27.01.2015 Views

complementary studies in physical land resources and

complementary studies in physical land resources and

complementary studies in physical land resources and

SHOW MORE
SHOW LESS
  • No tags were found...

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

EDITORIAL<br />

You will f<strong>in</strong>d this issue of Pedon this year a bit later <strong>in</strong> your postal box than<br />

usual. As announced last year, we are cop<strong>in</strong>g with a peak year of activities.<br />

On the one h<strong>and</strong>, there is the work related to the visitation of our programme<br />

for accreditation. On the other h<strong>and</strong>, we have to prepare the Refresher<br />

Workshop for Alumni that takes place next autumn, here <strong>in</strong> Ghent. And then<br />

there is the ever <strong>in</strong>creas<strong>in</strong>g number of applications for VLIR-scholarships for<br />

our programme. This year we had about 350 applications for 16 available<br />

scholarships. It means a noticeable <strong>in</strong>crease of our workload to go through all<br />

these applications. The good news however is, that also the average quality<br />

of the applications is ris<strong>in</strong>g <strong>and</strong> gett<strong>in</strong>g better than it already was. The past<br />

two years, also more <strong>and</strong> better applications from female c<strong>and</strong>idates were<br />

received, result<strong>in</strong>g <strong>in</strong> a higher number of female students than we usually had<br />

so far. Inevitably however, we will aga<strong>in</strong> have to disappo<strong>in</strong>t many truly<br />

deserv<strong>in</strong>g c<strong>and</strong>idates.<br />

CONTENTS<br />

Editorial ................................................ 1<br />

Staff News ............................................. 2<br />

Students, research fellows &<br />

tra<strong>in</strong>ees .................................................. 5<br />

Publications ........................................ 17<br />

Soils <strong>and</strong> maps .................................... 22<br />

Project profiles .................................... 23<br />

Communications received .................. 25<br />

Meet<strong>in</strong>gs .............................................. 28<br />

Advanced Tra<strong>in</strong><strong>in</strong>g <strong>and</strong> Research<br />

Opportunities ...................................... 31<br />

At the moment of writ<strong>in</strong>g this editorial, most of the work related to the<br />

visitation is beh<strong>in</strong>d us, allow<strong>in</strong>g us to concentrate better now on the alumni<br />

workshop (our apologies to all alumni that were mail<strong>in</strong>g the past few weeks<br />

<strong>and</strong> at times had to wait for an answer !). As for the outcome of the whole<br />

"visitation exercise", it may take quite a while before we will receive any<br />

news. We keep you <strong>in</strong>formed of course ! By the way, I would like to thank<br />

here all alumni who gave us some of their precious time to respond to the<br />

questionnaire which we sent to obta<strong>in</strong> valuable <strong>in</strong>formation for our report to<br />

the visitation commission. Note that only alumni of the M.Sc. Physical L<strong>and</strong><br />

Resources have been <strong>in</strong>volved, for obvious reasons. By now, 131 students<br />

have graduated from the <strong>in</strong>teruniversity M.Sc. programme <strong>in</strong> Physical L<strong>and</strong><br />

Resources. They took either "Analysis", "Use" or (mostly) "Management" of<br />

Physical L<strong>and</strong> Resources as major. As of 2006, graduates will major <strong>in</strong> either<br />

"Soil Science" or "Eng<strong>in</strong>eer<strong>in</strong>g Geology". Most graduates return to their former<br />

job, albeit <strong>in</strong> higher positions, <strong>and</strong> many turn to a job fitt<strong>in</strong>g better the M.Sc.<br />

<strong>studies</strong> done here <strong>in</strong> Ghent. Quite a number of alumni pursue(d) a Ph.D.<br />

degree, many abroad (USA, Canada, New Zea<strong>l<strong>and</strong></strong>, Europe – <strong>in</strong>clud<strong>in</strong>g<br />

Belgium). Quite often, we discover this almost "by accident". Please do keep<br />

us <strong>in</strong>formed about your whereabouts, Ph.D. <strong>and</strong> other promotions ! Us<strong>in</strong>g<br />

the leaflet <strong>in</strong>cluded here or send<strong>in</strong>g us an e-mail are ready-to-use options to<br />

this purpose. Both we here <strong>in</strong> Ghent, as well as your former colleague<br />

students are <strong>in</strong>terested <strong>in</strong> this k<strong>in</strong>d of news. Thanks to the alumni who wrote<br />

us already. Please cont<strong>in</strong>ue …<br />

Prof. Dr. E. Van Ranst<br />

May 2006<br />

- 1 -


STAFF NEWS<br />

LAUDATIO<br />

Prof. Dr. R. Langohr was born <strong>in</strong><br />

Antwerp on November 7, 1939. He<br />

graduated <strong>in</strong> 1963 at the Free<br />

University of Brussels as a botanist<br />

with specialization <strong>in</strong> plant ecology<br />

<strong>and</strong> systematics. In 1965 Prof. Langohr<br />

became a student at the ITC.<br />

His motivation was to get a better underst<strong>and</strong><strong>in</strong>g of nature<br />

through the study of soils.<br />

After his <strong>studies</strong> Prof. Langohr worked as an Expert for the<br />

Centre Technique Forestier Tropical <strong>in</strong> Ivory Coast<br />

followed by a post as an Associate expert, then as an<br />

Expert <strong>in</strong> soil science for FAO <strong>in</strong> Chile. Field data, many<br />

reports <strong>and</strong> soil samples were brought to Belgium <strong>and</strong><br />

served as the base of his Ph.D. thesis, which concerned the<br />

soilscape <strong>and</strong> quaternary geology of the Central Valley <strong>in</strong><br />

Chile. In between his <strong>in</strong>ternational missions Prof. Langohr<br />

was also active <strong>in</strong> the soil mapp<strong>in</strong>g of Belgium.<br />

From 1971, Roger Langohr was attached to the Ghent<br />

University, at first as an Assistant, then as Assist<strong>in</strong>g<br />

Professor <strong>and</strong> s<strong>in</strong>ce 1992 as Associated Professor. Dur<strong>in</strong>g<br />

his career, he was teach<strong>in</strong>g several courses, such as :<br />

general pedology (graduate), soil science for archaeologists<br />

(graduate), pedology, soil <strong>and</strong> regolith prospection, soil<br />

classification <strong>and</strong> mapp<strong>in</strong>g, geo- <strong>and</strong> archaeopedology<br />

(post-graduate courses). His teach<strong>in</strong>g always offered an<br />

alternative viewpo<strong>in</strong>t <strong>and</strong> his captivat<strong>in</strong>g lectures were<br />

illustrated with large attractive photographs <strong>and</strong> numerous<br />

slides. In the lectures he stressed the importance of rais<strong>in</strong>g<br />

the quality of field soil databases. To make his scientific<br />

po<strong>in</strong>ts clear, numerous monoliths <strong>and</strong> other soil samples<br />

were used <strong>in</strong> the lecture room – his class room with the<br />

many samples, photos etc. was an open book of nature <strong>and</strong><br />

a paradise for any enthusiastic student. The field trips<br />

formed an important part of the curriculum <strong>and</strong> were an<br />

<strong>in</strong>tensive tra<strong>in</strong><strong>in</strong>g period for practic<strong>in</strong>g, collect<strong>in</strong>g <strong>and</strong><br />

<strong>in</strong>terpret<strong>in</strong>g field data. When Prof. Langohr was expla<strong>in</strong><strong>in</strong>g<br />

one of his chapters out of the "Book of Nature" he could<br />

easily forget time <strong>and</strong> place, so it happened more than once<br />

that his students had to rem<strong>in</strong>d him that it was time for a<br />

break or lunch.<br />

Dur<strong>in</strong>g the seventies <strong>and</strong> eighties several research projects<br />

<strong>in</strong> the Zonian forest were performed under Prof. Langohr's<br />

supervision. Nature was studied from a holistic or global<br />

po<strong>in</strong>t of view but with the soil as central source of<br />

<strong>in</strong>formation : the l<strong>in</strong>k between soil characteristics, plant<br />

ecology <strong>and</strong> (paleo)environmental conditions (extension of<br />

the factors of soil <strong>in</strong>formation) was made.<br />

S<strong>in</strong>ce the late eighties Prof. Langohr's <strong>in</strong>terest turned more<br />

<strong>and</strong> more towards archaeo-pedology. Archaeologists tend<br />

to make very large sections; the many peculiarities <strong>in</strong> soil<br />

morphology gave him new <strong>in</strong>sights <strong>in</strong>to soil processes <strong>and</strong><br />

the evolution of the soilscape. This cooperation lead to<br />

several research projects such as the study on the<br />

distribution of Bronze age circles <strong>in</strong> F<strong>l<strong>and</strong></strong>ers, Bronze age<br />

burial sites <strong>in</strong> Denmark, burial sites <strong>in</strong> Altai (Siberia), soils<br />

of the Eemian-<strong>in</strong>terglacial <strong>in</strong> Europe <strong>and</strong> Central Siberia,<br />

old agricultural habits on Easter Is<strong>l<strong>and</strong></strong>, <strong>l<strong>and</strong></strong>scape<br />

reconstruction on the site of Verrebroek dok. Roger<br />

Langohr's expertise was called upon <strong>in</strong> many excavations<br />

throughout Belgium, France, Switzer<strong>l<strong>and</strong></strong> <strong>and</strong> many other<br />

countries. The <strong>in</strong>troduction of soil science as part of the<br />

course "Natural science techniques <strong>in</strong> Archaeology" <strong>in</strong> the<br />

curriculum for archaeology students is one of his merits.<br />

"It is all <strong>in</strong> the book of nature ! Dig deeper <strong>and</strong> wider !<br />

Follow the corridors <strong>and</strong> don't jump through the<br />

w<strong>in</strong>dows !" … dixit Prof. Langohr. These are the say<strong>in</strong>gs<br />

that the alumni of the International Tra<strong>in</strong><strong>in</strong>g Centre for<br />

Post-graduate Soil Scientists at the Ghent University <strong>and</strong><br />

the International Centre for Physical L<strong>and</strong> Resources<br />

(Ghent University, Vrije Universiteit Brussel) will cherish<br />

throughout their own professional lives.<br />

The 1 st of October 2005, Prof. Langohr took up his<br />

retirement. We wish him a pleasant retirement. Fortunately<br />

Roger will only retire from his adm<strong>in</strong>istrative tasks at the<br />

University, his scientific work we expect he will carry on<br />

for many more years.<br />

C. Ampe<br />

Hugo Decleir was born <strong>in</strong> Berchem<br />

(Antwerp-Belgium) the 7th of<br />

December 1939. He studied<br />

Geography at the Ghent University<br />

(1957-61) <strong>and</strong> obta<strong>in</strong>ed his doctoral<br />

degree <strong>in</strong> 1971 at the same<br />

university.<br />

From 1961 till 1985 he worked at the Observatory of the<br />

Ghent University first as teach<strong>in</strong>g assistant later as senior<br />

researcher. In the period 1979-1985 he was part time<br />

professor at the Geography Department of the Vrije<br />

Universiteit Brussel (VUB), where he than became full<br />

professor till 2005, date of his retirement.<br />

Dur<strong>in</strong>g his carrier as a university professor he was teach<strong>in</strong>g<br />

courses on cartography, geodesy <strong>and</strong> topography, as well<br />

as Climatology, Glacial <strong>and</strong> Periglacial Geosystems.<br />

Together with his student Frank Canters he succeeded to<br />

develop a successful research on automated cartography<br />

<strong>and</strong> GIS. This made it possible to <strong>in</strong>troduce the first course<br />

on GIS at university level <strong>in</strong> Belgium.<br />

However the ma<strong>in</strong> concern of his research was modell<strong>in</strong>g<br />

with the fields of glaciology <strong>and</strong> climatology, with<br />

emphasis on the close <strong>in</strong>teraction between both. Here he<br />

developed an <strong>in</strong>ternational recognised expertise together<br />

- 2 -


STAFF NEWS<br />

with two of his most successful students (Ph. Huybrechts<br />

<strong>and</strong> F. Canters).<br />

As a researcher Hugo Decleir was <strong>in</strong>volved <strong>in</strong> 8<br />

<strong>in</strong>ternational expeditions on the ma<strong>in</strong><strong>l<strong>and</strong></strong> of the Antarctic,<br />

<strong>in</strong>clud<strong>in</strong>g a 15 month long expedition <strong>in</strong> 1966. Furthermore<br />

he conducted fieldwork on Green<strong>l<strong>and</strong></strong>, Spitsbergh <strong>and</strong><br />

Siberia.<br />

Hugo Decleir is author of some 60 scientific publications<br />

<strong>in</strong> lead<strong>in</strong>g <strong>in</strong>ternational scientific journals, <strong>and</strong> he is holder<br />

of Richard P. Goldwaith Award of the Byrd Polar<br />

Research Center (Ohio State University).<br />

Hugo Decleir was member <strong>and</strong>/or president of several<br />

scientific societies: Scientific Committee on GIS for<br />

F<strong>l<strong>and</strong></strong>ers, Council for Geographical Information F<strong>l<strong>and</strong></strong>ers,<br />

Commission Sciences of the Earth (National Scientific<br />

Foundation, F<strong>l<strong>and</strong></strong>ers), National Committee for Antarctic<br />

Research, National Committee for the IPY, SCAR<br />

(Scientific Committee on Antarctic Research) work<strong>in</strong>g<br />

group on Glaciology <strong>and</strong> Geophysics, Belgian (National<br />

Scientific Foundation, F<strong>l<strong>and</strong></strong>ers) representative to the<br />

European Polar Board (EPB) <strong>and</strong> the European Polar<br />

Consortium, Committee of Environmental Protection<br />

(CEP) at the ATCM (Antarctic Treaty Consultative<br />

Meet<strong>in</strong>g).<br />

In May 1998 he organised the International Symposium at<br />

the occasion of the 100 th anniversary of the „Belgica‟<br />

expedition. At this occasion Hugo Decleir edited the book<br />

„The Belgium Expedition Centennial: Perspectives on<br />

Antarctic Science <strong>and</strong> History‟ (VUB press, 366 pp.,<br />

2001). He was also editor of the Dutch („Roald Amundsens<br />

Belgica-Dagboek‟, Hadewych, 230 pp. 1998) <strong>and</strong> English<br />

(Roald Amundsen‟s Belgica Diary, Bluntisham Books, 208<br />

pp.,1999) translation of Roald Amundsen‟s diary on the<br />

same expedition.<br />

Hugo Decleir is co-founder (2002) of the „International<br />

Polar Foundation‟ (IPF). This foundation was charged by<br />

the Belgian government with the construction <strong>and</strong><br />

f<strong>in</strong>anc<strong>in</strong>g of a new Belgian scientific research station on<br />

Antarctic. The <strong>in</strong>auguration of this station is due by 2008,<br />

dur<strong>in</strong>g the International Polar Year (2007-2008).<br />

M. Van Molle<br />

OBITUARY<br />

Prof. Em. Robert Maréchal passed<br />

away <strong>in</strong> Ghent on December 5, 2006<br />

R. Maréchal was born <strong>in</strong> Ghent on January 11, 1926. After<br />

his secondary school <strong>studies</strong> <strong>in</strong> his home city, he received<br />

his professional education <strong>in</strong> geology at the local<br />

university. He graduated with a licence degree <strong>in</strong> 1948,<br />

earned his Ph.D. diploma <strong>in</strong> 1951 <strong>and</strong> became „aggregate‟<br />

