topsoil 

sabsoil 


•ineralsoil 

c. Drainage: 


sabsoil 

«j. xocai. BMtz rapsoix 

sabsoil 

t. Avail. P: aethod 

topsoil 

sabsoil 


sabsoil 


sabsoil 


sabsoil 

j. AI Sat. topsoil 

sabsoil 


1. Acid salpta. pot.: 





q. TEB : 


19. ALTITUDE: 

20. PLAH/PfiOFILE: 

21. L.D. DRAJHAGE: 

22. SLOPE: 

23. SLOPE DISTfi.: 


25. TBHBATW- 



29. FRftGMBrnTIOB: 

Daninant > SOX 

fine 

fine 

deep 

Well drained 

medium 

medium 

nign 

medium 

medium 

low 

low 

low 

moderately 

moderately 

80 cm 

1.2 

5.1 

1 

acid 

acid 

• 

Associated 1 

medium 

medium 

deep 

Well drained 

-- 

— 

very high 

very high 

mediummedium 

-- 


neutral 

80 cm 

'1.3 

0.0 

1 

Associated 2 

0.0 

0.0 

0 

250 m Minis«: 100 m Range: 150 m 

Dominant: non-linear and random > 60Ï of area crested/peaked 

Included: 



a. Steepness:mod. steep 

•:. Length: short 


Valleybottons: X 

Interfluves : 0-81:10 X 




hillocKy >16*, 0-50 m 

a. Shape:' Irregular b. Length:Short c. Variability: High 

d. Hidth: moderate e. Variability: Medium 

a. Hidth: 


—1— Crost up óc luw sïlup is, dystropepts, 75% 

-2- Middle slopes, kanhapludults, 20Ï 

-3- 

-4- 

Valleys: Interfluves: Small bloclts 



, 9-25X: 60 X, 25-551: 20 X. >55X: 10 Ï 

30. RELIABILITY: 1- reliable. 2» probable, 3= tenable, 4-= plausible 

lO.b : 2 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 2 18.b: 1 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITIONAL BOTES: 

1110 - 106

LAND UHIT REPORT LREP-SDBM, CSR-BO3OR 

1. LAUD UHIT: Hab.1.3.3 

«. OOCUREHCE by PROVINCE: 

MAP IMAGE: SECTION: 

B.7 

coconut 

~-' if cor3l fragnenls 

E.l.3.3 

/y volcanic rocks : 

5. STATUS IDEHTIFIEBS : Updated by: DR edit date: 03/06/89 Status: Final 

6. LAND DBIT DESCRIPTION: 

7. SATELLITE SCENES : 123/64/14/11/84 

b. Lithology : andesitic tuffs, basalt, 






b. Inundation : None 

H.1.2.2 

•V-T «etatorphic rocks - -^c- "" x' 

15. VEGEIATIOH/LAND OSE : secondary forest, alang-alang, shifting cultivation, upland crops, 


16. ACCELERATED EROSION 

a. Occurence : Extensive 

b. Evidence 

Lampung: 99% 

2. HAP SHEET: 1110- 3. AREA: 121 kmZ 

Strongly dissected hills intermediate and mafic tuffs and lavas, 

steep to very steep slopes (30-75%). 

8. AfiHTAI. PHOTOGRAPHS : 1:100.000 60 /8295-005, 58 /8292-65 , 62 /8282-77 

9. RADAR : Star-I/250/88/1110-2,3 

10. FÄRBST MATERIAL 

a. Heatherin« : Partial 



Dominant >5OI 

Associated 1 

Associated 2 


mixed gardens of fruit trees, clove (cengkeh), coffee (kopi) 

Various 


dystropept:; 

hapludults 

hiunitropepts 

ity/ /340-10 /71/SK/1110/ / /26a/ 

ith/ / /87/HK/1010/ / /22 / 

1110 - 107 

Z of area 

55 % 

35 % 

10 % 

Lab. checked 

yes 

yes 

yes 

uda/ /184-16 /68/IS/1110/ / /96 /

IR snn rHABArrrT 501 

fine 

fine 

-deep 

Well drained 

high 

medium 

medium 

low 

-- 

-very 

high 

high 

medium 

low 

slightly acid 

strong acid 

— 

-- 

-- 

— 

— 

-- 

60 cm 

1.4 

0.0 

1 

Associated 1 

medium 

fine 

— 


Well drained 

— 

-very 

high 

low 

— 

-very 

high 

medium 

-- 

-moderately 

acid 


— 

-- 

-- 

— 

-- 

— 

50 cm 

3.6 

0.0 

1 

Associated 2 


fine 

-- 

- - very deep 

Well drained 

medium 

medium 

low 

medium 

Bray I 

very low 

very low 

medium 

medium 

medium 

high 

strong acid 

strong acid 

very low 

very low 

-- 

— 

-- 

-- 

110 cm 

4.6 

0.0 

0 

300 m Minim«: 15 m Range: 250 m 

Dominant: non-linear and random > 60% of area crested/peaked 

Included: 

a. Pattern: dendritic . b. density: Mod. high 


a. Steepness:very steep b. Variability: Medium 

c. Length: moderate d. Variability: High 



Interfluves : 0-8Z:0 X, 9-251: 20 X. 25-551: 30 X, >55X: 40 X 

a. A^litnde: high b. Variability: Medium 

Hilly >165;,51-300m 


d. Width: moderate e. Variability: High 


-1- Crests & upper slopes, dystropepts, 55? 

-2— Miùdlw siopes, hapiuduits, 35Ï 

-3- Lw. slope & VI. bottom, humitropepts, 10Ï 

-4- 

Valleys: Interfluves: 

30. RELIABILITY: 1= reliable, 2« probable, 3= tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 1 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADDITIOBAL BOTES: Representative profiles for Humitropepl.; 

Sheet (KotaAgung.Hab.1.3. 3). 

1110 - 108 

is extrapolated frum other

LAND OBIT REPCBT LREP-SBBM, CSR-BOGOB 

MAP IMAGE: CBOSS SBCTICH: 

1. LAHB OHIT: dHab . 1. 3 . 3 

• . OCCHRERCE by PROVHBCE: Lampung: 99% 

A.2.2.1 

(iH.1.3.3 

/;- r "tùff cover ~'!*$••* 

volcanic rocks 

H.1.3.3 

5. STATUS EDEHTIFIERS : Updated by: DR edit date: 03/06/89 Status: Final 

6. LAHD OBIT DESCSIFTIC8: Strongly dissected hills,intermediate and mafic tuffs and lavas 


8. ABBTAH- PHOTOGRAPHS : 

9. RABAR : 





12. HATER a. Qnal: ty : 





15. VBSETATICS/LAHD USE : moist primary lowland forest, alang-alang, shifting cultivation, 

Area used : 



b. Evidence 

17. SOIL GREAT GBOOP 

Dominant >SOZ 

Associated 1 

Associated 2 



covered by acid tuffs, steep to very steep slopes (30-75%) 

123/64/14/11/84 

1:100.000 62 /8282-7S 

Star-I/250/88/1110-1 

High 

andesitic tuffs, basalt, dacite 

Fresh 

None 

mixed gardens of fruit trees, clove (cengkeh) 

60 % 

Extensive 

Various 


dystropepts 

hapludults 

humitropepts 

ity/ /.340-10 /71/SK/1110/ / /26a/ 

1110 - 109 

Z of area 

50 % 

30 % 

10 % 

11. BOX OOTCBQP: 10 % 

Lab. checked 

yes 

yes 

no

Properties 


subsoil 


•inATÎ 

«ni 1 

c. Drainage: 


subsoil 


f. Avail. P: •nthnri 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 

J. Al Sat. topsoil 

subsoil 


1. Acid sulph. 

pot.: 

m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FL&H/FKOFILE: 

21. L.B. DKaHUGE: 

22. SLOPE: 

23. SLOPE DIST&-: 

24. RELIEF «HPLI.: 

25. TEKBAIH: 

26. C8EST/RIDSES: 


28. LARD FACETS: . 

29. FRAGMEn&TIOR: 

30. RELIABILITST: 

10.b : 1 12.a: 2 

18.d-q: 2 19: 2 


fine 

fine 

— 

deep 

Well drained 

high 

medium 

medium 

— 

— 

very high 

high 

medium 

low 

slightly acid 

strong acid 

— 

-- 

— 

— 

— 

-- 

60 cm 

1.4 

0.0 

0 

Associated 1 


fine 

— 

deerj 

Well drained 

very low 

very low 

very low 

very low 

very low 

very low 

low 

very low 

medium 

low 



— 

-- 

-- 

-- 

— 

-- 

-- 

0.0 

0.0 

0 

Associated 2 

0.0 

0.0 

0 

150 m Minima: 25 m Range: 75 m. 