Higher Education at the very end of the fifties. He was<br />

laureate of the Inter-University Competition 1947-1949<br />

<strong>and</strong> was awarded the Wetrems prize by the Belgian Royal<br />

Academy <strong>in</strong> 1960.<br />

R. Maréchal began his academic career as an assistant<br />

(1948) <strong>and</strong> “work leader” (1951) of the Belgian Centre for<br />

Soil Survey (head : the late Prof. Dr. R. Tavernier). In<br />

1954 he was appo<strong>in</strong>ted “work leader” at the Geological<br />

Institute of the State University of Ghent. In 1960 followed<br />

his nom<strong>in</strong>ation as Associate Professor <strong>and</strong> three years later<br />

he became Full Professor. From October 1965 onwards he<br />

was the head of the Department of Dynamic <strong>and</strong><br />

Stratigraphic Geology, <strong>and</strong> subsequently became director<br />

of the Laboratory of Geology. R. Maréchal‟s scientific<br />

work focused on soil mapp<strong>in</strong>g, hydrogeologic research,<br />

geological survey, <strong>and</strong> stratigraphy of the Tertiary of<br />

Belgium.<br />

For almost thirty years (1963-1991), R. Maréchal was<br />

member of the Academic Teach<strong>in</strong>g Staff of the<br />

International Tra<strong>in</strong><strong>in</strong>g Centre for Post-Graduate Soil<br />

Scientists (ITC) of the University of Ghent. In this<br />

position, he was <strong>in</strong> charge of a basic course on geology <strong>and</strong><br />

petrography of parent materials <strong>and</strong> was particularly<br />

helpful to his students. Dur<strong>in</strong>g his long university career,<br />

he served on several faculty committees, supervised<br />

research projects, <strong>and</strong> was an active <strong>and</strong> honoured<br />

member, secretary, vice-president <strong>and</strong>/or president of many<br />

national committees, commissions, professional<br />

associations <strong>and</strong> other scientific bodies <strong>in</strong> the field of earth<br />

sciences. All these activities lasted until his retirement on<br />

October 1, 1991.<br />

The friends, colleagues, ITC-students <strong>and</strong> personnel of<br />

the former Laboratory of Geology of the University of<br />

Ghent will remember Prof. Maréchal as a man of<br />

exemplary scientific rigour <strong>and</strong> <strong>in</strong>tellectual <strong>in</strong>tegrity, <strong>and</strong>,<br />

above all, as a very modest, tactful, generous <strong>and</strong><br />

underst<strong>and</strong><strong>in</strong>g person.<br />

P. De Paepe<br />

- 3 -


STAFF NEWS<br />

INTERESTING LINKS<br />

The International Union of Soil Science (IUSS) has an<br />

electronic newsletter that can be consulted onl<strong>in</strong>e at the<br />

IUSS-webpages : http://www.iuss.org/<strong>in</strong>dex.htm. If you<br />

wish to receive the newsletter by e-mail, send your request<br />

to be listed to Alfred.hartem<strong>in</strong>k@wur.nl.<br />

The ASA-CSSA-SSSA offers a "free science policy e-<br />

newsletter that you can read at the Society Web Pages.<br />

You can also subscribe onl<strong>in</strong>e with your e-mail address at<br />

the follow<strong>in</strong>g site : http://www.asa-cssasssa.org/public_affairs_sspr.html<br />

to receive bi-weekly<br />

copies.<br />

The L<strong>and</strong>-Water-L electronic newsletter is a free service<br />

from the FAO L<strong>and</strong> <strong>and</strong> Water Development Division,<br />

aimed at provid<strong>in</strong>g up-to-date <strong>in</strong>formation <strong>in</strong> the field of<br />

<strong>l<strong>and</strong></strong> <strong>and</strong> water development. To subscribe, send an e-mail<br />

to mailserv@mailserv.fao.org, leave the subject blanc <strong>and</strong><br />

write : SUBSCRIBE <strong>l<strong>and</strong></strong>-<strong>and</strong>-water-L your address.<br />

Former issues of the newsletter are available at<br />

http://www.fao.org/ag/agl/newsletter/default.stm.<br />

WORLD SOIL DAY<br />

FOCUS<br />

In 2002, the International Union of Soil Science (IUSS)<br />

made a resolution to propose the 5th of December as the<br />

World Soil Day to honour His Majesty the K<strong>in</strong>g of<br />

Thai<strong>l<strong>and</strong></strong> for his promotion of soil science <strong>and</strong> soil<br />

<strong>resources</strong> conservation. The 5 th of December is the<br />

birthday of His Majesty. S<strong>in</strong>ce then the IUSS has <strong>in</strong>itiated<br />

various activities to proclaim the 5 th December as the<br />

World Soil Day. The World Soil Day will be used to<br />

advocate the use <strong>and</strong> need of soils for human survival <strong>and</strong><br />

its susta<strong>in</strong>able management. We aim to draw more<br />

attention for the natural resource on which all life depends<br />

: the soil !<br />

work<strong>in</strong>g <strong>in</strong> these <strong>and</strong> related fields <strong>and</strong> of others with<br />

strong ties to the region. Colleagues <strong>in</strong>terested <strong>in</strong> be<strong>in</strong>g<br />

<strong>in</strong>cluded <strong>in</strong> the database should contact m.pillay@icsuafrica.org<br />

<strong>and</strong> secretariat@icsu-africa.org.<br />

DIGITAL SOIL MAPPING<br />

The second Global Digital Soil Mapp<strong>in</strong>g workshop will be<br />

held <strong>in</strong> Rio de Janeiro <strong>in</strong> July 2006. The workshop will<br />

focus on countries with sparse spatial data <strong>in</strong>frastructures<br />

but a range of topics related to soil mapp<strong>in</strong>g will be<br />

presented <strong>and</strong> discussed. The Digital Soil Mapp<strong>in</strong>g<br />

work<strong>in</strong>g group is a new work<strong>in</strong>g group of the IUSS. For<br />

further <strong>in</strong>formation on this IUSS work<strong>in</strong>g group <strong>and</strong> the<br />

Rio Workship see their website :<br />

http://www.digitalsoilmapp<strong>in</strong>g.org/.<br />

VLIR-ICP GET TOGETHER DAY 2005<br />

Each year the Flemish Interuniversity Council (VLIR)<br />

organizes together with a Flemish university the VLIR ICP<br />

Get Together Day. This year the ICP Get Together Day<br />

was organized together with the International Relations <strong>and</strong><br />

Mobility Office of the Vrije Universiteit Brussel. It took<br />

place on December 2, 2005 <strong>in</strong> Brussels. The Get Together<br />

Day is a special day for all <strong>in</strong>ternational students who are<br />

awarded a VLIR scholarship. The aim of this <strong>in</strong>itiative is to<br />

have a meet <strong>and</strong> greet between people from all corners of<br />

the world while offer<strong>in</strong>g fun activities to them. There were<br />

about 350 participants count<strong>in</strong>g almost 45 nationalities<br />

from Lat<strong>in</strong>-America, Europe, Asia <strong>and</strong> Africa.<br />

NETWORKING IN AFRICA<br />

ICSU (The International Council of Science) has recently<br />

established a regional office for Africa under the<br />

leadership of Sospeter Muhongo s.muhongo@icsuafrica.org.<br />

The office is seek<strong>in</strong>g to coord<strong>in</strong>ate the work of<br />

African scientists <strong>and</strong> those from other parts of the<br />

globe actively <strong>in</strong>volved <strong>in</strong> research <strong>and</strong> capacity build<strong>in</strong>g<br />

<strong>in</strong> the Africa region. Four priority areas have been<br />

identified : 1. Health <strong>and</strong> Human Well-be<strong>in</strong>g, 2.<br />

Susta<strong>in</strong>able Energy, 3. Natural <strong>and</strong> Human-<strong>in</strong>duced<br />

Hazards <strong>and</strong> Disasters <strong>and</strong> 4. Global Change. The first task<br />

is to establish a database of African scientists who are<br />

The day started with a visit to the exhibition "Made <strong>in</strong><br />

Belgium", an expo about the history of Belgium. Then<br />

there was a lunch <strong>and</strong> an <strong>in</strong>ternational quiz called "The<br />

smartest team of the world" <strong>in</strong> La Tentation, an authentic<br />

banquet hall <strong>in</strong> the center of Brussels. Every team had to<br />

work together to collect as much correct answers as<br />

possible.<br />

- 4 -


STAFF NEWS<br />

Afterwards Rector B. Van Camp, Chairman of VLIR,<br />

addressed a word of welcome to the students dur<strong>in</strong>g the<br />

academic session at Campus Etterbeek. Dur<strong>in</strong>g this session<br />

the w<strong>in</strong>ners of the VLIR Scholar Contest were announced.<br />

By the start of the academic year VLIR challenged all ICP<br />

<strong>and</strong> IOB scholars to send them a design for a Christmas<br />

<strong>and</strong> New Year‟s greet<strong>in</strong>gs‟ card or to send them an<br />

animated movie/presentation about their experiences as a<br />

foreign student : what does it mean to live <strong>in</strong> Belgium <br />

The w<strong>in</strong>ner of each category received a travel cheque of €<br />

500.<br />

Later on d<strong>in</strong>ner was served at the university restaurant<br />

where the students could taste the typical Belgian fries.<br />

After d<strong>in</strong>ner all participants were <strong>in</strong>vited for a party <strong>in</strong> the<br />

Kultuurkaffee to dance the night away on <strong>in</strong>ternational<br />

music.<br />

To conclude, for many December 2, 2005 will be a day to<br />

remember !<br />

GUEST LECTURERS<br />

October 1, 2004 : Prof. Em. A. Z<strong>in</strong>ck from ITC Enschede<br />

gave the open<strong>in</strong>g lecture of the academic year entitled :<br />

"Soils, Soil Information <strong>and</strong> Society"<br />

December 10, 2004 : K. Lamorski, A. Bieganowski, R.T.<br />

Walczak <strong>and</strong> Nosalewicz gave lectures entitled :<br />

"Specificity <strong>and</strong> the needs of st<strong>and</strong>ardization of<br />

agro<strong>physical</strong> methods", "Heat flux meter, accuracy of<br />

measurements, Modell<strong>in</strong>g <strong>and</strong> sensitivity analysis", "Effect<br />

of soil compaction on root <strong>and</strong> shoot growth <strong>and</strong> water<br />