Damnant: non-linear and random > 601 of area crested/peaked 

Included: 



a. Steepness:very steep 



Valleybottoas: 10 Z 

Interflnves : O-8X:0 X 

a. A^litode: high 

Hilly >16%,51-300m 

a. Shape: Irregular b. Length:Short 

d. Hidtb: moderate e. Variability: High 


-1- Crests & upper slopes, dystropepts, 50Ï 

-2- slope plt:dult= 

-3- Lw. slope & VI. bottom, humitropepts, 10% 

-4- 

Valleys: Interdnves : 

1» reliable, Z= probable, 3= tenable, 

14.a: 1 14.b: 1 17: 2 18.a: 2 

22: 2 23: 2 24: 2 28: 2 




9-25X: 20 *, 25-551: 30 X. >55Z: 40 X 


4** plausible 

18.b: 2 18.c: 1 

29: 2 

c. Variability: High 

31. ADDITIOHAL ROTES: Representative profiles for Dystropepts is extrapolated from Hb.l. 

3.3. Hapludults extrapolation based on RePPProt (Land System BMS). 

1110 - 110

itm on HEKST 

1. LAID OBIT: Hb.1.3.3 

4* 

5. 

MAP IMAGE: CROSS SECTIOH: 

STATUS HUHTliTEBS 

6. LAID OBIT DESCRIPTIOB 

7. SATELLITE SCEHES 

8. AERIAL PBDI0G8APBS 

9. PATmp 

10. mwPWT MATKRTAT. 

a. Weathering 

b. Litbology 

c. Formation 

12. HATES a. Quality 

b. Source 

13. FISHERIES 

1*. RIVERS a. Floodrisk 

*». Tnumliiti on 

15. VBSETATICII/LAHD OSE 

Area used 

16. 

a. Occurence 

b. Evidence 

17. SOU. GSEAT G80DP 

Dcadnant >50X 

Associated 1 

Associated 2 

T ^...L. n • Q ^ ^/ 

L


Properties 


subsoil 


Bineraisoil 

c. Drainage: 

d. fitch. K: topsoil 

subsoil 


subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 



p. Qrgaaic Matter : 

q. TEB : 


19. ALTITUDE: 

20. FLAH/PROFILE: 

21. L.Ü. DRAIBAGE: 

22. SLOPE: 



25. TfnntATU- 




29. FRAOŒHTATI0H: 


fine 

fine 

— 


Well drained , 

low 

low 

low 

low 

Bray I 

very low 

very low 

medium 

medium 

medium 

low 

strong acid 


high 

very high 

yes 

-- 

-- 

-- 

67 cm 

1/8 

2.6 

0 

Associated 1 

fine 

fine 

— 

very deep 

Well drained 

low 

low 

low 

very low 

Bray I 

very low 

very low 

low 

very low 

medium 

high 



medium 

medium 

yes 

-- 

-- 

-- 

142 cm 

2.1 

8.0 

0 

Associated 2 

fine 

fine 

— 

very deep 

Well drained 

very low 

very low 

low 

very low 

very low 

very low 

low 

very low 

medium 

low 



very high 

very high 

-- 

-- 

-- 

— 

0.0 

0.0 

0 

Maxima: 350 m Minimum: 25 m Range: 300 m 


Included: 

a. Pattern: dendritic b. density: Mod. high 






Interfluves : 0-8Z:0 X, 


Hilly >16%,51-300m 




-1- Crests S. upper slopes, dystropepts, 55% 

-2- Middle slopes, hapludults, 35% 

-3- Lw. slope & VI. bottom, humitropepts, 10% 

-4- 




9-25Z: 20 X, 25-551: 30 X, >55Z: 40 X 


b. Length:Shurt 

30. RELIABILITY: 1= reliable, 2= probable, 3= tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 3 


31. ADDITIONAL BOTES: Humitropepts extrapolation based on RePPProt (LS BB6). Dystropepts 

and Hapludults extrapolation based on L U Hb.1.3.3 .sheet 1010. 

1110 - 112

AID OBIT REPORT LREP-SDHM, CSR-BOBOR 


1. LARD OBIT: Hd.1.3.3 2. MAP SHEET: 1110 

CE by PROVINCE: Lampung: 99% 

H.1.3.3 1.1.3.3 

3. AREA: 26 km2 

5. SIATOS IDERTIFIERS : Updated by: DR edit date:, 03/06/89 Status: Final 

H.2.2.3 

leid tuff*«* tolcamc rocc 

6. LARD DRIT DESCRIPTION: Strongly dissected hills,acid tuffs,steep to very steep slopes 

(30-75%) 

7. SATELLITE SCEHES : 123/64/14/11/84 

8. AERIAL PHOTOGRAPHS : 1:100.000 58 /8292-69 , 57 /8292-73 

9. RADAR : Star-I/250/88/1110-1,2 

10. PAREHT MATERIAL 11. ROCK OUTCROP: 10 % 


b. Lithology : dacite 

c. Formation : Tmda 




14. RIVERS'a. Floodrisk : None 

^) • • tmmifltri OP * Noïi6 

15. VEGEIAnOR/LARD USE : secondary forest, bush, banana, clove (cengkeh) 




17. SOIL G8EAT GSOOP : 

Dominant >50Z 

Associated 1 

Associated 2 


Extensive 


dystropepts 

hapludults 

ity/ / /87/HJ/1010/52/ /06 / 

1110 - 113 

X of area 

60 X 

30 % 

Lab. checked 

yes 

yes


Properties 


subsoil 


c. Drainage: 

mineralsoil 


subsoil 


subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 



subsoil 


m. Salinity : 




q. TEB : 


19. ALTITUDE: 


21. L.D. DBAHUGE: 

22. SLOPE: 



25. TEHRAIH: 




29. FBAGMEBTATIOH: 


lO.b : 1 12.a: 2 

18.d-q: 3 19: 2 


fine 

fine 

very deep 

Well drained 

high 

medium 

medium 

low 

Bray I 

very low 

very low 

low 

low 

high 

' — 



very low 

high 

yes 1 

140 cm 

1.8 

2.5 

0 

Associated 1 

fine 

fine 

very deep 

Well drained 

-- 

-low 

low 

low 

-- 

-- 

very low 

low 

very low 

strong acid 


-- 

-- 

— 

0.0 

0.0 

0 

Associated 2 

0.0 

0.0 

375 m Minium: 15 m Range: 350 m 


Included: 






Valleybottoms: % 

Interfluves : 0-81:0 %, 


Hilly >16%,51-300m 


9-25Z: 0 



-1- Crests & upper slopes, dystropepts, 60% 

-2- Middle & lower slopes, hapludults, 'in 

-3- 

-4- 


0 




25-551: 15 %, >55I: 85 % 

b. Variability: Medium. 



14.a: 1 14.b: 1 17: 3 18.a: 2 18.b: 2 18.c: 2 

22: 2 23: 2 24: 2 28: 3 29: 

31. ADDITIORAL BOTES: Representatative profile for Dystropepts is extrapolated from sheet 

1010. Hapludults extrapolation based on RePPProT (Land Sys B6A) 

1110 - 114

LAHD OUT BEEOBT . CSR-BOGGR 

1. LAHD OBIT: Hg.1.3.3 

MAF IMAGE: SECTIOH: 

4. OCCOREHCE by FROVIHCE: 

A.2.2.1 

H.l.3.3 

* :* '" tiff'cover"ifS? ' 


5. STATUS IDEHTIÏTERS .: Updated by: DR edit date: 03/06/89 Status: Final 

6. LAHD OMIT DESCRIPTICH: 


8. AERIAL PBOTOGKAPBS : 

9. BADAR : 

10. FARE« MATERIAL 


b. LAthology : granite 

c. Formation : Kgr 

12. MATER a. Quality : Fresh 





15. VEGETATIOH/LAD) OSE : moist primary lowland forest, bush, alang-alang, shifting cu 

Area used : 20 : 


a. Qccurence : Extensive 

b. Evidence 

17. SOIL GREAT GKODP 

Dominant >50Z 

Associated 1 

Associated 2 

32. REPRESERIATIVE PROFILES: 

2. MAF SHEET: 1110- 3. AREA: 8 km2 

Lampung: 0% 

Strongly dissected hills,acid plutonic rocks,steep to very steep 

slopes(30-75j;) 

123/64/14/11/84 

1:100.000 59 /8292-21 

Star-I/250/88/1110-3 

ltivation, upland crops 

Various 


dystropepts 

hapludults 

troporthents 

Z of area 

65 X 

20 X 

5 X 

11. ROCK OUTCROP: 10 X 

Lab. checked 

yes 

ity/ / /88/ER/1010/24/ /42 / uda/ /86/AH/1010/64/ /7a / 

1110 - 115 

yes 

no

IR snrrf- raAB«rTFBT«rrTr 501 

a. Taxtaxe: topsoil 

subsoil 


•in aralsoil 

c. Drainage: 

d. Erch. K: 

e. xouu. IÔJZ topson 

f. Avail. F: 

8- Total P: 

h. CEE pH 7 

topsoil 

subsoil 

subsoil 

method 

topsoil 

subsoil 

topsoil 

subsoil 

topsoil 

subsoil 


j. Al Sat. 


subsoil 

topsoil 

subsoil 

1. Acid salpfa. . pot. : 

m. Salinity : 


o. Boot obstr.. layer : 


q. TEB : 


fine 

fine 

— 

very deep 

Well drained 

medium 

medium 

medium 

medium 

Bray I 

very low 

very low 

low 

low 

medium 

medium 



very low 

very low 

— 

— 

— 

— 

110 cm 

2.1 

7.0 

0 

Associated 1 

fine 

fine 

deep 

— 

Well drained 

medium 

medium 

medium 

medium 

Bray I 

very low 

very low 

very low 

very low 

low 

medium 



high 

very high 

yes 

— 

— 

-- 

98 cm 

19. ALTITUDE: Maximum: 150 m Minimum: 100 m Range: 125 m 

1.6 

3.4 

0 

Associated 2 

20. PLâH/PHOFILE: Dominant: non-linear and random > 60% of area crested/peaked 

Included: 

21. L.U. DBAIHAGE: a. Pattern: dendritic b. density: Mod. high 


22. SLOPE: a. Steepness:Steep b. Variability: Medium 


a. Curvature: straight 

23. SLOPE DISTH.: Valleybottoms: 5 % 

Interfluves : 0-81:0 X, 9-25X: 10 X, 25-55Z: 40 Z, >55Z: 45 Ï 

24. BELIEF AMFLI.: a. Amplitude: high b. Variability: High 

25. Twraww- Hilly >16Z,51-300m 

26. CSEST/RIDGES: a. Shape: Irregular b. LengttuModerately long c. Variability: Medium 


27. VALLEY FLOOR: a. Width: very narrow b. Variability: Low 

33. T *"* FACETS: ~~ 1~ "ppër «. lowêï àlupoa, uysLrupepLs, 65% 

-2- Middle slopes, hapludults, 20Z 

-3- Crest, troporthents, 5% 

-4- 

29. FBAGMEHTATIOH: Valleys: Interfluves: 

30. BEUABHITY: 1« reliable, 2° probable, 3° tenable, 4« plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 2 

18.d-q: 3 19: 2 22: 2 23: 2 24: 2 28: 3 29: 0 

31. ADDITIGHaL MUTES: Representative profiles are extrapolated from sheet 1010(Hg.1.2.2 

and Hg.1.3.3) 

1110 - 116 

0.0 

0.0 

0

LAID UH1T BEFORT LREP-SDBM, CSR-BOGOR 

1. LAHD OBIT: Htn.1.3.3 

MAP HUGE: CSQSS SBCTIOB: 

4. OOCOBEBCE by FBCVIBCE: 

5. SIATOS IDfflTIFIHSS : 

6. LAH) OBIT DESCSIPTIOB: 

7. SATELLITE SCERES 

8. AERIAL PHOTOGRAPHS 

g. RADAR 

10. PARERT MATERIAL 


13. FISHERIES 

b. Litbology 

c. Formation 

b. Source 

1*. RIVERS a. Floodrisk : None 

b. Immdatioii: 

None 

Area used 

16. Af V'KI.FRATMI HMKÇ|TW 

a. Occorence 

b. Evidence 

: 123/64/14/11/84 

: 1:100.000 60 

: Star-I/250/88/1] 10-3 

: gneiss, schists, 

: Ptse 


: Rain 

: None 

15. VEGEXATiaH/LARD OSE : , bush, alang-alang, alang-al upland crops, banana, clove (cengkeh) 

17. SOIL GREAT GROUP • 

Donnant >SOX 

Associated 1 

Associated 2 

Lampung: 99X 

: 70 Z 


: Extensive 

: Various 

2. MAP SBEET: 1110- 3. AREA: 14 km2 

Updated by: DR edit dat«: 03/06/89 Status: Final 

Strongly dissected hills,metamorphic rocks,steep to very steep 

slopes (30-75Z). 


dystropepts 

kanhapludults 

/8292-005, 

Z of area 

80 Z 

10 Z 

Z 

11. ROCK OUTCROP: 10 Z 

Lab. checked 

yes 

ity/ /340-16 /71/DN/1110/42/ /80 / udh/ /340-14 /71/SK/1110/42/ /45 / 

1110 - 117 

yes


Properties 


subsoil 


- •nneralsoil 

c. Drainase: 


subsoil 

e. lotai uu: topsoix 

subsoil 

t. Avail. F: netfaod 

topsoil 

subsoil 


subsoil 

h. CEC pfl 7 topsoil 

subsoil 


subsoil 


subsoil 


1. Acid snlpfa. pot.: 

a. Salinity : 




q. TEB : 



fine 

fine 

deep 

Well drained 

medium 

medium 

nign 

medium 

medium 

low 

low 

low 

moderately 

moderately 

80 cm 

1.1 

0.0 

0 

acid 

acid 

Associated 1 

medium 

medium 

deep 

Well drained 

— 

— 

very nign 

very high 

medium 

medium 

-- 

— 


neutral 

80 cm 

1.3 

0.0 

0 

Associated 2 

19. ALTITUDE: Maxima»: 270 m Minimi: 10 m Range: 225 m 

20. FLAH/PROFILE: Dominant: non-linear and random > 60Z of area crested/peaked 

Included: 

21. L.0. DRAIHAGE: a. Pattern: dendritic b. density: Mod. high 


22. SLOPE: a. Steepness:very steep b. Variability: High 

c. Length: short d. Variability: High 


23. SLOPE DISTR. : Valleybottoas: 5 X 

Interfluves : O-8Z:0 X, 9-25X: 20 X. 25-55Z: 30 X, >55X: 45 X 

24. RELIEF AMPLI.: a. Asciitode: high b. Variability: Medium 

25. TBMlATli- hillocKy >16X, 0-50 m 

26. CREST/RIDGES: a. Shape: Irregular b. Length:Short c. Variability: Medium 


27. VALLET FLOOR: a. Width: very narrow b. Variability: Low 

-2- Middle & lower slopes, kanhapludults, 10X 

-3- 

-4- 

29. FRAGMEHTATIOH: Valleys: Interfluves: 

0.0 

0.0 

0 

30. RELIABILIR: 1= reliable, 2= probable, 3= tenable, 4** plausible 

10.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 

31. ADOITIQHAL BOTES: All representative profiles are extrapolated from Htn.1.2.2 

1110 - 118

TJIfl LREP-SOBM, CSR-BOSOR 

MàP IMAGE: 

1. LAID DUIT: Hab.1.5.2 

4. nmrow:K by IBuvxauE: 

5. STATUS IDEHTIFIEHS : 

1.6.3 H.l.5.2 H.l.6.3 

Kta»rphic 

6. LAID OHII DESCRIPTIOH: Moderately dissected rolling land with hillocks,intermediate 

and mafic tuffs and lavas, slopes 8-25X. 