uptake of wheat".<br />

STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

COMPLEMENTARY AND ADVANCED STUDIES<br />

IN PHYSICAL LAND RESOURCES 2005-2006<br />

Complementary Studies<br />

<strong>in</strong> Physical L<strong>and</strong> Resources<br />

Option :<br />

Soil Science<br />

Option : Analysis of<br />

Mr. Adortse Peter<br />

Physical L<strong>and</strong> B.Sc. Agriculture Resources<br />

Post Office Box 488,<br />

G.P.H.A., Tema, Ghana<br />

E-mail :<br />

Peter.Adortse@UGent.be<br />

Mr. Alam Md. Nazmul<br />

B.Sc. Agriculture<br />

Shamkhali, P.O. Hizalfala,<br />

Kotwali, Barisal, Bangladesh<br />

E-mail :<br />

Md.Nazmul.Alam@UGent.be<br />

Ms. Alipour Rounak<br />

Bachelor Civil Eng., Islamic<br />

Azad University, Iran<br />

E-mail :<br />

rounakalipour@yahoo.com<br />

Mr. Amakor Xystus Ndubuisi<br />

C.<br />

B. Techn. (Soil Sc. & Techn.)<br />

P.M.B. 1526, 40016 Owerri,<br />

Imo State, Nigeria<br />

E-mail :<br />

Amakor.Ndubuisi@UGent.be<br />

Ms. Anggria L<strong>in</strong>ca<br />

B.Sc. Chemistry<br />

Jl. Arzimar 1, n° 9, Perumnas<br />

Bantarjati, 16152 Bogor, Jawa<br />

Barat, Indonesia<br />

E-mail :<br />

L<strong>in</strong>ca.Anggria@UGent.be<br />

Ms. Begum Ara Shamim<br />

M.Sc. Horticulture<br />

Regional Agricultural<br />

Research Station, 2000<br />

Jamalpur, Bangladesh<br />

E-mail :<br />

ShamimAra.Begum@UGent.<br />

be<br />

Mr. Botula Manyala Yves-<br />

Dady<br />

Ir. Agronome<br />

P.O. Box 170, K<strong>in</strong> XI,<br />

K<strong>in</strong>shasa, Congo D.R.<br />

E-mail :<br />

YvesDady.BotulaManyala@U<br />

Gent.be<br />

Mr. Eshetu Belayneh Bruk<br />

B.Sc. Plant Science<br />

Alemaya University, P.O. Box<br />

284, Alemaya, Oromiya,<br />

Ethiopia<br />

E-mail :<br />

Bruk.Eshetu@UGent.be<br />

Mr. Funwi Joshua<br />

B.Sc. Zoology<br />

P.O. Box 275, Bamenda,<br />

North West Prov<strong>in</strong>ce,<br />

Cameroon<br />

E-mail :<br />

Joshua.Funwi@UGent.be<br />

Ms. Gharahi Ghehi Nasr<strong>in</strong><br />

B.Sc. Agricultural Eng<strong>in</strong>eer<br />

N° 124, Ostad Homaei St.<br />

Ahmad Abad, St. Esfahan,<br />

Esfahan, Iran<br />

E-mail : Nasr<strong>in</strong>.GharahiGhehi<br />

@UGent.be<br />

- 5 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

Ms. Hosse<strong>in</strong>i Joshanizadeh<br />

Zahra<br />

B. Agr. Eng., Yazd University,<br />

Iran<br />

E-mail : hsodaee@yahoo.com<br />

Mr. Mpulila Thadeo<br />

B.Sc. Agronomy<br />

P.O. Box 3120, Morogoro,<br />

Tanzania<br />

E-mail :<br />

Thadeo.Mpulila@UGent.be<br />

Mr. Velghe Filip<br />

Bio-ir. Milieutechnologie<br />

V<strong>and</strong>ewallestraat 7, 8810<br />

Lichtervelde<br />

E-mail :<br />

Filip.Velghe@UGent.be<br />

Mr. Islam Mohammad<br />

Monirul<br />

B.Sc. Agriculture, M.Sc.<br />

Agriculture<br />

113, R.K. Mission Road,<br />

Nawmohall, 2200<br />

Mymens<strong>in</strong>gh, Bangladesh<br />

E-mail :<br />

MohammadMonirul.Islam@<br />

UGent.be<br />

Ms. Jalilpour Marzieh<br />

B.Sc. Geology, Isfahan<br />

University, Iran<br />

E-mail :<br />

m_jalilpoor@yahoo.com<br />

Mr. Ngwira Robert Amos<br />

B.Sc. Agriculture (Crop Sci.)<br />

Chitedze Research Station,<br />

P.O. Box 158, Lilongwe,<br />

Malawi<br />

E-mail :<br />

Robert.Ngwira@UGent.be<br />

Ms. Nuha Abdalla Mohamed<br />

K.<br />

B.Sc. Chemistry, M.Sc.<br />

Chemistry<br />

P.O. Box 3881, Wad Medani,<br />

Gezira, Sudan<br />

E-mail :<br />

AbdallaMohamed.Nuha@<br />

UGent.be<br />

Mr. Wickramas<strong>in</strong>ghe<br />

Mudiyanselage Diana Ranjan<br />

W.<br />

B.Sc. Agriculture<br />

Sri Lanka<br />

E-mail :<br />

Diana.Ranjan@UGent.be<br />

Ms. Wollelo Tigist Oicha<br />

B.Sc. Soil <strong>and</strong> Water<br />

Conservation<br />

P.O. Box 231, Mekelle,<br />

Ethiopia<br />

E-mail :<br />

TigistOicha.Wollelo@UGent.<br />

be<br />

Ms. Katuwal Sheela<br />

B.Sc. Agr. Eng. (Soil Cons. &<br />

Watershed Mant.)<br />

Purwanchal Campus, dharan-<br />

8, Sunsari, Nepal<br />

E-mail :<br />

Sheela.Katuwal@UGent.be<br />

Mr. L<strong>in</strong>h Nguyen Si<br />

B. Environmental Sci.<br />

RIFAV, Gia Lam Res.<br />

Experimental Centre of Fruits<br />

<strong>and</strong> Vegetables, Trau Quy, Gia<br />

Lam district, Hanoi, Vietnam<br />

E-mail :<br />

L<strong>in</strong>h.NguyenSy@UGent.be<br />

Ms. Manimel Wadu<br />

Chathurika Wilas<strong>in</strong>i Mihiri<br />

B.Sc. Agriculture<br />

Madawa Kalapaya, n° 174/8,<br />

81000 Bogahawatta,<br />

Walgiama-South, Matara, Sri<br />

Lanka<br />

E-mail :<br />

MihiriC.W.;ManimelWadu@<br />

UGent.be<br />

Mr. Mohammed El Sadig<br />

B.Sc. Agricultural Sciences<br />

L<strong>and</strong> & Water Research<br />

Centre, P.O. Box 388, Wad<br />

Medani, Sudan<br />

E-mail : Elsadig.Mohammed@<br />

UGent.be<br />

Ms. Salibay Ligtas Asuncion<br />

B.Sc. Agriculture (Soil Sci.)<br />

Lap<strong>and</strong>ay Agricultural &<br />

Development Corporation,<br />

Research <strong>and</strong> Development<br />

Department, M<strong>and</strong>ug,<br />

Buhang<strong>in</strong> District, 8000<br />

Davao City, Philipp<strong>in</strong>es E-<br />

mail :<br />

Ma.AsuncionLigtas.Salibay@<br />

UGent.be<br />

Mr. Sam<strong>in</strong>athan Boopathi<br />

Kumar<br />

B.Sc. Horticulture<br />

M.Sc. Water Sci. & Techn.<br />

150 Shishir Hostel, IARI, Pusa<br />

Campus, 110012 New Delhi,<br />

India<br />

E-mail :<br />

Boopathi.Kumar@UGent.be<br />

Mr. Shah Syed Haleem<br />

B.Sc. Agr. Eng. (Soil Sci.)<br />

M.Sc. Agriculture (Soil Sci.)<br />

Dept. of Soil <strong>and</strong><br />

Environmental Sciences,<br />

NFWP Agricultural University<br />

Peshawar, 25000 Peshawar,<br />

Pakistan<br />

E-mail :<br />

SyedHaleem.Shah@UGent.be<br />

Ms. Tytgat Nele<br />

Lic. Geology<br />

Hulstboomstraat 3An 8760<br />

Meulebeke<br />

E-mail :<br />

Nele.Tytgat@UGent.be<br />

Option :<br />

Eng<strong>in</strong>eer<strong>in</strong>g Geology<br />

Option : Analysis Mr. Adhikari of Surendra<br />

B. Agricultural Eng<strong>in</strong>eer<br />

Physical L<strong>and</strong> c/o Mr. prakash Resources Adhikari,<br />

Dept. of Electrical Eng., Joe<br />

Pulchowk Campus, Katm<strong>and</strong>u,<br />

Nepal<br />

E-mail :<br />

Surendra.Adhikari@UGent.be<br />

Mr. Bayasgalan Gantulga<br />

B.Sc. Physics & Applied<br />

Ecology<br />

Apartment 25, build<strong>in</strong>g 17,<br />

Baga Toiruu Street, 210646<br />

Ulaanbaatar City, Mongolia<br />

E-mail :<br />

Gantulga.Bayasgalan@UGent.<br />

be<br />

Mr. Bui Le V<strong>in</strong>h<br />

B.L<strong>and</strong> Adm<strong>in</strong>.<br />

Dept. Of L<strong>and</strong> Resources <strong>and</strong><br />

Environment, Hanoi<br />

Agricultural University,<br />

Vietnam<br />

E-mail :<br />

LeV<strong>in</strong>h.Bui@UGent.be<br />

Mr. Esaifan Muayad<br />

B.Sc. Chemistry<br />

University of Jordan,<br />

Chemistry Dept., Queen Rania<br />

El-Abdallah Street, 11942<br />

Amman, Jordan<br />

E-mail :<br />

Muayad.Esaifan@UGent.be<br />

- 6 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

Mr. Le Nguyen Hoang<br />

B.Sc. Geophysics<br />

Remote Sens<strong>in</strong>g <strong>and</strong><br />

Geomatics Dept., Res. Inst. of<br />

Geol. & M<strong>in</strong>. Res., Nguyen<br />

Trai-Thanh Xuan Dist., Hanoi,<br />

Vietnam.<br />

E-mail : hoang_ln@yahoo.com<br />

Ms. Nguyen Thi Thuy<br />

B.Sc. Geology (Geo-<br />

Chemistry)<br />

54, Chien Thang Road, Xuan,<br />

Hanoi, Vietnam<br />

E-mail :<br />

Thuy.NguyenThi@UGent.be<br />

Mr. Qudaih Ahmed A.<br />

B.Sc. Geology/Water<br />

Resources<br />

El Majed St., 14-4, Khuza'a,<br />

Gaza Strip, Palest<strong>in</strong>e<br />

E-mail :<br />

Ahmed.Qudaih@UGent.be<br />

Mr. Zulu Joseph Dryson Saul<br />

B.M<strong>in</strong>.Sci. Geology<br />

Great East Road, UNZA,<br />

School of M<strong>in</strong>es, Geology<br />

Dept., Box 32379, 10101<br />

Lusaka, Zambia<br />

E-mail :<br />

JosephDrysonSaul.Zulu@<br />

UGent.be<br />

Option : Analysis of<br />

Physical L<strong>and</strong> Resources<br />

Advanced Studies<br />

<strong>in</strong> Physical L<strong>and</strong> Resources<br />

Option :<br />

Soil Science<br />

Option : Analysis of<br />

Mr. Adhikari Kab<strong>in</strong>dra<br />

Physical L<strong>and</strong> B.Sc. Agriculture Resources<br />

Geetanangar-4, Dgunagar,<br />

Chitwan, Nepal<br />

E-mail :<br />

Kab<strong>in</strong>dra.Adhikari@UGent.be<br />

Mr. Bari Md. Khaled Nasimul<br />

M.Sc. Agronomy<br />

Upazila Agriculture Office,<br />

Lalmatighat, Borogola, 5800<br />

Bogra, Bangladesh<br />

E-mail :<br />

Md.KhaledNasimul.Bari@<br />

UGent.be<br />

Option : Analysis of<br />

Physical L<strong>and</strong> Resources<br />

Ms. Bonne Kathelijne P.M.D.<br />

Lic. Geology<br />

Kon<strong>in</strong>g<strong>in</strong> Astridstraat 12, 9250<br />

Waasmunster, Belgium<br />

E-mail :<br />

Kathelijne.Bonne@UGent.be<br />

Option : Analysis Mr. Chilongo of Kal<strong>in</strong>ga<br />

B.Sc. Agriculture<br />

Physical L<strong>and</strong> Resources<br />

Prof. Master Rural L<strong>and</strong><br />

Ecology Survey<br />

Box 350001, Chilanga,<br />

Lusaka, Zambia E-mail :<br />

Kal<strong>in</strong>ga.Chilongo@UGent.be<br />

Option : Analysis Mr. Dabalos of Vernon Cacacho<br />

B.Sc. Agricultural Eng<strong>in</strong>eer<br />

Physical L<strong>and</strong> Blk. 26, Resources<br />

lot-8, Wonder<strong>l<strong>and</strong></strong><br />

Homes Subdivision, Sta<br />

Teresa, Iguig, 3504 Cagayan,<br />

The Philipp<strong>in</strong>es<br />

E-mail :<br />

VernonCacacho.Dabalos@<br />

UGent.be<br />

Option : Analysis of<br />

Mr. Duchatelet Jérémie<br />

Physical L<strong>and</strong> Lic. Biology Resources<br />

Rue des Tanneurs 12, 7730<br />

Estaimbourg, Belgium<br />

E-mail :<br />

Jeremie.Duchatelet@UGent.be<br />

Option : Analysis Mr. Herath Mudiyanselage of<br />

Saman Kumara Herath<br />

Physical L<strong>and</strong> B.Sc. Agricultural Resources Sciences<br />

Sisirasewana, Kudawa,<br />

Aluthwela South, 90150<br />

Diyatalawa, Uva, Sri Lanka<br />

E-mail :<br />

Saman.Kumara@UGent.be<br />

Mr. Kader MD Abdul<br />

M.Sc. Soil Science<br />

Department of Soil Science,<br />

Bangladesh Agricultural<br />

University, Mymens<strong>in</strong>gh 2202,<br />

Bangladesh<br />

E-mail :<br />

MDAbdul.Kader@UGent.be<br />

Option : Analysis Mr. Messiga of Aime Jean<br />

Nyamsi<br />

Physical L<strong>and</strong> ir. Agronome Resources<br />

P.O. Box 30517, Messa,<br />

Yaoundé, Cameroon<br />

E-mail :<br />

AimeJeanNyamsi.Messiga@<br />

UGent.be<br />

Option : Analysis of<br />

Physical L<strong>and</strong> Resources<br />

- 7 -<br />

Mr. Muj<strong>in</strong>ya Bazirake Basile<br />

Ingénieur Agronome<br />

Kasangulu 64, Lubumbashi,<br />

D.R. Congo<br />

E-mail :<br />

Basile.Muj<strong>in</strong>yabazirake@<br />

UGent.be<br />

Mr. Mureithi Stephen<br />

Mwangi<br />

B.Sc. Range Management<br />

P.O. Box 11421, c/o W<strong>in</strong>nie,<br />

00400 Nairobi, Kenya<br />

E-mail :<br />

StephenMwangi.Mureithi@<br />

UGent.be<br />

Ms. Ne<strong>in</strong>a Dora<br />

B.Sc. Agriculture<br />

Soil Science Dept., University<br />

Post Office, Cape Coast,<br />

Ghana<br />

E-mail :<br />

Dora.Ne<strong>in</strong>a@UGent.be<br />

Mr. Neira Mendez Fredy<br />

Hern<strong>and</strong>o<br />

Agrologist<br />

C/o Manuel Olarte, Calle<br />

53#81-36, Piso 2, Bogota,<br />

Colombia<br />

E-mail :<br />

FredyHern<strong>and</strong>o.NeiraMendez<br />

@UGent.be<br />

Ms. Nguyen M<strong>in</strong>h Phuong<br />

B.Sc. L<strong>and</strong> Management<br />

2/5A Le Lai Street, Cantho,<br />

Vietnam<br />

E-mail :<br />

M<strong>in</strong>hPhuong.Nguyen@UGent.<br />

be<br />

Mr. Nicosia Cristiano<br />

Laurea Archeology<br />

Via Cilento 10, 36100<br />

Vicenza, Italy<br />

E-mail :<br />

cristianonicosia@libero.it<br />

Option : Analysis Mr. Uzoma K<strong>in</strong>gsley of Ch<strong>in</strong>yere<br />

B. Agricultural Technology<br />

Physical L<strong>and</strong> P.M.B. 1526 Resources Owerri, Soil<br />

Science & Techn. Dept., Uni.<br />

Of Techn. Owerri, Imo State,<br />

Nigeria. E-mail :<br />

K<strong>in</strong>gsleyCh<strong>in</strong>yere.Uzoma@<br />

UGent.be<br />

Mr. Wickramas<strong>in</strong>ghe<br />

Mudiyanselage Diana Ranjan<br />

W.<br />

B.Sc. Agriculture<br />

Sri Lanka<br />

E-mail :<br />

Diana.Ranjan@UGent.be


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

Mr. Yadessa Sonessa Mergia<br />

PG diploma Groundwater<br />

Resources Exploration<br />

P.O. Box 1032, Awassa,<br />

Sidama, Ethiopia<br />

E-mail :<br />

Mergia.YadessaSonessa@<br />

UGent.be<br />

Mr. Youssef Ali Amer Ali<br />

B.Sc. Agriculture<br />

87, Masr Street, apartment n°<br />

1, Ismailia, Egypt<br />

E-mail :<br />

Ali.YoussefAliAmer@UGent.<br />

be<br />

Option :<br />

Eng<strong>in</strong>eer<strong>in</strong>g Geology<br />

Ms. Alfarrah Nawal<br />

B.Sc. Geology<br />

P.O. Box 16418, 7th April<br />

University, Zawia, Libya<br />

E-mail :<br />

Nawal.Alfarrah@UGent.be<br />

Option : Analysis of<br />

Mr. Kayastha Prab<strong>in</strong><br />

Physical L<strong>and</strong> B.Eng. Civil Resources Eng<strong>in</strong>eer<strong>in</strong>g<br />

28 Bhagwan Bahal Marg,<br />

Thamel, Kathm<strong>and</strong>u, Nepal<br />

E-mail :<br />

Prab<strong>in</strong>.Kayastha@UGent.be<br />

Mr. Ndofor Akongnui Fai<br />

B.Sc. Geology<br />

P.O. Box 18, Bambili, N.W.<br />

Prov<strong>in</strong>ce, Cameroon<br />

E-mail :<br />

Fai.NdoforAkongnui@UGent.<br />

be<br />

Option : Analysis Mr. Shaheen of Sami<br />

B.Sc. Geology/Chemistry<br />

Physical L<strong>and</strong> Resources<br />

54-Abu Baker El-Sedeek St.,<br />

The Sea, El-Nusairat, Gaza<br />

strip, Palest<strong>in</strong>ian Authority<br />

(PA), Palest<strong>in</strong>e<br />

E-mail : sshaheen@vub.ac.be<br />

M.Sc. promoted 2005<br />

Physical L<strong>and</strong> Resources<br />

Option :<br />

Analysis of Physical L<strong>and</strong> Resources<br />

Ms. Fehér Olga<br />

MORPHOLOGICAL AND CHEMICAL<br />

CHARACTERIZATION OF SOILS DEVELOPED<br />

ON ANDESITIC ROCKS IN SOUTH-EASTERN<br />

CARPATHS<br />

Promoter(s) : R. Langohr<br />

Contact address : Budapest 1107 somfa Köz 10.v.15,<br />

Hungary<br />

Abstract :<br />

In the Miocene <strong>and</strong>esitic area of SW-Carpaths (Gurghiu Mounta<strong>in</strong>s)<br />

10 representative soil profiles have been studied <strong>in</strong> detail. Based on<br />

macromorphological, micromorphological <strong>and</strong> chemical properties, it<br />

was possible to identify that the soils are composed of two major types<br />

of soil material: a relict type with crystall<strong>in</strong>e clay fraction <strong>and</strong> a<br />

strongly amorphous type. Where the latter predom<strong>in</strong>ates, the soils bear<br />

the characteristics of a Si<strong>l<strong>and</strong></strong>ic (WRB, 1998 Soil Classification)<br />

diagnostic horizon. Four ma<strong>in</strong> hypotheses were exam<strong>in</strong>ed to expla<strong>in</strong><br />

the orig<strong>in</strong> <strong>and</strong> mode of deposition of the soil parent material of the<br />