7. SATELLITE Mi-Mi «K : 123/64/14/11/84 

8. AERIAL PHOTOGRAPHS : 

9. PAIMP 

10. IHRER 1OTEPTAI 

: Star-I/250/88/1110-2,3 

a. Weathering : Partial 

b. Litbologjr : andesitic tuffs, basalt, 


12. HUER a. Quality : Fresh 


None 



13. VBGEïATICÏI/LAMD OSE : 



a. Occurence : Localised 

b. Evidence 


32. 

ity/ 

Dominant >50Z 

Associated 1 

Associated 2 

HATIVE PROFILES: 


Lampung: 99% 


1:100.000 57 /8292-081, 60 /8295-007 

11. ROCK OUTCROP: I 

, bush, shifting cultivation, upland crops, mixed gardens of 

fruit trees 

Various 


dystropepts 

humitropepts 

Z of area 

70 X 

30 X 

X 

Lab. checked 

yes 

yes 

1.4.2 

qoarse s«diKntary 

/ • /87/HJ/1010/61/ /02 / ith/ /87/ES/1010/54/ /17 / 

1110 - 119


Properties 


subsoil 


•rimraluiil 

c. Drainage: 


subsoil 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/PROFILE: 


22. SLOPE: 



25. TERRAIH: 

26. CSEST/RIDSES: 

27. VALLES FLOOR: 


29. FRAGMEHTATICH: 

Donnant > 501 


fine 

— 

very deep 

Well drained 

very high 

medium 

medium 

Bray I 

very low 

very low 

very low 

very low 

medium 

medium 



very low 

very low 

— 

-- 

— 

— 

140 cm 

2.9 

11.5 

0 

Associated 1 

fine 

fine 

-very 

deep 

Well drained 

low 

low 

very low 

Bray I 

very low 

very low 

medium 

low 

medium 

low 



medium 

high 

yes 

-- 

-- 

-- 

160 cm 

2.7 

1.8 

0 

Associated 2 

0.0 

0.0 

0 

155 m Minimum: 100 m Range: 125 m 

Dominant: non-linear and random 40-60% of area crested/peaked 

Included: 






ValleybotUais: 5 % 

Interfloves : 0-81:10 


Rolling 9-15%, 0-50 m 

a. Shape: Undulating b 

d. Width: moderate e 

a. Width: very narrow b 



9-251: 85 %, 25-55X: 0 % 


Length:Short 



-1- Hilly area&upper slope dystropepts, 70% 

-2- Middle & lower slopes, humitropepts, 30% 

-3- 

-4- 

Valleys: 

Interfluves: Medium blocks 

30. RELIABILITY: 1- reliable, 2= probable, 3» tenable, 4-= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 3 29: 2 

c. Variability: Low 

31. ADDITIOHAL HOTES: Representative profiles are extrapolated from sheet 1010(Hab.1.5.2 

and Hab.1.6.2) 

1110 - 120

LAHD UHU PKW HT LREP-SDBi, CSR-BOGOR 

1. LATO OBIT: Hg.1.5.2 

MAP IMAGE: C8GSS SECTICH: 

4. • »i JI»»J» » by raovnicE 

S. SIAIDS IDEBTIIXffiS 

6. IAHD UBIT DISUUFTIUH 

7. SATELLITE SSOZ 

Associated 1 

Associated 2 

E.l.2.1 H.1.5.2 H.l.6.3 

^ V'' Plutonic roete ^ J . «taWphlc'X 

'"volcanic rocks •' * : . N ^T " rocks 


Lampung: 99% 


Moderatelly dissected rolling land with hillociks.acid plutonic 

rocks, slopes 8-25%. 

123/64/14/11/84, 

1:100.000 59 /8292-021, 

Star-I/250/88/1110-2,3 

11. ROCK OUTC80P: % 

Partial 

granite, 

Kgr 

Fresh 

Rain 

None 

None 

None 

moist primary lowland forest, bush, alang-alang, upland crops, 

clove (cengkeh) 

50 X 

Common 

Gulleys 


dystropepts 

hapludults 

troporthents 

X of area 

75 X 

20 % 

5 X 

Lab. checked 

yes 

yes 

no 

32. REPRESBBIATIVE PROFILES: 

ity/ / /88/ER/1010/24/ /42 / uda/ /86-24 /81/SR/lllO/ / /ll / 

1110 - 121

18. SOIL CBARACTERISTICS 

Properties 


subsoil 


mineralsoil 

c. Drainage: 


subsoil 


subsoil 


topsoil 

subsoil 


subsoil 

h. CEC pfl 7 topsoil 

subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 



22. SLOPE: 



25. TESRA1B: 




29. FRAGMESTATiaW: 


fine 

fine 

very deep 

Well drained 

medium 

medium 

medium 

medium 

Bray I 

very low 

very low 

low 

low 

medium 

medium 



very low 

very low 

110 cm 

2.1 

7.0 

0 

Associated 1 



very deep 

Well drained 

very low 

very low 

very low 

very low 

very low 

very low 

low 

low 

strong acid 

strong acid 

0.9 

3.4 

0 

Associated 2 

0.0 

0.0 

0 

ISO m Minimum: 100 m Range: 125 m 


Included: 



a. Steepness:mod. steep b. Variability: Medium 




Interfluves : 0-81:0 %, 9-25Z: 80 X. 25-551: 15 % 

a. Amplitude: medium b. Variability: High 

Rolling 9-15%, 0-50 m 

a. Shape: Undulating b. Length:Short 

d. Width: narrow e. Variability: 

a. Width: very narrow b. Variability: 

Medium 

Low 

-1- Hilly area&upper slope, dystropepts, 75% 

-Z- Middle slopes, hapiuduits, 2ÙÏ 

-3- Lower slopes, troporthents, 5% 

-4- 


30. RELIABILITY: 1= reliable, 2= probable, 3= tenable, 4= plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 1 

18.d-q: 2 19: 2 22: 2 23: 2 24: 2 28: 2 29: 2 


31. ADDITIOBAL BOTES: Representative profile for Dystropepts is extrapolated from sheet 

1010. 

1110 - 122

LAUD H u REPORT LKEP-SDBM, CSR-BGGCR 

1. LARD HUIT: Hab.1.6.3 

4. OCCOREKE by PROVIKE: 

MAP IMAGE: CSOSS SECTKM: 

1.6.3 

setaiorpbic 

H.I.5.2 H.I.6.) 

5. SXAIDS IDEHTIFIERS : Updated by: DR edit date: 07/06/89 Status: Final 

6. LAHD DH1T DESCBIPTIOH: 


8. AERIAL. PHOTOGHAPBS : 

9. BADAR : 

10. BAREBT MATERIAL 







14. RIVERS a. Floodxisk : None 


15. VEGETATIGH/LAHD USE : 

Area used : 

16. ACCELERATED EROSIOB 


b. Evidence 

17. SOIL G8EAI GBDOF 

Dominant >SOZ 

Associated 1 

Associated 2 

32. REPSESEHTATIVE PROFILES: 

2. MAP SHEET: 1110-14 3. AREA: 75 km2 

Lampung: 99Z 

Strongly dissected hillocks in rolling pattern,intermediate and 

mafic tuffs and lavas, slopes 8-30%. 

123/64/14/11/84, 

1:100.000 60 /8295-007, 

Star-I/250/88/1110-2,3 


11. ROCK UUTCBOP: X 

1.4.2 

, bush, upland crops, rainfed wetland rice, coffee (kopi), coconut 

(kelapa) 

80 X 

Various 


dystropepts 

hapludults 

Z of area 

90 X 

10 X 

X 

Lab. checked 

ity/ /86-50 /81/DK/1110/14/ uda/ /341-49 /72/DR/1110/14/ /41 / 

1110 - 123 

yes 

yes


Properties 


subsoil 


mineralsoil 

c. Drainage: 


subsoil 

e. ïuuii ïLêû: uipsoii 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 




fine 

-very 

deep 

Well drained 

-- 

— 

nign 

low 

high 

low 

-- 

-- 

— 

— 


strong acid 

-- 

-- 

— 

-- 

-- 

-- 

-- 

2.1 

O.C 

0 

Associated 1 

medium 

fine 

— 

very deep 

Well drained 

-- 

-- 

very low 

medium 

Olsen 

medium 

very low 

very low 

low 

-- 

-- 

neutral 

neutral 

— 

-- 

-- 

— 

— 

— 

— 

2.2 

0.0 

1 

Associated 2 

19. ALTITUDE: Maximo: 200 m Minimum: 50 m Range: 75 m 

20. FLAU/PROFILE: Dominant: non-linear and random 40-60Z of area crested/peaked 

Included: 

21. L.U. DRAIHAGE: a. Pattern: dendritic b. density: Mod. high 


22. SLOPE: a. Steepness:sloping b. Variability: Medium 

0.0 

0.0 

0 



23. SLOPE DISTR.: Valleybottoms: 5 X 

Interfluves : 0-81:5 X, 9-251: 85 X, 25-551: 5 X 

24. BELIEF AMPLI.: a. Amplitude: medium b. Variability: Medium 

25. TERRAIS: Rolling 9-15%, 0-50 m 

26. CREST/RIDGES: a. Shape: Undulating b. Length:Short c. Variability: Medium 


27. VALLEI FLOOR: a. Width: very narrow b. Variability: Low 

. -2- Rolling area, hapludults, 10X 

-3- 

-4- 

29. FRAGMEHTATIGH: Valleys: Interfluves: Medium blocks 

30. RELIABILITT: 1= reliable, 2= probable, 3= tenable, 4» plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 1 18.a: 2 18.b: 2 18.c: 1 

18.d-q: 1 19: 2 22: 2 23: 2 24: 2 28: 3 29: 2 

31. ADDITIONAL BOTES: 

1110 - 124

LAK) UHXT REFOBT ' 

LBEP-SDBM, CSK-1 

MAP IMAGE: CBQSS SECTIGH: 

H.1.2.1 

'volcanic rocks ''* 

B.I.5.2 H.1.G.3 

1. LAHD ISIT: Htn.1.6.3 


4. ""fty by PBOVIKE: Lampung: 99Ï 

5. STATUS IDE8TIFIERS : Updated by: DR edit date: 03/06/89 Status: Final 

6. LAHD DHIT DESCRTPTICH: 

7. SATELLITE SCECES : 

8. AFPTAt. PHOTOGRAPHS : 

9. RADAE : Star-I/250/88/1110-2,3 

10. PAREflT MATERIAL 



c. Fomatxan : PTse 




14. RIVERS a. Floodxisk : None 

None 

15. VBOTIATIOB/LAIID USE : 

16. 

Area used 

oetatorpMc •» 

rocks 

Strongly dissected hillocks in rolling pattern,metamorfic rocks, 

slopes 8-30Z. 

123/64/14/11/84, 

1:100.000 59 /8292-021, 

High 

gneiss, schists, 



mixed gardens of fruit trees, rubber (karet) 

80 X 

a. Occorence : Common 


17. SOU. GREAT GROUP : 

Damnant >50Z 

Associated 1 

Associated 2 


dystropepts 

hapludults 

eutropepts 

ity/ /341-37 /72/DR/1110/42/ /020/ 

ite/ /86-39 /81/DK/1110/14/ /07 / 

Z of area 

60 X 

30 X 

10 X 

'1110 - 125 

Lab. checked 

yes 

yes 

yes 

uda/ /341-10 /72/SK/1110/14/ /26 /


Properties 


subsoil 


miner alsoil 

c. Drainage: 

d. Ezcfa. K: topsoil 

subsoil 

subsoil 


topsoil 

subsoil 

8- Total F: topsoil 

subsoil 


subsoil 


subsoil 


subsoil 



B. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FLAU/PROFILE: 

21. L.O. D8AŒAGE: 

22. SLOPE: 


24. RELIEF AMPLE. : 

23. TEBRAIB: 




29. FBAGMEHTATIGH: 

30. HELIABILITÏ: 

lO.b : 1 12.a: 2 

18.d-q: 1 19: 2 

31. ADDITIONAL HOTES: 


fine 

fine 


Well drained 

low 

Olsen 

medium 

very low 

medium 

medium 

— 

-neutral 

neutral 

— 

-- 

— 

-- 

-- 

-- 

50 cm 

2.2 

0.0 

1 

Associated 1 


fine 

deep 

Well drained 

very low 

Olsen 

very low 

very low 

medium 

low 

neutral 

slightly acid 

120 cm 

1.4 

0.0 

2 

Associated 2 

medium 

fine 

mod. shallow 

Well drained 

medium 

very low 

low 

Bray I 

medium 

low 

low 

low 


strong acid 

42 cm 

2.4 

6.2 

2 

1 25 m Minimum: 100 m Range: 110 m 


Included: 







Interfluves : 0-81:20 %, 


Rolling 9-15%, 0-50 m 




9-25Z: 55 %, 25-55Z: 20 % 


a. Shape: Undulating b. Length:Short c. Variability: Medium 



-1- Crests & upper slopes, dyst-.ropfipt.s . fifiï 


-3- Lower slopes, eutropepts, 15% 

-4- 


1= reliable, 2= probable, 3= tenable, 

14.a: 1 14.b: 1 17: 1 18.a: 2 

22: 2 23: 2 24: 2 28: 2 

1110 - 126 

4= plausible 

18.b: 2 18.c: 1 

29: 2

LAUD OHIT REPOST LREP-SDBM, CSR-BOGOK 

l. LAHD OBIT: Hdq.4.4 

5. 

6. 

7. 

8. 

9. 

10. 

12. 

13. 

14. 

15. 

16. 

17. 

MAF HUGE: CROSS SBCTICH: 

STATUS EDEHTIFIERS 

LAHD UHIT DESCRIPTICH 

SATELLITE SCEHES 

AERIAL FHOTOGBAPHS 

BADAR 

FAREBT MATERIAL 

a. Heather ing 

b. Lithology 

c. Formation 

HATER a. Quality 

b. Source 

FISHERIES 


b. Inundation 

VBGEIATIOH/LAHD OSE 

Area used 

Ar"»-FI F»ATFTI VBfKjrm 

a. Occurence 

b. Evidence 

SOIL GREAT GROUP 

Dominant >50X 

Associated 1 

Associated 2 

32. BEPKESEHTATIVE PROFILES: 

B.7 

coconut 

a 

4.4 

M 

ait: 

m?" acid tuff »• felsic coarse sediientar 

2. MAP SHEET: 1110 3. 

Lampung: 99% 

updated by: DR edit date: 03/06/89 

Extremely dissected tectonic valley,acid 

sedimentary rocks, slopes 16-30Z. 

123/64/14/11/84, 

1:100.000 60 /8295-005, 

Star-I/250/88/1110-2 

11. 

High 

liparite, sandstone, 

Qlv 

Fresh 

: Perennial River . • 

None 

None 

None 

bush, alang-alang, upland crops, coffee 

80 X 

Common 

Gulleys 


dystropepts 

hapludults 

1110 - 127 

Z of area 

90 r. 

10 i 

% 

AREA: 34 km2 

I..3 

Status: Final 

tuffss and coarse felsic 

ROCK OUTCROP: % 

(kopi), coconut (kelapa) 

Lab. checked 

yes 

yes 

uda/ /341-8 ./72/SK/1110/14/ /ll /

in arm. naaarrnansxTni 

Properties 


subsoil 


* ¥1OT îll «rif 1 

c. Drainage: 


subsoil 

e. Total K2D: topsoil 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FLAH/EBOFILE: 

21. L.D. DBAHUGE: 

22. SLOPE: 

23. SLOPE DISTH. : 


25. TESRAH: 

26. CSEST/KIDGES: 


29. FRAGMESTATIOB: 


lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 



fine 

-deep 

Well drained 

low 

very low 

-- 

-- 

Bray I 

low 

very low 

-- 

-low 

very low 

strong acid 

strong acid 

-- 

-- 

— . 