Andosols: (1) direct weather<strong>in</strong>g from compact <strong>and</strong>esite rock, (2) eolian<br />

sedimentation, (3) mudflow <strong>and</strong> (4) glacial deposition. It is concluded<br />

that only the hypothesis of glacial transport <strong>and</strong> deposition can expla<strong>in</strong><br />

the complete set of properties of the studied Andosol profiles.<br />

Mr. Koy Kasongo Ruben<br />

IMPACT OF PLANTED ACACIA FOREST ON<br />

THE CHEMICAL FERTILITY OF SANDY SOILS<br />

OF THE BATEKE PLATEAU (D.R. CONGO)<br />

Promoter(s) : E. Van Ranst<br />

Contact address : P.O. Box 190, XI K<strong>in</strong>shasa, R.D.<br />

Congo<br />

Abstract :<br />

The s<strong>and</strong>y soils occurr<strong>in</strong>g on the Bateke plateau have a m<strong>in</strong>eralogical<br />

composition limited to quartz, kaol<strong>in</strong>ite <strong>and</strong> some residual oxides of<br />

Al <strong>and</strong> Ti, which results <strong>in</strong> a low chemical fertility <strong>and</strong> a low water<br />

hold<strong>in</strong>g capacity. Overall, these soils are acid, have a low CEC <strong>and</strong> a<br />

low base saturation.<br />

The results of this research allow to establish a more specific chemical<br />

management, tak<strong>in</strong>g <strong>in</strong>to account the impact of the acacia trees on the<br />

chemical soil quality. It was found that the soil chemical fertility status<br />

significantly <strong>in</strong>creased with the age of the forest. The N-fix<strong>in</strong>g Acacia<br />

trees act as a major source for organic matter <strong>in</strong>clud<strong>in</strong>g nitrogen,<br />

hence <strong>in</strong>creas<strong>in</strong>g the soil O.C content <strong>and</strong> decreas<strong>in</strong>g the C/N ratio.<br />

Together with the <strong>in</strong>crease <strong>in</strong> organic matter, significant <strong>in</strong>crease <strong>in</strong><br />

CEC <strong>and</strong> sum of basic cations was observed.<br />

Study<strong>in</strong>g the charge properties of the Bateke soils, it was found that<br />

the pH 0 was systematically lower than the soil pH <strong>and</strong> decreases with<br />

<strong>in</strong>creas<strong>in</strong>g organic matter content. Furthermore, the surface charge is<br />

largely pH dependent <strong>and</strong> <strong>in</strong>creases with <strong>in</strong>creas<strong>in</strong>g organic matter<br />

content. The soil underneath the 17 years old Acacia forest has the<br />

highest fertility level, <strong>in</strong>dicat<strong>in</strong>g the importance of organic matter on<br />

the fertility of the studied soils.<br />

The chemical fertility of the Bateke soils can be further improved by<br />

better manag<strong>in</strong>g the organic matter <strong>and</strong> add<strong>in</strong>g m<strong>in</strong>eral fertilizers to<br />

restore the soil cation balance.<br />

Mr. Lambiv Dzemua<br />

MINERALOGICAL AND<br />

MICROMORPHOLOGICAL<br />

CHARACTERIZATION OF WEATHERED<br />

SERPENTINITE FROM SOUTH-EAST<br />

CAMEROON<br />

Promoter(s) : E. Van Ranst, F. Mees<br />

Contact address : B.P. 11555 Yaoundé, Cameroon<br />

Abstract :<br />

M<strong>in</strong>eralogical <strong>and</strong> micromorphological characteristics of serpent<strong>in</strong>ite<br />

at different weather<strong>in</strong>g stages <strong>in</strong> Southeast Cameroon were studied<br />

us<strong>in</strong>g chemical, XRD <strong>and</strong> micromorphological analyses with the aim<br />

of underst<strong>and</strong><strong>in</strong>g the occurrence of Co, Cr, Mn <strong>and</strong> Ni <strong>in</strong> the<br />

- 8 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

weathered material. The serpent<strong>in</strong>ite is characterised by antigorite,<br />

magnetite <strong>and</strong> magnesite conta<strong>in</strong><strong>in</strong>g significant Co, Cr <strong>and</strong> Ni. The<br />

serpent<strong>in</strong>ite is overla<strong>in</strong> by a thick highly weathered material with a<br />

granular microstructure <strong>and</strong> gibbsite coat<strong>in</strong>gs <strong>and</strong> <strong>in</strong>fill<strong>in</strong>gs. Three<br />

units are dist<strong>in</strong>guishable <strong>in</strong> the weathered material: (1) an upper, very<br />

dusky red (2.5YR 2.5/2, moist) unit, conta<strong>in</strong><strong>in</strong>g kaol<strong>in</strong>ite, gibbsite,<br />

iron (hydr)oxides <strong>and</strong> quartz; (2) a second unit conta<strong>in</strong><strong>in</strong>g pisolithic<br />

gravel; <strong>and</strong> (3) a strong brown (7.5YR 5/8, dry) bottom clayey unit,<br />

with a soft consistency conta<strong>in</strong><strong>in</strong>g solely kaol<strong>in</strong>ite <strong>and</strong> iron<br />

(hydr)oxides. The <strong>in</strong>vestigated elements, Co, Cr, Mn <strong>and</strong> Ni, occur<br />

throughout the weathered material, with important amounts <strong>in</strong> the<br />

bottom unit. They occur <strong>in</strong> the lattices of neoformed <strong>and</strong>/or <strong>in</strong>herited<br />

sesquioxides <strong>and</strong> clays or are adsorbed onto these m<strong>in</strong>erals.<br />

Mr. Tafesse Kebede Demeke<br />

LAND SUITABILITY ASSESSMENT OF THE<br />

DEBREZEIT AGRICULTURAL RESEARCH<br />

FARMLAND FOR THE CULTIVATION OF<br />

WHEAT AND TEFF (ETHIOPIA)<br />

Promoter(s) : E. Van Ranst<br />

Contact address : National Soil Research Center,<br />

P.O. Box 144, Addis Ababa, Ethiopia<br />

Abstract :<br />

In this study, the yields of wheat <strong>and</strong> teff <strong>in</strong> Debrezeit Agricultural<br />

Research center were simulated us<strong>in</strong>g a three-hierarchical level crop<br />

growth model. The radiation-thermal production potential was quite<br />

high, be<strong>in</strong>g 6.62 <strong>and</strong> 8.34 t/ha dry gra<strong>in</strong>s for wheat <strong>and</strong> teff,<br />

respectively. A yield reduction vary<strong>in</strong>g between 23 to 29% for wheat<br />

<strong>and</strong> 14 to 22% for teff was reported when estimat<strong>in</strong>g the water-limited<br />

production potential. The <strong>l<strong>and</strong></strong> production potential ranged from 0.84<br />

to 3.57 t/ha for wheat <strong>and</strong> 0.53 to 4.58 t/ha for teff. Both the spatial<br />

<strong>and</strong> temporal yield variability were high. The model was validated<br />

us<strong>in</strong>g the actual yields <strong>and</strong> showed good performance (r 2 =0.74 for<br />

wheat <strong>and</strong> 0.78 for teff). A yield gap analysis was performed to<br />

identify the ma<strong>in</strong> production limit<strong>in</strong>g factors (moisture availability,<br />

slope, dra<strong>in</strong>age <strong>and</strong> organic carbon). Possible <strong>l<strong>and</strong></strong> use management<br />

practices were identified to m<strong>in</strong>imize the yield gaps.<br />

Option :<br />

Use of Physical L<strong>and</strong> Resources<br />

Mr. El Desouky Hamdy<br />

ECONOMIC MINERALIZATIONS IN THE AREA<br />

OF ABU KHARIF MOUNTAIN, NORTHERN<br />

EASTERN DESERT, EGYPT. A COMBINED<br />

REMOTE SENSING AND GEOCHEMISTRY<br />

STUDY AFTER FIELD WORK<br />

Promoter (s) : E. Keppens, O. Batelaan<br />

Contact address : Brusselsestraat 165/J118, 3000<br />

Leuven, Belgium<br />

Abstract :<br />

The thesis offers a unique comb<strong>in</strong>ation between Remote Sens<strong>in</strong>g,<br />

Geochemistry <strong>and</strong> Fieldwork for geological mapp<strong>in</strong>g <strong>and</strong> m<strong>in</strong>eral<br />

resource exploration. This unique comb<strong>in</strong>ation has been used to<br />

explore <strong>and</strong> map the area of Abu Kharif Mounta<strong>in</strong> with focus<strong>in</strong>g on its<br />

economic m<strong>in</strong>eralizations. Further more the thesis offers a unique<br />

comparison between some different remote sens<strong>in</strong>g techniques applied<br />

on different remote sens<strong>in</strong>g data sets with different spatial <strong>and</strong> spectral<br />

resolutions, first to test the validity of these data sets <strong>and</strong> these<br />

techniques for geological mapp<strong>in</strong>g <strong>and</strong> ore deposit exploration, then to<br />

select the best results for the study area. The research resulted <strong>in</strong> a set<br />

of new maps, which were presented for the first time <strong>in</strong> this thesis,<br />

these <strong>in</strong>clud<strong>in</strong>g: one geologic map, one l<strong>in</strong>eament map, three<br />

l<strong>in</strong>eament density maps <strong>and</strong> one ore deposit map, this <strong>in</strong> addition to a<br />

set of rose diagrams, one cross section <strong>and</strong> one sketch <strong>in</strong> the ore<br />

deposit map.<br />

Mr. Michael Ndemo Bogonko<br />

HYPERSPECTRAL REMOTE SENSING OF SOIL<br />

MOISTURE GRADIENTS IN THE<br />

MILLINGERWAARD, THE NETHERLANDS<br />

Promoter(s) : O. Batelaan, J. Bogaert<br />

Contact address : Rubensstraat 52, 1030 Brussel,<br />

Belgium<br />

Abstract :<br />

Hyperspectral remote sens<strong>in</strong>g by HyMap imag<strong>in</strong>g might provide a<br />

methodology to map surface moisture conditions over space <strong>and</strong> time.<br />

The purpose of this thesis is to <strong>in</strong>vestigate the potential of the HyMap<br />

data for soil moisture mapp<strong>in</strong>g. This is performed by compar<strong>in</strong>g the <strong>in</strong><br />

situ soil moisture data from Mill<strong>in</strong>gerwaard study area (Nether<strong>l<strong>and</strong></strong>s)<br />

with the hyperspectral high-resolution data acquired by the HyMap<br />

sensor.<br />

As part of part of the „HyEco‟04 project‟, the Department of<br />

Hydrology <strong>and</strong> Hydraulic Eng<strong>in</strong>eer<strong>in</strong>g executed on July 28 th 2004 a<br />

field campaign <strong>in</strong> which eighty eight ground truth soil moisture<br />

measurements us<strong>in</strong>g a Theta Probe Type ML2 were taken. On the<br />

same day also the HyMap 5 m resolution imagery were taken. Soil<br />

moisture po<strong>in</strong>t measurements were spatially <strong>in</strong>terpolated us<strong>in</strong>g a spl<strong>in</strong>e<br />

<strong>in</strong>terpolation technique. Statistical analyses, <strong>in</strong>clud<strong>in</strong>g simple l<strong>in</strong>ear<br />

correlation, pr<strong>in</strong>cipal component analysis (PCA) <strong>and</strong> cluster analysis<br />

were used to compare the generated soil moisture map with the<br />

imagery. Obta<strong>in</strong>ed correlations showed a weak relationship between<br />

the observed soil moisture <strong>and</strong> the hyperspectral data. Correlations<br />

between 0.2 <strong>and</strong> 0.4 could not s<strong>in</strong>gle out an effective HyMap b<strong>and</strong><br />

suitable for soil moisture mapp<strong>in</strong>g. Three pr<strong>in</strong>ciple components that<br />

expla<strong>in</strong>ed more than 99% of the <strong>in</strong>formation equally <strong>in</strong>dicated a weak<br />

correlation of less than 0.2 with field soil moisture data. Indices like<br />

NDVI, SAVI or NDWI, did not give a better correlation than the<br />

<strong>in</strong>dividual b<strong>and</strong>s. The NDVI <strong>in</strong>dex could only expla<strong>in</strong> 32% of the total<br />

variance. The patterns of soil moisture could be <strong>in</strong>ferred as a function<br />

of topography which <strong>in</strong>dicated a higher correlation with an R 2 of 0.76.<br />

Spatial patterns of the moisture could not be expla<strong>in</strong>ed by cluster<br />

analysis as no clear clusters were def<strong>in</strong>ed.<br />

HyMap data could not be effectively used <strong>in</strong> mapp<strong>in</strong>g of soil moisture<br />

<strong>in</strong> the study area. Better methods for def<strong>in</strong><strong>in</strong>g spatial variability of soil<br />

moisture can be used <strong>and</strong> the temporal aspect for this k<strong>in</strong>d of study<br />

can constitute effective means of monitor<strong>in</strong>g <strong>and</strong> mapp<strong>in</strong>g of soil<br />

moisture.<br />

Mr. Prigiarto Hokkal Yonatan<br />

DRAINED AND UNDRAINED SLOPE<br />

STABILITY ANALYSIS USING GIS ON A<br />

REGIONAL SCALE<br />

Promoter(s) : F. De Smedt, O. Batelaan<br />

Contact address : Jl. Karet GG; TIONG Ujung N° 5,<br />

12940 Jakarta, Indonesia<br />

Abstract :<br />

This study is the cont<strong>in</strong>uation of the previous study done by Ram<br />

Lakhan Ray, 2004, that applied stability model on an area of 341 km 2<br />

of Dhad<strong>in</strong>g district, Nepal. In this study, a spatial distributed<br />

<strong>physical</strong>ly based slope stability model was presented <strong>and</strong> applied on<br />

84 km 2 of cohesive soil, covered about 25% of the orig<strong>in</strong>al study area.<br />

Two methods of analysis were performed, i.e. total <strong>and</strong> effective stress<br />

analyses <strong>and</strong> Taylor <strong>and</strong> <strong>in</strong>f<strong>in</strong>ite slope methods were applied on the<br />

analysis. Critical height <strong>and</strong> safety factor maps were produced based<br />

on those analyses. Steady state <strong>and</strong> quasi dynamic conditions were<br />

considered for the present study with vary<strong>in</strong>g soil thickness. For quasi<br />

dynamic conditions, wetness <strong>in</strong>dex was applied based on direct<br />

ra<strong>in</strong>fall <strong>in</strong>filtrations. Slope angle of 38 <strong>and</strong> 17 can be considered as<br />

the average mean slope angle to cause <strong>in</strong>stability <strong>and</strong> the lower most<br />

slope angle for stable conditions, respectively. This value was derived<br />

from the analysis based on half saturated conditions. It was also<br />

concluded that this case can serve as general conditions of safety<br />

factor map at the site where this case also has a similar result with<br />

models based on different return periods. Taylor method was not<br />

applicable for this study area s<strong>in</strong>ce this method is only applicable for<br />

assess<strong>in</strong>g safety factor with high slope angle. For short term safety<br />