— 

— 

-- 

— 

0.0 

0.0 

0 

150 m MLnimnm: 

Dominant: non-linear and random 

Included: 






Valleybottams: 5 X 

InterCluves : 0-81:0 X 


hillocKy >16*, 0-50 m 

Associated 1 

medium 

fine 

— 

deeu 

Well drained 

-- 

-very 

high 

medium 

Olsen 

very high 

very low 

very high 

medium 

— 

-neutral 

slightly acid 

-- 

-- 

-- 

— 

-- 

-- 

100 cm 

3.1 

0.0 

1 

a. Shape: .Undulating b. Length:Short 

d. Width: narrow e. Variability: Low 


-2- Middle Slopes, hapludults, 10Z 

-3- 

-4- 


1= reliable, 2° probable, 3= tenable, 

14.a: 1 14.b: 1 17: 2 18.a: 2 

22: 2 23: 2 24: 2 28: 2 

Associated 2 

0.0 

0.0 

0 

25 m Range: 75 m 

40% of area flat-topped 

b. density: High 



9-25X: 60 X, 25-55X: 35 X 


4° plausible 

18.b: 2 18.c: 

29: 2 


31. ADDITIOHAL BOTES: Dystropepts extrapolation based on RePPProT (Land System SAA). 

1110 - 128

LAHD OBIT REFOBT LREP-SDBM, CSB-BOGOR 

1. LAHD UHIT: Mab.2.2.3 

MAP IMAGE: CEOSS SECTIOH: 

*. OCCOREBCE by PROVTACE: 

5. STATUS IDEHTIFIERS : Updated by: DR' edit date: 05/06/89 Status: Final 

6. LABD OMIT DESCRIPTIOH: 

7. SATELLITE 

8. AERIAL PHOTOS8APHS : 

9. RADAR : 







13.. FISHERIES : None 


b. Inundation : None 

15. VEGETATICH/LAHD OSE : moist primary lowland forest, bush, alang-alang, shifting cu 

Area used : 

16. ACCELERATED EROSIOB 


17. SOIL GSEAT GBOOP 

Lampung: 99% 


Dominant >SOZ 

Associated 1 

Associated 2 



Strongly dissected mountains,intermediate and mafic tuffs and 

lavas, steep to very steep slopes (30-75%) 

123/64/14/11/84 

1:100.000 57 /S292-073, 57 /8292-077, 58 /8292-063 

Star-I/250/88/1110-2,3 

Partial 


Fresh 

11. ROCS OUTCROP: % 

ltivation, upland crops, clove (cengkeh), banana, towns, villages 

40 X 

Extensive 


dystropepts 

hapludults . 

humitropepts 

ity/ / /87/US/1010/ / /19 / 

ith/ / /87/SR/1010/ / /31 / 

1110 - 129 

Z of area 

50 % 

40 X 

10 % 

Lab. checked 

yes 

yes 

yes 

uda/ /87/TB/1010/ / /05

18. SOIL CHAKACTEBISTICS 

Properties 


subsoil 


mineralsoil 

c. Drainage: 


subsoil 

c. Tct=l r2O: tcpcrii 

subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 

k. Al tenacity : 


m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. FLAH/FK0FILE: 

21. L.0. DRAIHAGE: 

22. SLOPE: 


24. RELIEF AMPLE.: 

25. TERRAIH: 




29. FKAGHEBTATICB: 


lO.b : 2 12.a: 2 

18.d-q: 2 19: 2 

Dominant > 50Z 


fine 

— 

very deep 

Well drained 

medium 

low 

1c:: 

low 

Bray I 

very low 

very low 

low 

very low 

low 

low 



medium 

high 

no 

— 

-- 

-- 

120 cm 

2.2 

2.0 

0 

Associated 1 

fine 

fine 

' -very 

deep 

Well drained 

very low 

very low 

vc^j lu» 

very low 

Bray I 

very low 

very low 

medium 

medium 

medium 

medium 

strong acid 

strong acid 

very low 

high 

no 

— 

-- 

-- 

120 cm 

2.1 

4.2 

0 

450 m Minim: 100 m Range: 300 m 

Dominant: linear and random > 60% of area crested/peaked ' 

Included: 






Valleybottoms: X 

Interfluves : 0-81:0 X, 





a. Width: 

-1- Crest & upper slopes rivst.rnnpnt.s SOÏ 


-3- Lower slopes, humitropepts, 10% 

-4- 


Associated 2 

fine 

fine 

-deep 


low 

low 

low 

Bray I 

very low 

very low 

low 

low 

low 

low 



high 

very high 

no 

-- 

-- 

-- 

90 cm 

3.0 

2.5 

0 




9-25Z: 10 %, 25-55Z: 50 %, >55Z: 40 % 






14.a: 1 14.b: 1 17: 2 18.a: 1 18.b: 2 18.c: 

22: 2 23: 2 24: 2 28: 3 29: 2 

31. ADDITIOHAL HOTES: Representative profiles are extrapolated from sheet 1010. 

1110 - 130 


LAND UHIT REPOST LREP-SDBM, CSS-BOGCB 

1. LAHD OBIT: Mb . 2 . 2 . 3 

M&F IMAGE: CROSS SECTIOH: 

*. nmiBwm:r. by PRCWHJCE: 

5. SUTOS nJEHTIFIERS : 

6. LAHD HUIT DESCRIPTION: 


8. ATBPTAT- PHOTOGRAPHS : 

9. RADAR : 



b. Litfaology : 





14. RIVERS a. Flocdrisk : 


15. VBGETATICH/LAHD OSE : 

Area used : 


a. Occnrence : 


Lampung: 99% 


Dominant >50I 

Associated 1 

Associated 2 



Strongly dissected mountains,intermediate and mafic lavas, steep 

to very steep slopes (30-75%). 

123./64/14/11/84, 

1:100.000 57 /8292-77 , 58 /8292-67 

Star-I/250/88/1110-2,3 

High 

andesitic lavas, 

Tov 


None 

None 

None 

None 

secondary forest, bush, clove (cengkeh) 

40 % 

Extensive 


dystropepts 

hapludults 

Z of area 

55 % 

35 % 

11. ROCK OTTCBOP: 10 % ' 

Lab. checked 

ity/ / /87/US/1010/ / /19 / uda/ /87/TB/1010/ / /05- / 

1110 - 131


Properties 


subsoil 


mineralsoil 

c. Drainage: 


subsoil 

e. Total K2O- *»«»»•«*;> 

subsoil 


topsoil 

subsoil 


subsoil 

fa. CBC pH 7 topsoil 

subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 




fine 

very deep 

Well drained 

medium 

low 

low 

Bray I 

very low 

very low 

low 

very low 

low 

low 



medium 

high 

yes 

120 cm 

2.2 

2.0 

0 

Associated 1 

fine 

fine 

very deep 

Well drained 

very low 

very low 

very low 

very low 

Bray I 

very low 

very low 

medium 

medium 

medium 

medium 

strong acid 

strong acid 

very low 

high 

yes 

120 cm 

2.1 

4.2 

0 

Associated 2 

19. ALTITUDE: M,niiimmm- 400 m Minimum: 25 m Range: 250 m 

20. PLAH/HBÛFILE: Dominant: non-linear and random > 60X of area crested/peaked 

Included: 

21. L-0- DRAXBAGE: a. Pattern: dendritic b. density: Mod. high 


22. SLOPE: a. Steepness:very steep b. Variability: Medium 

c. Length: long d. Variability: Medium 


23. SLOPE DISTR.: Valleybottoms: % 

Interduves : O-8Z:10 %. 9-251: 15 X, 25-551: 30 Z, >55I: 45 % 

24. BETTET AMPLI.: a. Amplitude: very high b. Variability: Medium 

25. TERRAIS: Mountainous >16%, >300m 

26. CREST/RIDGES: a. Shape: Irregular b. Lengtb:Long c. Variability: Medium 

d. Width: wide e. Variability: High 

27. VALLES FLOOR: a. Width: b. Variability: 

28. LAND FACETS: -1- Crest & upper'slopes_ dystropcpts, 55Ï 

-2- Middle & lower slopes, hapludults, 35% 

-3- 

-4- 

29. FRAGMEHTATIGH: Valleys: Interfiles: 

30. RELIABILITY: 1° reliable, 2= probable, 3= tenable, 4= plausible 

lO.b : 2 12.a: 2 14.a: 1 14.b: 1 17: 2 18.a: 3 18.b: 3 18.c; 1 

18.d-q: 2 19: 2 22: 2 23: 3 24: 2 28: 2 29: 2 

31. ADDITIONAL BOTES: Representative profiles are extrapolated from sheet 1010. 

1110 - 132 

0.0 

0.0 

0

LABD UHU BERST LREP-SDBM, GSR-BOSOR 

MAP IMAGE: 

1. LAHD DIIT: Mb. 2. 3. 3 

4. OOCDRENCE by PRUVJUCE: 

5. STATUS ÜJEHTIFIERS : 

6. LAHD DUT DESCRIPTION: 


8. AFBTAÏÏ, PHOTOGRAPHS : 

9. BADAR : 

10. PARBST M&TEBIAL 









15. VEEEIATIQH/LAHD USE : moist primary lowland forest, bush, upland crops, clove (cengkeh), 

Area used : 

16. ACCELERATED ER0SI0H 

a. Occurence 

b. Evidence 

17. SOIL GREAT GBOTP 

Dominant >50I 

Associated 1 

Associated 2 

Lampung: 99% 


Updated by: DR edit data: 05/06/89 Status: Final 

Strongly dissected mountain, intermediate and mafic lavas, ubrupts 

slopes (>75!5) 

123/64/14/11/88, 

1:100.000 57 /8292-073, 58 /8292-069, 

Star-I/250/88/1110-2,3 

High 


Tov 

None 

coffee (kopi) 

40 X 

Common 

Gulleys 


dystropepts 

hapludults 

I of area 

60 X 

30 X 

z 


Lab. checked 

no 


ity/ / /87/SR/1010/ / /3 / uda/ /87/HJ/1010/ / /ll / 

1 10 - IV! 

no

18. SOIL 

Properties 


subsoil 


•inaraimil 

c. Drainage: 


subsoil 


subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITUDE: 

20. PLAH/PBOFILE: 

21. L.D. DBAIBBSB: 

22. SLOPE: 

23. SLOPE DISTB. : 


25. TERRAIH: 

26. C8E5T/BIDGES: 



29. FBACMEHTATIOH: 

30. KELJABILITi: 

lO.b : 1 12.a: 2 

18.d-q: 2 19: 2 

Damnant > SOI 

fine 

fine 

— 

very deep 

Well drained 

high 

high 

hiRh 

high 

Bray I 

very low 

very low 

medium 

low 

low 

low 


strong acid 

very low 

very low 

— 

-- 

— 

— 

— 

3.8 

7.7 

0 

Associated 1 

fine 

fine 

— 

very deep 

Well drained 

low 

very low 

low 

very low 

Bray I 

very low 

very low 

medium 

medium 

low 

low 


strong acid 

very low 

very low 

-- 

-- 

— 

-- 

2.3 

11.2 

0 

Associated 2 

0.0 

0.0 

0 

450 m Minina: 25 m Bange: 300 m 

Damnant: non-linear and random > 60% of area crested/peaked 

Included: non-linear and random 40-60% of area flat-topped 




a. Steepness:extremely steep b. Variability: High 




ValleybottOBs: % 

Interfluves : 0-8Z:0 %, 9-2SZ: 

a. »ill il mill: very high 


0 X, 25-55Z: 10 X, >55X: 90 X 


»: Irregular b. Length:Short c. Variability: Medium 


a. Width: 


-1- Crests & upper slopes, dystropepts, 60% 

-2- Middle & lower slopes, hapludults, 30% 

-3- 

-4- 


' reliable, 2° probable, 3= tenable, 4= plausible 

14.a: 1 14.b: 1 17: 2 18.a: 2 18.b: 2 18.c: 2 

22: 2 23: 2 24: 2 28: 3 29: 0 

31. AEOITIGHAL BOTES: Representative profiles are extrapolated from sheet 1010. 

1110 - 134

LARD DHIT EEPCBT IBEP-SDSM, CSK-BOGGR 

KAP DOGE: SBCTIOH: 

1. 1ABD BHIT: Md.2.3.3 . 2. MAP SHEEI: 1110 3. AREA: 19 km2 

4. nrniBHTK by PHGVHICE: Lampung: 99% 

5. STATDS IDEHTXFIERS : Updated by: DR edit date: 05/06/89 Status: Final 

6. LAUD OMIT DESCRIPTION: Strongly dissected mountains, acid tuffs,abrupt slopes (>75%). 

7. SATELLITE SCBHES : 123/64/14/11/88, 

8. AERIAL PBDTOG8APBS : 1:100.000 58 /8292-65 

9. RADAR : Star-I/250/88/1110-2,3 

10. PAREHT tttTERIAL 


b. Lithology : dacite, 

c. Formation : Tmda 






15. VBGEIATICH/LAHD OSE : secondary forest, bush, upland crops 


16. ACCELERATED EROSIGB 

17. SOIL GREAT GROOP 

a. Occurence : Extensive 


DoMinant >5OI 

Associated 1 

Associated Z 

32. REFKESEHTATIVE PROFILES: 


hapludults 

dystropepts 

troporthents 

1110 - 135 

Z of area 

50 % 

40 % 

10 % 

11. BOCK GUTCKQP: 10 % 

Lab. checked 

yes 

no 

no

is. son. 

Properties 


subsoil 


c. Drainage: 


subsoil 

e_ Tnfc«l K2HJ- fconx/ti 1 

subsoil 

£. Avail. F: aethod 

topsoil 

subsoil 


subsoil 


subsoil 


subsoil 


subsoil 



m. Salinity : 




q. TEB : 


19. ALTITODE: 

20. PLAB/PBOFILE: 

21. L.D. DBAIKAGE: 

22. SLOPE: 

23. SLOPE DISTS. : 

24. BELIEF AMFLI.: 

25. TEBBAIH: 

26. CKEST/BIDGES : 



29. FBAGMEBTATICH: 


10.b : 1 12.a: 2 

18.d-q: 3 19: 2 

Drainant > SOX 

fine 

fine 

— 

very deep 

Well drained 

low 

low 

very low 

Bray I 

very low 

very low 

medium 

low 

medium 

low 

strong acid 

strong acid 

medium 

medium 

0.0 

0.0 

0 

— 

-- 

— 

-- 

— 

Associated 1 Associated 2 

0.0 

0.0 

0 

0.0 

0.0 

0 

600 m Minimn: 250 m Bange: 500 m 

uoannant: non-linear and random > 601 of area crested/peaked 

Included: 



a. Steepness:extremely steep 




Interfluves : 0-81:0 X. 9-251: 


Mountainous >16£, >300m 


d. Width: moderate. 

a. Width: 




X, 25-55X: 15 X, >55X: 85 X 





-1- Upper & middle slopes, hapludults, 

-2- Crest & lower slopes, dystropepts, 

-3- lower slopes, troporthents, 10X 

-4- 


1= reliable, 2= probable, 3= tenable, 

14.a: 1 14.b: 1 17: 3 18.a: 3 

22: 2 23: 2 24: 2 28: 3 

50Ï 

40Z 

4= plausible 

18.b: 2 18.c: 

29: 2 

31. ADDITIOHAL BOIES: Hapludults extrapolation based on RePPProT (Land System TWI). 

1110 - 136 


USD OBIT REPORT LREP-SDBM, CSR-BOGGR 

1. LAID OBIT: Mab.2.3.4 

MAP IMAGE: CROSS SECTIOH: 

4. «»fiiUHMi-R by PRGWIHCE: 

5. STATUS IDENTIFIERS : 

6. LAHD OHIT DESCRIPTIOH: 


8. AHITAT. l^f Vfi i-JP A***dy ; 

9. SADAR : 

10. BARER MATERIAL 





A.5 




b. Inondation: 

Lampung: 99% 

éscarpient 

M.2.2.3 



K.2.3.4 

Extremely dissected mountains,intermediate and mafic tuffs and 

lavas, abrupts slopes (>75X). 