- 9 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

factor map, completely dry conditions resulted from <strong>in</strong>f<strong>in</strong>ite slope<br />

method can be used as a short term applications. Half saturated case<br />

can be considered as general <strong>and</strong> long term safety factor map as this<br />

condition reveals similar result as given by various return periods.<br />

This study has proved that models developed with <strong>in</strong>f<strong>in</strong>ite slope<br />

models have given the best result even with some assumption.<br />

Ms. Udas Anju<br />

SLOPE STABILITY ANALYSIS USING GIS ON A<br />

REGIONAL SCALE: A CASE STUDY OF<br />

NARAYANGHAT - MUNGLING HIGHWAY<br />

SECTION, NEPAL<br />

Promoter(s) : F. De Smedt<br />

Contact address : Dharan-3, 12940 Sunsari, Nepal<br />

Abstract :<br />

In this study, the stability of the slope has been analyzed with the help<br />

of Arcview GIS 3.2. The study area is located <strong>in</strong> the western part of<br />

Nepal <strong>in</strong> Chitwan district <strong>and</strong> the total area is near about 287.62 km 2.<br />

Dur<strong>in</strong>g this study the maps for the stability of the slope for seven areas<br />

have been produced, <strong>in</strong>clud<strong>in</strong>g three steady state conditions assum<strong>in</strong>g<br />

either completely dry rocks, half saturated rocks, or fully saturated<br />

rocks <strong>and</strong> four quasi dynamic conditions, i.e. soil wetness result<strong>in</strong>g<br />

from storm events with respectively 2, 10, 25 <strong>and</strong> 50 years return<br />

periods. The methodology is applied only for rock slope <strong>and</strong> analysis<br />

<strong>and</strong> is conducted to evaluate the safety factor of various steady state<br />

conditions <strong>and</strong> different return periods. Most of the areas are prone to<br />

slope failure <strong>in</strong> function of topography. It has been found from the<br />

study that only 24.58% of the rocks are unconditionally stable<br />

(characterized by slopes smaller than 30°) while 45 % of the soils are<br />

found to be unstable under fully dry conditions. Only 1.28% of the<br />

rocks are unconditionally stable (characterized by slopes smaller than<br />

10°) while 91.76 % of the soils are found to be unstable under fully<br />

saturated conditions. Thus, it can be concluded that the study area is<br />

prone for rock slide <strong>and</strong> susceptible to slope failure. As the analysis<br />

derived from the present study reveals that the areas are <strong>in</strong> critical state<br />

of slope failure, the detailed study for the slope stability should be<br />

taken to avoid severe damages <strong>in</strong> near future.<br />

Option :<br />

Management of Physical L<strong>and</strong> Resources<br />

Mr. Addisu Delelle Molla<br />

THE ROLE OF INTEGRATED ORGANIC AND<br />

MINERAL FERTILIZER APPLICATION ON SOIL<br />

FERTILITY PARAMETERS AND YIELD OF<br />

WHEAT UNDER THE DRYLAND CONDITIONS<br />

OF NORTHERN ETHIOPIA<br />

Promoter(s) : H. Verplancke<br />

Contact address : Sir<strong>in</strong>ka Agric. Research Centre, 74<br />

Weldia, N. Welo, Ethiopia<br />

Abstract :<br />

A field experiment was conducted to assess the role of <strong>in</strong>tegrated use<br />

of farm yard manure (FYM) <strong>and</strong> m<strong>in</strong>eral fertilizers on soil fertility<br />

parameters <strong>and</strong> gra<strong>in</strong> yield <strong>and</strong> yield components of wheat <strong>in</strong> the<br />

high<strong>l<strong>and</strong></strong>s of northeastern Ethiopia. The soil chemical properties were<br />

affected by both application of FYM alone <strong>and</strong> <strong>in</strong>tegrated with m<strong>in</strong>eral<br />

fertilizers. Increases <strong>in</strong> soil fertility parameters were observed with<br />

<strong>in</strong>creased levels of FYM application. The <strong>in</strong>tegrated application of<br />

FYM with m<strong>in</strong>eral fertilizers significantly <strong>in</strong>creased wheat yield <strong>and</strong><br />

yield components. The addition of 5 <strong>and</strong> 10 ton ha -1 FYM gave yield<br />

advantages of 15.7 <strong>and</strong> 16.4% over the non-manured plots,<br />

respectively. The highest gra<strong>in</strong> yield of wheat (2253.4 kg ha -1 ) was<br />

obta<strong>in</strong>ed by apply<strong>in</strong>g 5 ton ha -1 FYM comb<strong>in</strong>ed with 0/10 Kg ha -1<br />

N/P. As a conclusion, the application of FYM at 5 <strong>and</strong> 10 ton ha -1<br />

with 50% the locally recommended m<strong>in</strong>eral fertilizer rates had a<br />

positive effect on soil fertility parameters <strong>and</strong> wheat yield <strong>and</strong> yield<br />

components.<br />

Mr. Bekiebang Nuikwangho Peter<br />

APPLICATION OF QUALITATIVE AND<br />

QUANTITATIVE LAND EVALUATION TOOLS<br />

TO ASSESS THE AGRICULTURAL<br />

PRODUCTION POTENTIAL OF NORTH-WEST<br />

CAMEROON<br />

Promoter(s) : E. Van Ranst, H. Verplancke<br />

Contact address : P.O. Box 30, NDOP, Ngoketunjia<br />

div. N.W.P., Cameroon<br />

Abstract :<br />

Qualitative <strong>and</strong> quantitative <strong>l<strong>and</strong></strong> evaluation tools were applied to<br />

asses the agricultural potential of North-West Cameroon for the<br />

production of groundnut. Us<strong>in</strong>g GIS tools, a digital spatial <strong>and</strong><br />

numerical database of the natural <strong>resources</strong> was generated. The <strong>l<strong>and</strong></strong><br />

suitability classification revealed that a greater part of the study area<br />

was moderately suitable with respect to climate but marg<strong>in</strong>ally suitable<br />

with respect to edaphic properties. With regard to the crop growth<br />

model, the estimated yield ranged from 0.34 to 1.99 t/ha. The<br />

production of groundnut is strongly be<strong>in</strong>g hampered by high soil<br />

acidity <strong>and</strong> low sum of basic cations. The results of both <strong>l<strong>and</strong></strong><br />

evaluation tools were validated us<strong>in</strong>g locally recorded <strong>and</strong><br />

<strong>in</strong>ternationally reported yield data<br />

Ms. Berko Cynthia<br />

MANIPULATION OF NITROGEN RELEASE<br />

FROM 15N LABELLED CROP RESIDUES<br />

THROUGH APPLICATION OF ON-AND OFF-<br />

FARM ORGANIC WASTE PRODUCTS<br />

Promoter(s) : P. Boeckx, B. Chaves Daguilar<br />

Contact address : c/o Mr. William Berko, IRS<br />

(accounts), P.O. Box 2202, Accra, Ghana<br />

Abstract :<br />

This <strong>in</strong>cubation experiment imitated two w<strong>in</strong>ter – spr<strong>in</strong>g seasons (380<br />

days) to asses the effectiveness of straw to immobilize N released from<br />

N- rich celery residues dur<strong>in</strong>g the w<strong>in</strong>ter period <strong>and</strong> v<strong>in</strong>asses to<br />

stimulate rem<strong>in</strong>eralisation of previous immobilized N <strong>in</strong> spr<strong>in</strong>g, when<br />

crops need N for growth. We employed 15 N techniques to better<br />

underst<strong>and</strong> the N processes <strong>in</strong>volved <strong>and</strong> to quantify N content <strong>in</strong> the<br />

various N pools.<br />

N m<strong>in</strong>eralization from celery was highest (57.4 mg N kg -1 ) at the end<br />

of the first w<strong>in</strong>ter- spr<strong>in</strong>g phase. The straw + celery treatment showed<br />

a net N immobilization effect of –56.1 mg N kg -1 . Still a net<br />

immobilization effect of –7.5 mg kg -1 was observed after the addition<br />

of v<strong>in</strong>asse <strong>in</strong> spr<strong>in</strong>g. The same pattern was noticed dur<strong>in</strong>g the second<br />

w<strong>in</strong>ter – spr<strong>in</strong>g season (198-380 days) <strong>in</strong> which the above<br />

experimental set-up was ma<strong>in</strong>ta<strong>in</strong>ed but unlabelled celery was used.<br />

Reduced levels of m<strong>in</strong>eral N were associated with higher levels of<br />

microbial biomass N (MB-N).<br />

Mr. Chapaga<strong>in</strong> Kumar Saroj<br />

RELEASE OF ARSENIC FROM INTERTIDAL<br />

SEDIMENTS OF THE RIVER SCHELDT :<br />

INFLUENCE OF MOISTURE REGIME<br />

Promoter(s) : M. Verloo, G. Du La<strong>in</strong>g<br />

Contact address : c/o Giridhar Upadhayaya, General<br />

Post Box n° 8345, Kathm<strong>and</strong>u, Nepal<br />

Abstract :<br />

This study aimed to assess the occurrence of arsenic <strong>in</strong> the <strong>in</strong>tertidal<br />

sediments of River Scheldt <strong>and</strong> the relationship between arsenic<br />

release <strong>and</strong> the level of the ground water table. On an average, the<br />

arsenic concentrations <strong>in</strong> the sediments were below the background<br />

<strong>and</strong> the remediation levels of arsenic <strong>in</strong> F<strong>l<strong>and</strong></strong>ers. Strong positive<br />

correlation existed between arsenic <strong>and</strong> organic matter, <strong>and</strong> between<br />

arsenic <strong>and</strong> clay content. In contrary, negative correlation existed<br />

between arsenic <strong>and</strong> s<strong>and</strong> content, <strong>and</strong> between arsenic <strong>and</strong> pH.<br />

The results of arsenic release under different ground water conditions<br />

<strong>in</strong> the greenhouse revealed that arsenic release depended upon the<br />

redox conditions. The release of arsenic was quite low <strong>and</strong> stable <strong>in</strong><br />

the oxic zones where as, arsenic release was much higher at depths<br />

below the groundwater table with a significant temporal variation.<br />

- 10 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

Mr. Kam<strong>and</strong>e Peter Njoroge<br />

METAL CONTAMINATION IN IRRIGATED<br />

AGRICULTURAL LAND : CASE STUDY OF<br />

NAIROBI RIVER BASIN, KENYA<br />

Promoter(s) : F. Tack<br />

Contact address : University of Nairobi, P.O. Box<br />

29053 Nairobi, c/o Dr. Njoka, Nairobi, Kenya<br />

Abstract :<br />

This study was conducted to assess the impact of us<strong>in</strong>g polluted river<br />

water on the farm<strong>l<strong>and</strong></strong>s along the Ngong river <strong>in</strong> Nairobi. Soil samples<br />

were taken at depths of 0-20 cm, 20-40 cm <strong>and</strong> 40-60 cm. The total<br />

metal concentrations of Cd, Cr, Cu, Ni, Pb <strong>and</strong> Zn were determ<strong>in</strong>ed<br />

with aqua regia extraction. S<strong>in</strong>gle extractions were used to establish<br />

the environmental risk <strong>and</strong> metal bioavailability : a 0.5 M HCl<br />

extraction assessed the labile phase while 0.05 M EDTA <strong>and</strong> 0.11 M<br />

acetic acid extractions assessed the fraction correlat<strong>in</strong>g with plant<br />

contents; a 0.01 M CaCl 2 extraction assess the exchangeable fraction.<br />

The metal contents were analysed by ICP-OES. Except for Ni, there<br />

was significant anthropogenic <strong>in</strong>fluence <strong>and</strong> a possible environmental<br />

risk. This calls for a reversal of the trend <strong>and</strong> further study about the<br />

effects on plant nutrition <strong>and</strong> the food cha<strong>in</strong>, to prevent direct hazard<br />

to man.<br />

Mr. Olana Daniel Emiru<br />

NITROGEN DYNAMICS UNDER<br />

CONVENTIONAL AND REDUCED TILLAGE<br />

FIELDS<br />

Promoter(s) : S. De Neve, K. D'Haene<br />

Contact address : P.O. Box 24139, Addis Ababa,<br />

Ethiopia<br />

Abstract :<br />

To avert the negative impacts of conventional tillage (CVT) the<br />

adoption of conservation tillage (CST) has ga<strong>in</strong>ed a wide recognition.<br />

The study was conducted on samples from 18 fields that had been<br />

under CVT <strong>and</strong> CST. Soil nitrogen m<strong>in</strong>eralization, microbial biomass<br />

nitrogen (MBN) <strong>and</strong> total nitrogen was studied <strong>in</strong> this experiment.<br />

Results showed contrast<strong>in</strong>g nitrogen m<strong>in</strong>eralization rates <strong>in</strong> both CST<br />

<strong>and</strong> CVT fields. Most of CST fields had slightly higher m<strong>in</strong>eralization<br />

rate. Although few CST fields with long duration had higher<br />

m<strong>in</strong>eralization rates, the length of CST didn‟t necessarily reflect the<br />

m<strong>in</strong>eralization rate. The field with 10 year CST was found to have the<br />

highest m<strong>in</strong>eralization rate. The highest microbial biomass nitrogen<br />

(MBN) was found <strong>in</strong> fields with the longest (18 years) CST at the 10 th<br />

week of <strong>in</strong>cubation. The MBN decreased with <strong>in</strong>cubation time. Total<br />

nitrogen <strong>in</strong> the soil profile decreased sharply <strong>in</strong> CST. Overall, adopt<strong>in</strong>g<br />

CST seemed to have improved N m<strong>in</strong>eralization, total soil nitrogen<br />

<strong>and</strong> MBN as compared to CVT, but the variability of the results was<br />

large due to the specific experimental set-up adopted. Further research<br />

would be needed to better quantify the effect of tillage <strong>and</strong> soil<br />

disturbance on N m<strong>in</strong>eralization.<br />

Mr. Pervej Hasan Ahmed<br />

DENITRIFICATION ACTIVITY IN<br />

CONVENTIONAL AND REDUCED TILLED<br />

CROPLANDS<br />

Promoter(s) : P. Boeckx, D. Beheydt<br />

Contact address : Baitul Aman Jane Mosque Road,<br />

7433 Baganchara, Sharsha, Jessore, Bangladesh<br />

Abstract :<br />

A study was conducted dur<strong>in</strong>g 2004 to <strong>in</strong>vestigate the N 2O <strong>and</strong> total<br />

denitrification losses, us<strong>in</strong>g the acetylene <strong>in</strong>hibition method, from 2<br />

no-tilled (cropped with maize <strong>and</strong> summer oat) <strong>and</strong> 1 conventionally<br />

tilled field (cropped with maize) at Maulde, Henegouwen, Belgium.<br />

The N 2O production from the no-tilled soils was higher than from the<br />

conventional tilled soil although the no-tilled fields received less<br />

N-fertilization. N 2 losses from all three fields were low or absent<br />

which was also confirmed by the WFPS barely reach<strong>in</strong>g 60%. Based<br />

on field N 2O measurements <strong>and</strong> laboratory measurements of N 2O <strong>and</strong><br />

N 2O+N 2 the N 2O/(N 2O+N 2) ratio of the fields were calculated. The<br />

highest <strong>and</strong> lowest overall calculated ratio were recorded respectively<br />

from the no-tilled (1.02) <strong>and</strong> the conventional tilled (0.09) maize field.<br />

Mr. Senkondo Hassan Yas<strong>in</strong><br />

METAL CONTENTS IN REED (PHRAGMITES<br />

AUSTRALIS) AND WILLOW (SALIX SP.) IN<br />

FLOODPLAINS AS AFFECTED BY PHYSICO-<br />

CHEMICAL CONDITIONS<br />

Promoter(s) : F. Tack<br />

Contact address : P.O. Box 2409, Arusha, Tanzania<br />

Abstract :<br />

In Belgium, there has been a regular dredg<strong>in</strong>g of the Scheldt river. The<br />

disposed sediments are polluted by at least one of the metals, Cd, Cr,<br />

Zn or Pb. The pollution levels encountered is a subject of concern as<br />

most of the soils affected are currently <strong>in</strong> use for agriculture, nature<br />

development or forestry.<br />

Higher concentrations of Cu <strong>and</strong> Cd were found <strong>in</strong> roots than <strong>in</strong> shoots<br />

<strong>in</strong> both reed <strong>and</strong> willow plants. Cu was found to be more available <strong>in</strong><br />

alternat<strong>in</strong>g wett<strong>in</strong>g <strong>and</strong> dry<strong>in</strong>g conditions than <strong>in</strong> permanently flooded<br />

conditions. Plants that grew <strong>in</strong> soils where no organic matter was<br />

added had lower Cd <strong>and</strong> Cu concentrations than the plants that grew<br />

<strong>in</strong> soils where organic matter was added.<br />

Plants that grew <strong>in</strong> heavy textured soils had the lowest concentrations<br />

of Cd <strong>and</strong> Cu. The lower concentrations of Cd <strong>and</strong> Cu were observed<br />

<strong>in</strong> plants that grew under permanently flooded conditions than <strong>in</strong><br />

plants that grew under field capacity. In addition, plants grown <strong>in</strong><br />

oxidized soils had higher concentration of metals than the plants<br />

grown <strong>in</strong> reduced soils.<br />

There was no significant relationship between the concentration of Cu<br />

<strong>and</strong> Cd <strong>in</strong> the pore water <strong>and</strong> the concentration of Cu <strong>and</strong> Cd <strong>in</strong> reed<br />

<strong>and</strong> willow plants.<br />

Ms. Sultana Nasr<strong>in</strong><br />

USING ELECTROMAGNETIC INDUCTION<br />

MEASUREMENTS TO IDENTIFY SOIL<br />

SUITABILITY ZONES FOR TREE SPECIES<br />

Promoter(s) : M. Van Meirvenne<br />

Contact address : c/o Nasr<strong>in</strong> Sultana or Md. Monirul<br />

Islam, 88 St.Johns road, E174JQ Walthamstow, UK<br />

Abstract :<br />

This study focused on the electromagnetic <strong>in</strong>duction measurement to<br />

identify soil suitable zone for tree species for two fields: one is a<br />

pasture field <strong>and</strong> the other is a forest litter field <strong>in</strong> the West-F<strong>l<strong>and</strong></strong>ers,<br />

Belgium. EM38, sensor was used to measure the electrical<br />

conductivity (EC) of soil with<strong>in</strong> the field scale <strong>and</strong> those EC values<br />

were used to take site specific soil sampl<strong>in</strong>g for soil particle size<br />

analysis. A positive relationship was obta<strong>in</strong>ed between EC <strong>and</strong> clay<br />

content. Both fields were classified by us<strong>in</strong>g fuzzy k means analysis.<br />

Accord<strong>in</strong>g to EC, the pasture field was classified <strong>in</strong>to 2 zones <strong>and</strong> the<br />

litter field was classified <strong>in</strong>to 3 zones. Betula pendula Roth <strong>and</strong> P<strong>in</strong>us<br />

sylvestris L. were selected for zone 1 <strong>and</strong> zone 2 for the pasture field.<br />

Quercus robur L. tree species was selected for the litter field.<br />

Electromagnetic <strong>in</strong>duction measurement was functional to classify soil<br />

suitability zones <strong>and</strong> select<strong>in</strong>g tree species for specific sites.<br />

Mr. Tekele Alemu Legesse<br />

DETERMINANTS OF RURAL LIVELIHOOD<br />

DIVERSIFICATION : CASE STUDY OF<br />

CENTRAL RIFT VALLEY, ETHIOPIA<br />

Promoter(s) : L. D'Haese<br />

Contact address : P.O. Box 32888, Addis Ababa,<br />

Ethiopia<br />

Abstract :<br />

This study focuses on determ<strong>in</strong>ants of rural livelihood diversification<br />

<strong>in</strong> Central Rift Valley of Ethiopia. Four key questions have been<br />

addressed: i) what are exist<strong>in</strong>g categories of potential off-farm<br />

activities ; ii) How much is the contribution of farm <strong>and</strong> off-farm<br />

activities to the livelihood of rural households; iii) Are there barriers<br />

to rural off-farm employment opportunities; <strong>and</strong> iv) What are<br />

practical remedies to the barriers of rural livelihood diversification at<br />

the household level A survey of 60 households us<strong>in</strong>g a structured<br />

- 11 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

questionnaire complemented by focused group discussions were<br />

carried out by the author. Descriptive <strong>and</strong> quantitative analysis has<br />

been undertaken. From descriptive analysis, it has been found out that<br />

off-farm employment opportunities contribute 36.3%, 42.9 %, <strong>and</strong><br />

27.8% of total <strong>in</strong>come for rural household with high, medium <strong>and</strong> low<br />

<strong>in</strong>come level respectively. The logit regression results verified many of<br />

hypotheses set forth. In other words, off-farm employment is<br />

significantly <strong>in</strong>fluenced by literacy level of household head, number of<br />

active family members, number of livestock owned, household head<br />

age, perception of rural households towards farm<strong>in</strong>g, <strong>in</strong>frastructure<br />

development such as access to credit <strong>and</strong> access to nearby town <strong>and</strong><br />

cities. But it has been discovered that off-farm activities are not much<br />

shaped by gender, which contradicts the hypothesis set forth.<br />

Mr. V<strong>and</strong>i David Kallon<br />

EFFECTS OF MULCHING AND SEED BED TYPE<br />

ON SOIL WATER STORAGE AND WATER USE<br />

EFFICIENCY : CASE STUDY OF PEPPER,<br />

FREETOWN (SIERRA LEONE)<br />

Promoter(s) : H. Verplancke<br />

Contact address : Njala University College, New<br />

Eng<strong>l<strong>and</strong></strong>, Freetown, Sierra Leone<br />

Abstract :<br />

Degradation of soils <strong>in</strong> Sub-Saharan Africa has left vast agricultural<br />

<strong>l<strong>and</strong></strong> largely unproductive <strong>in</strong> relation to soil water supply <strong>and</strong> nutrient<br />

management. A field experiment was conducted (Sept. – Nov./2004)<br />

on a s<strong>and</strong>y clay soil <strong>in</strong> Freetown, Sierra Leone, to evaluate the<br />

contribution of grow<strong>in</strong>g-season grass mulch <strong>and</strong> seed bed type to soil<br />

water storage, water use <strong>and</strong> water use efficiency, <strong>and</strong> yield of sweet<br />

pepper (capsicum annum). Six treatments each were laid out <strong>in</strong> a<br />

complete r<strong>and</strong>omized block <strong>in</strong> three replicates of equal numbers of<br />

raised <strong>and</strong> flat beds. Grass mulch was applied after transplant<strong>in</strong>g at<br />

rates of 2 cm <strong>and</strong> 4 cm leav<strong>in</strong>g one plot vacant as control. Mulch rate<br />

had a positive effect on water storage <strong>in</strong> both systems although this<br />

effect was complemented by moisture storage from the preced<strong>in</strong>g peak<br />

ra<strong>in</strong>fall <strong>in</strong> August/04. Total Available Water (TAW) was 148.5 mm.<br />

Above average yield was observed with values averag<strong>in</strong>g between<br />

1600, 1187 <strong>and</strong> 827 kg/ha-cm for the raised bed plots <strong>and</strong> 1310, 953,<br />

<strong>and</strong> 632 kg/ha-cm for the flat bed plots <strong>in</strong> the 4-, 2-, <strong>and</strong> 0-cm mulch<br />

plots respectively. Water use was favourably affected by both mulch<br />

rate <strong>and</strong> bed height. The values averaged 24.3, 23.2, <strong>and</strong> 22.8 cm <strong>and</strong><br />

21.3, 20.8, <strong>and</strong> 20.3 cm water <strong>in</strong> the 4-, 2-, <strong>and</strong> 0-cm mulch plots<br />

respectively. The 2- <strong>and</strong> 4-cm mulch rates respectively, <strong>in</strong>creased<br />

water use efficiency 45% <strong>and</strong> 29% <strong>in</strong> the raised bed <strong>and</strong> 50% <strong>and</strong> 32%<br />

<strong>in</strong> the flat bed plots over the no-mulch treatments. Apparently, canopy<br />

shad<strong>in</strong>g largely substituted for the beneficial effect of mulch dur<strong>in</strong>g<br />

the grow<strong>in</strong>g season. Soil water depletion (p-fraction) at average<br />

maximum ET rate of 3.26 mm/day was <strong>in</strong> the range of 0.41 – 0.35,<br />

with the lowest occurr<strong>in</strong>g dur<strong>in</strong>g the mid season. The effect of high<br />

depletion by ET on critical growth stages was m<strong>in</strong>imized <strong>and</strong><br />

apparently yields were generally good. In conclusion therefore,<br />

surface grass mulch application seems to have an <strong>in</strong>creas<strong>in</strong>g effect on<br />

water storage, water use <strong>and</strong> water use efficiency, <strong>and</strong> the yield<br />

response of pepper grown especially on st<strong>and</strong>ard raised beds <strong>in</strong> the<br />

study area.<br />

Ph.D. PROGRAMME PHYSICAL LAND RESOURCES<br />

Ph.D. promoted 2004-2005<br />

Dr. Charles Magori<br />

Present function <strong>and</strong> address : Research<br />

Scientist, Kenya Mar<strong>in</strong>e <strong>and</strong> Fisheries<br />

Research Institute (KMFRI), Mombasa,<br />

Kenya.<br />

Title of Ph.D. thesis : Hydrodynamic Modell<strong>in</strong>g of a<br />

Mangrove-Fr<strong>in</strong>ged Estuary, Mtwapa Creek, Kenya<br />

Date of promotion : July 2, 2004<br />

Promoter(s) : Prof. Dr. F. De Smedt<br />

Curriculum vitae :<br />

Charles Magori was born <strong>in</strong> Kenya <strong>in</strong> 1969. He holds a<br />

BSc <strong>in</strong> Mathematics (1993) from Jomo Kenyatta<br />

University of Agriculture <strong>and</strong> Technology (JKUAT) <strong>in</strong><br />

Kenya. He obta<strong>in</strong>ed a Master of Science degree <strong>in</strong><br />

Physical Oceanography from University of Gothenburg,<br />

Sweden <strong>in</strong> 1997. He is a Research Scientist work<strong>in</strong>g for<br />

Kenya Mar<strong>in</strong>e <strong>and</strong> Fisheries Research Institute (KMFRI)<br />

<strong>in</strong> Mombasa, Kenya. His PhD was carried out under the<br />

auspices of KMFRI <strong>and</strong> the Department of Hydrology <strong>and</strong><br />

Hydraulic Eng<strong>in</strong>eer<strong>in</strong>g, Faculty of Applied Sciences, Vrije<br />

Universiteit Brussel, from January 2000 to June 2004.<br />

Abstract :<br />

Mtwapa creek is a tropical estuar<strong>in</strong>e system located along<br />

the Kenyan coast <strong>in</strong> the Western Indian Ocean region. The<br />

creek is surrounded by vast mangrove swamps, while its<br />

offshore area is shielded by extensive share parallel coral<br />

reefs. It receives runoff from a seasonal river. This<br />

research concerns the development <strong>and</strong> application of a<br />

numerical model to describe the hydrodynamic<br />

characteristics of the creek.<br />

- 12 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

The model is based on RMA2, a f<strong>in</strong>ite element<br />

hydrodynamic numerical model for two- dimensional<br />

(depth-averaged) simulations. It uses a fully implicit<br />

scheme for solv<strong>in</strong>g shallow- water equations. The model<br />

predicts water level variations <strong>and</strong> current velocities <strong>in</strong> the<br />

creek reasonably well. Us<strong>in</strong>g scenario model<strong>in</strong>g, the<br />

sensitivity of Mtwapa creek to anticipated sea-level rise<br />

(<strong>in</strong>duced by climate change) <strong>in</strong> the 21st century has been<br />

<strong>in</strong>vestigated. Furthermore, us<strong>in</strong>g the numerical model,<br />

estimates of Mtwapa creek's volume, surface area <strong>and</strong> tidal<br />

prism dur<strong>in</strong>g spr<strong>in</strong>g <strong>and</strong> neap tides are computed. It is<br />

concluded that the numerical model presented <strong>in</strong> this<br />

dissertation can be used as a research tool for further<br />

<strong>in</strong>vestigations of estuar<strong>in</strong>e hydrodynamic processes. This is<br />

important for ecological <strong>studies</strong> <strong>and</strong> for the short- <strong>and</strong><br />

long-term susta<strong>in</strong>ability of the system.<br />

Dr. Adnan M. Aish<br />

Present function <strong>and</strong> address : Assistant<br />

Professor at Geology/Water Resources<br />

Department, Al Azhar University-Gaza,<br />

Palest<strong>in</strong>e.<br />

Title of Ph.D. thesis : Hydrogeological Study <strong>and</strong><br />

Artifitial Recharge Model<strong>in</strong>g of the Gaza Coastal<br />

Aquifer us<strong>in</strong>g GIS <strong>and</strong> MODFLOW<br />

Date of promotion : November 25, 2004<br />

Promoter(s) : Prof. Dr. F. De Smedt<br />

Curriculum vitae :<br />

Adnan Aish was born <strong>in</strong> Gaza (Palest<strong>in</strong>e) <strong>in</strong> 1964. He<br />

holds a Master of Science degree <strong>in</strong> Water Resources<br />

Eng<strong>in</strong>eer<strong>in</strong>g (Hydrogeology) from the Vrije Universiteit<br />

Brussel (VUB), Belgium <strong>in</strong> 2000, <strong>and</strong> a Postgraduate<br />

diploma <strong>in</strong> Water Resources Survey from the International<br />

Institute for Geo-Information Science <strong>and</strong> Earth<br />

Observation (ITC), Nether<strong>l<strong>and</strong></strong>s <strong>in</strong> 1997. He has worked as<br />

a PhD student <strong>in</strong> the Department of Hydrology <strong>and</strong><br />

Hydraulic Eng<strong>in</strong>eer<strong>in</strong>g at the VUB from October 2000 to<br />

November 2004. Before he came to Belgium for further<br />

study, he had been work<strong>in</strong>g as a lecturer at Al-Azhar<br />

University, Gaza, Palest<strong>in</strong>e.<br />

Abstract :<br />

This research work <strong>in</strong>vestigates the first phase of a<br />

feasibility study on the impact of artificial recharge from a<br />

planned wastewater treatment plant on the groundwater<br />

quantity <strong>and</strong> quality of the coastal aquifer <strong>in</strong> the Gaza<br />