123/64/14/11/84, 

1:100.000 59 /8292-19 

Star-I/250/88/1110-2,3 

Partial 


Qhv 

Fresh 

None 

None 

None 

11. BOCK OÜTCBQP: 15 % 

15. VBGEIATICH/LAHD USE : moist primary lowland forest, bush, alang-alang, clove (cengkeh) 

Area used 


: 45 % . 

a. Occnrence : Extensive 


17. SOIL G8EAT GSODP 

Dominant >50Z 

Associated 1 

Associated 2 



dystropepts 

humitropepts 

eutropepts 

ity/ / /87/US/1010/ / /19 / 

ite/ /184-4 . /81/NS/1110/14/ /ll / 

1110 - 137 

Z of area 

50 % 

20 X 

15 X 

Lab. checked 

yes 

yes 

yes

IA «SOTT, rMflMrTSBTSTTfSS 

Proportios 


subsoil 


Bineralsoil 

c. Drainage: 

d. Erch. K: topsoil 

subsoil 


subsoil 


topsoil 

subsoil 


subsoil 


subsoil 


subsoil 

j. AL Sat. topsoil 

subsoil 



B. Salinity : 


o. Soot abstr. layer : 


q. TEB : 


19. ALTITUDE: 

20. FLAH/PRQFTLE: 

21. L.D. DBAIBAGE: 

22. SLOPE: 



23. TERRAXB: 




29. FBAGMEnATICH: 

Drainant > SOX 


fine 

— 

very deep 

Well drained 

medium 

low 

low 

low 

Bray I 

very low 

very low 

low 

very low 

low 

low 



medium 

high 

yes 

-- 

-- 

— 

-- 

2.2 

2.0 

0 

Associated 1 

fine 

fine 

— 

very deep 

Well drained 

low 

low 

low 

very low 

very low 

very low 

low 

very low 

medium 

low 

excessive acia 


very high 

very high 

yes 

— 

-- 

— 

-- 

0.0 

0.0 

0 

Associated 2 

fine 

fine 

— 

very deep- 

Well drained 

low 

very low 

low 

low 

-- 

-low 

very low 

medium 

medium 

slightly acid 

slightly acid 

— 

-- 

-- 

— 

-- 

— 

-- 

2.4 

14.2 

0 

550 m Minimnsi: 25 m Range: 350 m 

Dominant.: linear and random > 60% of area crested/peaked 

Included: 

a. Pattern: dendritic b. density: High 


a. Steepness:extremely steep 

c. Ltmgth: short 



Inter£luves : 0-81:15 X. 9-25X: 0 




d. Width: narrow 

a. Width: 



X, 25-551: 10 X, >55X: 75 X 





-1- Crest,upper&mid slopes, dystropepts, 

-JS- Lower slopes, humitropepts, 'ZUH 

-3- Lower slopes, eutropepts, 15Ï 

-4- 

Valleys: Inter£luves: 

30. RELIABILITY: 1= reliable, 2= probable, 3= tenable, 4° plausible 

lO.b : 1 12.a: 2 14.a: 1 14.b: 1 17: 3 18.a: 2 18.b: 3 18.c: 2 

18.d-q: 3 19: 2 22: 2 23: 2 24: 2 28: 3 29: 2 

50% 


31. ADDITIONAL BOTES: Representative profiles for Dystropepts is extrapolated from sheet 

1010. Humitropepts extrapolation based on RePPProT. 

1110 - 138

LAHD OBIT REFCBT LREP-SDBM, CSR-BOGCB 

1. LAHD OMIT: Mb . 2 . 3 . 4 

MAP IMAGE: SECTIOS: 

*. OCCd&EBCE by PBOWIBCE: 

5. STAÏDS HJEHTIFIEBS : 

6. LAND OBIT DE9CHIPTICM: 

7. SATELLITE 

8. AB1BTAT. CBOTOGBâfBS 

9. BADêB 

10. FAREHT MâTEBIAL 

a. Weathering 

b. Litbology 

c. Formation 

12. HATES a. Quality 

13. FISHERIES 

b. Source 


b _ Inundation 

15. VBGEIATIGR/LAHD OSE 

Area used 

16. ACCELERATED EBOSIOH 

a. Occorence 

b. Evidence 

17. SOIL GBEAT GSODP 

Doainant >50Z 

Associated 1 

Associated 2 

32. HEFRESESTATTVE ROOTLES: 

: 0% 

A.2.2.1 

'' colluvial 'i 

K.2.2.3 «.2.3.4 




Extremely dissected mountains,intermediate and mafic lavas, abrupts 

slopes (>75%). 

123/63/14/11/84, 

1:100.000 58 /8292-67 

Star-I/250/88/1110-2,3 

High 


Tov 

Fresh 

Rain, Perennial River 

None 

None 

None 

11. BOCK OOTCSaP: 15 % 


clove (cengkeh) 

40 X 

Extensive 

Various 


dystropepts 

eutropepts 

humitropepts 

Z of area 

50 %' 

20 X 

15 % 

Lab. checked 

no 

ity/ / /87/SR/1010/ / /3 / ite/ /184-4 /81/NS/1110/14/ /Oil/ 

1110 - 139 

yes

18. SOIL CHABACTEKISTICS 

Properties 

a. Textare: topsail 

subsoil 


Biimral noi 1 

c. Drainas«: 


sobsoil 


subsoil 

f. Avail. P: aetbod 

topsoil 

subsoil 


subsoil 

h. CXC pH 7 topsoil 

subsoil 


subsoil 


k. Al tozicitT : 

subsoil 

1. Acid sulpta. pot.: 


n. Other Tenacity: 



q. TEB : 


19. ALTITUDE: 

20. FLAB/EHOFILE: 

21. L.O. 

22. SLOPE: 



25. TEBBAIB: 

26. 


28. LATO FACETS: 

29. 


lO.b : 2 12.a: 1 

18.d-q: 3 19: 1 

Donnant > 501 

fine 

fine 

— 

very deep 

Well drained 

high 

high 

high 

high 

Bray I 

very low 

very low 

medium . 

low 

low 

low 


strong acid 

very low 

very low 

-- 

-- 

— 

3.8 

7.7 

0 

- - • 

- - 

Associated 1 

fine 

fine 

— 

very deep 

Well drained 

low 

very low 

low 

low 

low 

-- 

-- 

very low 

medium 

medium - 

slightly acid 

slightly acid 

-- 

-- 

-- 

— 

-- 

-- 

— 

2.3 

14.2 

0 

Associated 2 

fine 

fine 

— 

very deep 

Well drained 

low 

low 

low 

very low 

very low 

very low 

low 

very low 

medium 

low 



very high 

very high 

-- 

-- 

— 

-- 

— 

0.0 

0.0 

0 

: 1225 m Miniaun: 250 m Bange: 800 m 

Damnant: linear and random > 60% of area crested/peaked 

Included: 

a. Pattern: dendritic b. density: High 


a. Stampuess:extremely steep 



Valleybottcas: 0 % 



Imterfloves : 0-81:15 X. 9-25Z: 0 X, 25-551: 5 %, >55I: 80 X 

a. Olli i I iwin : very high 


Mountainous >16X, >300m 

a. Shape: Irregular b. Length:Moderately long c. Variability: Medium 

d. Width: narrow 


a. Width: 


-1- Crest & upper slopes, dystropepts, 50Ï 

-3- Lower slopes, humitropepts, 15Ï 

-4- 

Valleys: Interduves: 

1' reliable, 2» probable, 3° tenable, 4= plausible 

14.a: 1 14.b: 1 17: 3 18.a: 3 18.b: 3 18.c: 3 

22: 1 23: 2 24: 1 28: 3 29: 0 

31. ADDITIONAL BOTES: This LU is extrapolated from sheet 1010 and RePPProT. 

1110 - l

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