Strip, Palest<strong>in</strong>e. Dur<strong>in</strong>g September 2001 to August 2002,<br />

an extensive program of hydrogeological <strong>in</strong>vestigation <strong>and</strong><br />

laboratory analysis of soil samples were undertaken to<br />

achieve the most reliable characterization of the subsoil<br />

<strong>and</strong> eventually to assist <strong>in</strong> the design <strong>and</strong> implementation<br />

of a pilot artificial recharge system for treated wastewater<br />

to groundwater.<br />

The ma<strong>in</strong> concerns of the hydrogeological study are to<br />

determ<strong>in</strong>e the hydrological parameters, lithological<br />

description, <strong>and</strong> geological sett<strong>in</strong>g. The study area extends<br />

over 336,000 m2, of which 212,000 m2 is used for a<br />

treatment plant <strong>and</strong> artificial recharge bas<strong>in</strong>. Three sets of<br />

boreholes have been drilled. The first set consists of 19<br />

shallow boreholes that penetrate the silty clay layer <strong>and</strong> the<br />

underly<strong>in</strong>g s<strong>and</strong>stone (kurkar). The second set consists of<br />

five boreholes that penetrate the unsaturated zone to at<br />

least 5 m below the groundwater level. The last set consists<br />

of three deep boreholes <strong>and</strong> one pump<strong>in</strong>g well. The deep<br />

boreholes were drilled at 100 m to 120 m depth go<strong>in</strong>g<br />

through the kurkar <strong>and</strong> clay formations. The pump<strong>in</strong>g well<br />

was drilled at 156 m reach<strong>in</strong>g the Saqiye formation. Packer<br />

tests were carried out to determ<strong>in</strong>e the hydraulic<br />

conductivity of the unsaturated zone. Also, 5 <strong>in</strong>filtration<br />

tests were conducted to assess the <strong>in</strong>filtration capacity at<br />

the location of the proposed artificial recharge. In addition,<br />

a pump<strong>in</strong>g test was also carried out to determ<strong>in</strong>e the<br />

hydraulic properties of the aquifer.<br />

In the local model of the artificial recharge simulation, an<br />

analytical <strong>and</strong> numerical solution of the transient<br />

groundwater flow is used to predict the time-dependency<br />

of the groundwater response <strong>in</strong> case of the planned<br />

artificial <strong>in</strong>filtration pond of the wastewater treatment<br />

plant. The maximum rise of the groundwater mound after<br />

100 days would be 14 m <strong>in</strong> the center of the <strong>in</strong>filtration<br />

pond <strong>and</strong> about 12 m at the edges.<br />

Regional groundwater flow simulations are made us<strong>in</strong>g the<br />

three-dimensional numerical model MODFLOW. The<br />

groundwater mound<strong>in</strong>g has been simulated with a constant<br />

recharge of 60000 m3/d, <strong>and</strong> an <strong>in</strong>filtration rate of 0.75<br />

m/d, while all other hydrogeological conditions are<br />

assumed as present conditions. The simulation shows that<br />

the groundwater mound beneath the center of the recharge<br />

bas<strong>in</strong> can be expected to rise to about 15 m above the<br />

present water table, <strong>and</strong> after about 2 years will be a slight<br />

<strong>in</strong>crement <strong>in</strong> the groundwater mound. The native<br />

groundwater downstream of the recharge area will<br />

gradually be <strong>in</strong>fluenced by the water orig<strong>in</strong>at<strong>in</strong>g from the<br />

<strong>in</strong>filtrated water <strong>and</strong> the cone of depression will dim<strong>in</strong>ish<br />

substantially due to the <strong>in</strong>filtration.<br />

In the solute transport model MT3D we assumed the<br />

<strong>in</strong>filtration water is at hypothetic conservative<br />

concentration of 100 mg/l that no absorption or adsorption<br />

solute is present, <strong>and</strong> that the <strong>in</strong>itial concentration <strong>in</strong> the<br />

aquifer is 0 mg/l. In the analysis of the results, the 100 mg/l<br />

of solute will be considered as the reference concentration<br />

(100% <strong>in</strong>jected water) <strong>and</strong> the simulated concentration <strong>in</strong><br />

the aquifer will be expressed relative to this value. The<br />

results <strong>in</strong>dicate that 90% of the <strong>in</strong>filtrated water will be<br />

mixed with the aquifer water after 1 year beneath the<br />

recharge area with decreas<strong>in</strong>g percentages <strong>in</strong> the<br />

surround<strong>in</strong>g area.<br />

- 13 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

Dr. Yongbo Liu<br />

Present function <strong>and</strong> address :<br />

Post-Doctoral Associate, Department of<br />

Geography, University of Guelph, Guelph,<br />

Ontario, Canada N1G 2W1<br />

Title of Ph.D. thesis : Development <strong>and</strong> application of a<br />

GIS-based hydrological model for flood prediction <strong>and</strong><br />

watershed management<br />

Date of promotion : December 23, 2004<br />

Promoter(s) : Prof. Dr. F. De Smedt<br />

Curriculum vitae :<br />

Yongbo Liu was born on November 15, 1965 <strong>in</strong> Jil<strong>in</strong>,<br />

Ch<strong>in</strong>a. He got his Bachelor of Science degree <strong>in</strong> Civil<br />

Eng<strong>in</strong>eer<strong>in</strong>g from Chengdu University of Science <strong>and</strong><br />

Technology (Sichuan University), Ch<strong>in</strong>a, <strong>in</strong> 1987. In<br />

August 1987, he started work<strong>in</strong>g as an eng<strong>in</strong>eer <strong>and</strong> a<br />

project manager <strong>in</strong> the Songhua <strong>and</strong> Liao River Water<br />

Resources Commission, M<strong>in</strong>istry of Water Resources,<br />

Ch<strong>in</strong>a. He got a Postgraduate diploma <strong>in</strong> Water Resources<br />

Eng<strong>in</strong>eer<strong>in</strong>g from Katholieke University Leuven (KUL),<br />

Belgium <strong>in</strong> 1998, <strong>and</strong> became a holder of Master of<br />

Science degree <strong>in</strong> Water Resources Eng<strong>in</strong>eer<strong>in</strong>g from Vrije<br />

University Brussel (VUB), Belgium <strong>in</strong> 1999 with a great<br />

dist<strong>in</strong>ction.<br />

From October 1999 onwards, he was <strong>in</strong>volved as a<br />

research assistant <strong>in</strong> the Department of Hydrology <strong>and</strong><br />

Hydraulic Eng<strong>in</strong>eer<strong>in</strong>g at the VUB work<strong>in</strong>g on the<br />

development of a distributed hydrological model of<br />

WetSpa (Water <strong>and</strong> Energy Transfer between Soil, Plant<br />

<strong>and</strong> Atmosphere). At the same time, he actively<br />

participated <strong>in</strong> several water <strong>resources</strong> eng<strong>in</strong>eer<strong>in</strong>g<br />

projects <strong>in</strong> Belgium, Luxemburg, Slovakia, Hungary,<br />

Romania, Po<strong>l<strong>and</strong></strong>, Vietnam, Sur<strong>in</strong>am, <strong>and</strong> Ch<strong>in</strong>a. His<br />

duties <strong>in</strong> these projects <strong>in</strong>clude flood prediction <strong>and</strong><br />

impact assessment of climate change, <strong>l<strong>and</strong></strong> use change <strong>and</strong><br />

river restoration on the hydrological processes us<strong>in</strong>g the<br />

WetSpa model.<br />

Yongbo Liu’s research results have been presented <strong>in</strong> the<br />

form of publications <strong>in</strong> <strong>in</strong>ternational journals <strong>in</strong>clud<strong>in</strong>g<br />

Journal of Hydrology, Hydrological Processes, Hydrology<br />

<strong>and</strong> Earth System Sciences, Water Resources<br />

Management, Environment Modell<strong>in</strong>g <strong>and</strong> Assessment,<br />

Environmental Geology, etc. He also attended several<br />

<strong>in</strong>ternational symposia <strong>and</strong> contributed to presentations,<br />

posters, proceed<strong>in</strong>gs <strong>and</strong> workshops. He presented his<br />

PhD thesis <strong>in</strong> December 2004 <strong>and</strong> was awarded with the<br />

grade of greatest dist<strong>in</strong>ction.<br />

cont<strong>in</strong>uous simulation model that may operate at a different<br />

time scale <strong>and</strong> at a different spatial resolution, which well<br />

represent the river bas<strong>in</strong> characteristics. The required<br />

<strong>in</strong>puts to the model <strong>in</strong>clude digital maps of elevation, soil<br />

type <strong>and</strong> <strong>l<strong>and</strong></strong> use, <strong>and</strong> time series of precipitation,<br />

temperature, potential evapotranspiration <strong>and</strong> flow<br />

discharge. The model enables one to simulate the complex<br />

hydrologic regimes of a river bas<strong>in</strong> with<strong>in</strong> a GIS<br />

framework, estimate runoff for each grid cell <strong>and</strong> route the<br />

flow along its flow path to the bas<strong>in</strong> outlet or any<br />

converg<strong>in</strong>g po<strong>in</strong>ts <strong>in</strong> the stream network, <strong>and</strong> eventually to<br />

simulate the spatial distribution of hydrological variables<br />

<strong>in</strong> a river bas<strong>in</strong>.<br />

The application of the WetSpa model was demonstrated <strong>in</strong><br />

three case <strong>studies</strong>, i.e. Barebeek (Belgium), Ste<strong>in</strong>sel<br />

(Luxembourg) <strong>and</strong> Margecany (Slovakia). The Barebeek<br />

catchment is a typical suburban watershed with dra<strong>in</strong>age<br />

area of 67.8 km2 situated northeast of Brussels, Belgium.<br />

The result<strong>in</strong>g calculated hydrographs with WetSpa model<br />

compare favourably with measurements at the gaug<strong>in</strong>g<br />

sites. The Ste<strong>in</strong>sel catchment is a highly urbanized<br />

watershed with a dra<strong>in</strong>age area of 407 km2 located <strong>in</strong> the<br />

upstream part of the Alzette River bas<strong>in</strong>, Gr<strong>and</strong> Duchy of<br />

Luxembourg. Results of WetSpa model simulation show<br />

that the model‟s level of representativeness to be quite<br />

satisfactory. Next, the runoff contribution from different<br />

<strong>l<strong>and</strong></strong> use areas <strong>and</strong> the impacts of <strong>l<strong>and</strong></strong> use change <strong>and</strong><br />

natural river restoration for the headwater areas on the<br />

flood behaviours are assessed us<strong>in</strong>g WetSpa model on an<br />

hourly time scale <strong>and</strong> 50×50 m resolution results. The<br />

Margecany catchment is a typical mounta<strong>in</strong>ous watershed<br />

with a dra<strong>in</strong>age area of 1133 km2 situated <strong>in</strong> the upstream<br />

part of the Hornad River bas<strong>in</strong>, Slovakia. Simulation<br />

results of WetSpa model show that the flow hydrographs of<br />

both snow melt<strong>in</strong>g floods <strong>and</strong> storm floods are well<br />

reproduced on a daily time scale <strong>and</strong> 100×100 m<br />

resolution.<br />

The WetSpa model makes full use of the remote sensed<br />

data <strong>and</strong> calculations are for the most part performed by<br />

GIS tools, such that the model is useful for flood prediction<br />

on complex terra<strong>in</strong> <strong>and</strong> analyz<strong>in</strong>g the effects of<br />

topography, soil type, <strong>and</strong> <strong>l<strong>and</strong></strong> use on the flood<br />

behaviours.<br />

Dr. Kurt Van Rompaey<br />

Present function <strong>and</strong> address : Consultant,<br />

Environmental Resources Management<br />

(ERM), Rouppeple<strong>in</strong> 16, Brussels<br />

Abstract :<br />

A GIS-based distributed hydrological model, WetSpa<br />

Extension, that operates on catchment scale is developed<br />

for flood prediction <strong>and</strong> watershed management. It is a<br />

Title of Ph.D. thesis : Study on the <strong>in</strong>teraction between<br />

atmospheric deposition, soil acidification <strong>and</strong> m<strong>in</strong>eral<br />

weather<strong>in</strong>g, us<strong>in</strong>g soil solution analyses, laboratory <strong>and</strong><br />

field experiments<br />

- 14 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

Date of promotion : January 7, 2005<br />

Promoter(s) : E. Van Ranst<br />

Curriculum vitae :<br />

Kurt Van Rompaey was born <strong>in</strong> Brasschaat on the 15 th of<br />

July 1975. He graduated as Agricultural Eng<strong>in</strong>eer <strong>in</strong><br />

Management of L<strong>and</strong> <strong>and</strong> Forest, option Soil <strong>and</strong> Water<br />

Management at the Ghent University <strong>in</strong> July 1998. His<br />

thesis focused on the determ<strong>in</strong>ation of background values<br />

of heavy metals <strong>in</strong> the prov<strong>in</strong>ce of Antwerp (F<strong>l<strong>and</strong></strong>ers,<br />

Belgium). From August 1998 till November 1998 he<br />

worked as a scientific collaborator at the Laboratory of<br />

Soil Science after which he became the assistant of Prof.<br />

Dr. E. Van Ranst. In this position he was responsible for<br />

the practical exercises of Soil M<strong>in</strong>eralogy, Clay<br />

M<strong>in</strong>eralogy, Tropical Soils, Environmental Soil<br />

Management. Dur<strong>in</strong>g his PhD research he worked on a<br />

large database obta<strong>in</strong>ed by a bi-weekly monitor<strong>in</strong>g (from<br />

the early 90’s till present) of ra<strong>in</strong>fall, throughfall <strong>and</strong> soil<br />

solutions at six monitor<strong>in</strong>g plots <strong>in</strong> F<strong>l<strong>and</strong></strong>ers <strong>and</strong><br />

performed field work <strong>in</strong> the Antwerp Camp<strong>in</strong>e (F<strong>l<strong>and</strong></strong>ers)<br />

to measure the <strong>in</strong> situ weather<strong>in</strong>g rates of m<strong>in</strong>erals <strong>in</strong><br />

soils. Several technical reports were written to distribute<br />

the results of the monitor<strong>in</strong>g campaign to different<br />

governmental agencies. The results of his PhD work were<br />

presented through oral <strong>and</strong> poster presentations on<br />

meet<strong>in</strong>gs of the Belgian Soil Science Society <strong>and</strong> on<br />

different <strong>in</strong>ternational conferences (USA, Po<strong>l<strong>and</strong></strong>,<br />

Thai<strong>l<strong>and</strong></strong>). He further worked on projects concern<strong>in</strong>g<br />

habitat characterization us<strong>in</strong>g soil profile research <strong>and</strong><br />

ground- <strong>and</strong> surface water analyses <strong>and</strong> the SPADE II<br />

(Soil Profile Attribute Data Environment) for Belgium <strong>and</strong><br />

Luxembourg, <strong>in</strong> cooporation with the National Soil<br />

Resources Institute of the Cranfield University, UK.<br />

Abstract :<br />

The first part of this work focused on the analyses of ra<strong>in</strong>-,<br />

throughfall <strong>and</strong> soil solutions <strong>in</strong> 6 forest ecosystems <strong>in</strong><br />

F<strong>l<strong>and</strong></strong>ers. Bi-weekly monitor<strong>in</strong>g dur<strong>in</strong>g more than a decade<br />

has shown that the pH values of the ra<strong>in</strong>- <strong>and</strong> throughfall<br />

lie <strong>in</strong> the range of what is <strong>in</strong>ternationally accepted as<br />

“natural values”. Any acid components <strong>in</strong> the atmosphere<br />

are thus fully neutralized before they reach the forest floor.<br />

Hence, it should be stressed that the NO 3 - <strong>and</strong> the SO 4<br />

2-<br />

compounds <strong>in</strong> the ra<strong>in</strong>fall can not cause acidify<strong>in</strong>g<br />

reactions. Only the NH 4 + can – by oxidation – cause a<br />

decrease <strong>in</strong> pH of the solutions. However, as all ra<strong>in</strong>- <strong>and</strong><br />

throughfall solutions also conta<strong>in</strong> HCO 3 - , the HNO 3 ,<br />

formed by the oxidation (nitrification) of NH 4 + will already<br />

be partly neutralised by this bicarbonate. The formula used<br />

to calculate the amount of acid deposition on a given site<br />

(conta<strong>in</strong><strong>in</strong>g nitrate, sulphate <strong>and</strong> ammonium as sources of<br />

acidity), presently used by policy makers is thus <strong>in</strong>correct<br />

<strong>and</strong> strongly overestimates the actual acid deposition.<br />

From the soil solution <strong>studies</strong> of 6 monitor<strong>in</strong>g plots, it was<br />

further concluded that the NO 3 - <strong>in</strong> the soil solutions largely<br />

comes from the breakdown of organic matter <strong>in</strong> the soil, as<br />

the N-<strong>in</strong>put from the atmosphere is <strong>in</strong>sufficient to expla<strong>in</strong><br />

the high concentrations of N <strong>in</strong> the soil water (> 60 mg.l -1<br />

NO 3 - ). Dur<strong>in</strong>g the breakdown of organic matter (oxidiz<strong>in</strong>g<br />

reaction), nitric acid is formed (H + + NO 3 - ). This strong<br />

m<strong>in</strong>eral acid must of course be neutralized immediately.<br />

Two reaction mechanisms were found that can play this<br />

role: (1) uptake by the vegetation of nitrate: when tak<strong>in</strong>g<br />

up this anion, the plant, <strong>in</strong> order to ma<strong>in</strong>ta<strong>in</strong> its electrical<br />

neutrality, reacts by secret<strong>in</strong>g a hydroxyl-group. This<br />

hydroxyl-group can then neutralize the acidity of the nitric<br />

acid. A second mechanism that was found (2) is the<br />

reaction of HNO 3 with silicate m<strong>in</strong>erals (the soils under<br />

study do not conta<strong>in</strong> any carbonates). Dur<strong>in</strong>g this reaction,<br />

the protons react with the silicate m<strong>in</strong>erals, as such<br />

liberat<strong>in</strong>g structural cations (e.g. Ca 2+ , Al 3+ ). When the<br />

turn-over of nutrients <strong>in</strong> the ecosystem is slow (low<br />

nutrient consumption), high concentrations of Al 3+ (from<br />

reaction with the m<strong>in</strong>erals) <strong>and</strong> NO 3 - (from the breakdown<br />

of the organic matter) are found. When the turn-over of<br />

nutrients occurs fast, hardly no alum<strong>in</strong>ium is leached from<br />

the soil as the acidity formed by the breakdown of the<br />

organic matter is fully neutralized by the uptake of<br />

nutrients from the soil solution. The leach<strong>in</strong>g of nitrate <strong>and</strong><br />

alum<strong>in</strong>ium from forest floors is thus directly related to the<br />

balance between breakdown of organic matter <strong>and</strong> uptake<br />

of nutrients by the vegetation. In some case however, this<br />

relationship can be strongly masked by external sources of<br />

nutrients (groundwater flow, fertilizer application, etc.).<br />

The <strong>in</strong>fluence of atmospheric deposition on the<br />

composition of the soil solutions thus seemed to be much<br />

smaller than the <strong>in</strong>fluence of other parameters: nutrient<br />

uptake, <strong>in</strong> situ breakdown of organic matter, <strong>in</strong>fluences<br />

from groundwater, etc.<br />

In the second part of the research, the weather<strong>in</strong>g of soil<br />

m<strong>in</strong>erals was studied us<strong>in</strong>g different approaches (batch-,<br />

column <strong>and</strong> field experiments). In general, the weather<strong>in</strong>g<br />

(breakdown) of silicate m<strong>in</strong>erals was found to be a very<br />

slow process.<br />

From the batch-experiments, it was found that the nature of<br />

the acid had little effect on the weather<strong>in</strong>g rate, but the<br />

effects of acid concentration, the temperature, the<br />

solid:liquid ratio <strong>and</strong> the particle size of the m<strong>in</strong>erals<br />

(glauconite, biotite, vermiculite, hectorite) were significant.<br />

Speed<strong>in</strong>g up the weather<strong>in</strong>g process <strong>in</strong> batch-experiments<br />

showed one major drawback, <strong>in</strong> that the extrapolation to<br />

the field conditions proved to be unjustified as batchexperiments<br />

are closed systems from which <strong>in</strong>termediary<br />

reaction products cannot be removed.<br />

To overcome this problem <strong>and</strong> to better imitate natural<br />

conditions, column experiments were set up <strong>in</strong> which<br />

vermiculite <strong>and</strong> glauconite were cont<strong>in</strong>uously leached with<br />

synthetically prepared ra<strong>in</strong>fall <strong>and</strong> soil solutions. A<br />

breakdown of the m<strong>in</strong>erals was not observed, but the fact<br />

that the pH of the effluent decreased after percolation<br />

through columns filled with glauconite, <strong>and</strong> strongly<br />

<strong>in</strong>creased after percolation through the vermiculite<br />

- 15 -


STUDENTS, RESEARCH FELLOWS & TRAINEES<br />

columns has opened new perspectives on research<br />

concern<strong>in</strong>g the acid neutraliz<strong>in</strong>g capacity of m<strong>in</strong>erals. It<br />

was found that it are ma<strong>in</strong>ly the exchangeable cations on<br />

the vermiculite that neutralize the acidity, as such<br />

suggest<strong>in</strong>g that a structural breakdown of silicate m<strong>in</strong>erals<br />

is a process which is too slow to have an acid neutraliz<strong>in</strong>g<br />

effect. To dissolve silicate m<strong>in</strong>erals <strong>in</strong> the soil, very strong<br />

acids (e.g. HNO 3 ) are thus needed <strong>in</strong> comb<strong>in</strong>ation with<br />

very small particle sizes.<br />

The fact that weather<strong>in</strong>g is a very slow process was also<br />

clear from the field experiments. Dur<strong>in</strong>g 4 years,<br />

glauconite <strong>and</strong> vermiculite were placed <strong>in</strong> different<br />

horizons of three different Podzol profiles accord<strong>in</strong>g to the<br />

test m<strong>in</strong>eral technique. After this period, the m<strong>in</strong>erals were<br />

characterized <strong>in</strong> detail us<strong>in</strong>g different chemical <strong>and</strong><br />

m<strong>in</strong>eralogical (XRD) techniques. After 4 years, no<br />

significant m<strong>in</strong>eralogical or chemical changes were found<br />

between the glauconite samples that were <strong>in</strong>cubated <strong>in</strong> the<br />

soil <strong>and</strong> the reference material stored <strong>in</strong> the lab.<br />

Vermiculite however did show some marked changes after<br />

4 years, among which the presence of non-exchangeable<br />

Al-polymers <strong>in</strong> the <strong>in</strong>terlayer <strong>and</strong> a strongly decreased<br />

cation exchange capacity (to about 10% of the orig<strong>in</strong>al<br />

CEC) were the most important ones. The formation of the<br />

Al-polymers is contradictory to the theory of acidocomplexolysis.<br />

Accord<strong>in</strong>g to this theory, the Al polymers<br />

<strong>in</strong> the <strong>in</strong>terlayer can not be formed <strong>in</strong> a Podzol as the Al 3+<br />

is too strongly bound to the organic molecules to form<br />

hydroxides <strong>in</strong> the <strong>in</strong>terlayer. Our results however, clearly<br />

show that, even <strong>in</strong> a Haplic Podzol, the formation of Alpolymers<br />

<strong>in</strong> the <strong>in</strong>terlayer is possible <strong>and</strong> occurs rather fast<br />

(< 2 years).<br />

In general, weather<strong>in</strong>g of the m<strong>in</strong>erals was not seen <strong>in</strong> the<br />

field experiments <strong>and</strong> for future <strong>studies</strong>, a longer<br />

<strong>in</strong>cubation period (10 – 15 years) <strong>and</strong> a smaller particle<br />

size (preferable < 2µm) are advised.<br />

SPECIAL TRAINING PROGRAMMES<br />

PHYSICAL LAND RESOURCES<br />

2005-2006<br />

Mr. Mbayo Ndekanya Doudou<br />

Université de Lubumbashi, R.D. Congo<br />

From : March 11, 2006 till September 10, 2006<br />

Subject : Valorisation des données disponibles des<br />

ressources naturelles physiques de la R.D. Congo<br />

pour une gestion rationnelle et durable des terres :<br />

SIG et Cartographie des Sols<br />

Promotor(s) : Prof. Dr. E. Van Ranst, Prof. Dr. G.<br />

Baert, Prof. Dr. M. Ngongo (UNILU)<br />

Physical<br />

L<strong>and</strong><br />

Resources<br />

New Ph.D. students 2005-2006<br />

Mr. Johan Van de Wauw (Belgium)<br />

Assistent<br />

Subject : Mapp<strong>in</strong>g of ground water dynamics<br />

Promotor(s) : Prof. Dr. P.A. F<strong>in</strong>ke<br />

Ms. Denef Karolien (Belgium)<br />

Scholarship : FWO (Research Foundation – F<strong>l<strong>and</strong></strong>ers)<br />

Subject : Characterization of the ecological <strong>and</strong> biogechemical<br />

functionality of microbial community structures via molecular &<br />

component-specific isotope analyses<br />

Promotor(s) : Prof. Dr. ir. P. Boeckx<br />

- 16 -


PUBLICATIONS<br />

ITC - ICE<br />

Papers<br />

ACCOE, F., BOECKX, P., VIDELA, X., PINO, I.,<br />

HOFMAN, G. & VAN CLEEMPUT, O. 2005. Estimation<br />

of potential gross nitrogen transformations <strong>and</strong> nitrogen<br />

retention <strong>in</strong> different grass<strong>l<strong>and</strong></strong> soils us<strong>in</strong>g FLUAZ. Soil<br />

Science Society of America Journal 69:1967-1976.<br />

BAHREMAND, A., CORLUY, J., LIU, Y.B., DE<br />

SMEDT, F., POOROVA, J. & VELCICKA, L., 2005.<br />

Stream flow simulation by WetSpa model <strong>in</strong> Hornad river<br />

bas<strong>in</strong>, Slovakia. Van Alphen, J., van Beek, E., & Taal, M.<br />

(eds.), Floods, from Defence to Management, Taylor &<br />

Francis Group, London: 67-74.<br />

BARRERA-BASSOLS, N., ZINCK, J.A., VAN RANST,<br />

E. 2006. Symbolism, knowledge <strong>and</strong> management of soil<br />

<strong>and</strong> <strong>l<strong>and</strong></strong> <strong>resources</strong> <strong>in</strong> <strong>in</strong>digenous communities :<br />

Ethnopedology at global, regional <strong>and</strong> local scales. Catena<br />

65:118-137.<br />

BATELAAN, O., HUNG, L.Q., TAM, V.T., VAN,<br />

N.T.H., NGUYET, V.T.M., LONG, N.T. & DE SMEDT,<br />

F., 2005. Geology <strong>and</strong> M<strong>in</strong>eral Resources, Volume 9, <strong>in</strong><br />

observance of the 40th anniversary of the Research<br />

Institute of Geology <strong>and</strong> M<strong>in</strong>eral Resources (1965-2005),<br />

Hanoi: 564-577.<br />

BEHEYDT, D., BOECKX, P., CLOUGH, T.J.,<br />

VERMEULEN, J., SHERLOCK, R.R. & VAN<br />

CLEEMPUT, O. 2005. Methods to adjust for<br />

the<strong>in</strong>terference of N 2 O on 13 C <strong>and</strong> 18 O measurements of<br />

CO 2 from soil m<strong>in</strong>eralization. Rapid communications <strong>in</strong><br />

Mass Spectrometry 19, 1365-1372.<br />

BOECKX, P., PAULINO, L., OYARZUN, C., VAN<br />

CLEEMPUT, O. & GODOY, R. 2005. Soil 15 N patterns<br />

<strong>in</strong> old-growth forests of southern Chile as <strong>in</strong>tegrator for N<br />

cycl<strong>in</strong>g. Isotopes <strong>in</strong> Environmental <strong>and</strong> Health Studies<br />

41:249-259.<br />

BOECKX, P., XU, X. & VAN CLEEMPUT, O. 2005.<br />

Mitigation of N 2 O <strong>and</strong> CH 4 emission from rice <strong>and</strong> wheat<br />

cropp<strong>in</strong>g systems us<strong>in</strong>g dicy<strong>and</strong>iamide <strong>and</strong> hydroqu<strong>in</strong>one.<br />

Nutrient Cycl<strong>in</strong>g <strong>in</strong> Agroecosystems 72:41-49.<br />

CHAVES, B., DE NEVE, S., LILLO CABRERA, M.C.,<br />

BOECKX, P., VAN CLEEMPUT, O. & HOFMAN, G.<br />

2005. The effect of mix<strong>in</strong>g organic biological waste<br />

materials <strong>and</strong> high-N crop residues on the short-time N 2 O<br />

emission from horticultural soil <strong>in</strong> model experiments.<br />

Biology <strong>and</strong> Fertility of Soils 41:411-418.<br />

CORLUY, J., VERBEIREN, B., BATELAAN, O. & DE<br />

SMEDT, F., 2004. Integrat<strong>in</strong>g vegetation mapp<strong>in</strong>g <strong>in</strong><br />

groundwater modell<strong>in</strong>g for ecohydrological predictions<br />

with<strong>in</strong> an ecosystem vision. In : Model application for<br />

wet<strong>l<strong>and</strong></strong>s hydrology <strong>and</strong> hydraulics, Eds. Kubrak, J.,<br />

Okruszko, T. & Ignar, S., Center of excellence <strong>in</strong> wet<strong>l<strong>and</strong></strong><br />

hydrology, WETHYDRO, Warsaw Agricultural University<br />

Press: 155-166.<br />

DE SMEDT, F., BREVIS VERGARA W. & DEBELS, P.<br />

2005. Analytical solution for solute transport result<strong>in</strong>g<br />

from <strong>in</strong>stantaneous <strong>in</strong>jection <strong>in</strong> streams with transient<br />

storage. Journal of Hydrology (<strong>in</strong> press), available on l<strong>in</strong>e:<br />

1-15.<br />

DUDAL, R., DECKERS, J., VAN ORSHOVEN, J. &<br />

VAN RANST, E. 2005. Soil survey <strong>in</strong> Belgium <strong>and</strong> its<br />

applications. In : Soil Resources of Europe, second<br />

edition. R.J.A. Jones, B. Houškové, P. Bullock <strong>and</strong> L.<br />

Montanarella (eds). European Soil Bureau Research<br />

Report N° 9, EUR 20559 EN, 420 pp. Office for Official<br />

Publications of the European Communities, Luxembourg :<br />

63-71.<br />

FINKE, P.A., BRUS, D.J., BIERKENS, M.F.P.,<br />

HOOGLAND, T., KNOTTERS, M. & DE VRIES, F.<br />

2004. Mapp<strong>in</strong>g ground water dynamics us<strong>in</strong>g multiple<br />

sources of exhaustive high resolution data. Geoderma 123:<br />

23-39..<br />

FINKE, P.A., BRUS, D.J., BIERKENS, M.F.P.,<br />

HOOGLAND, T., KNOTTERS, M. & DE VRIES, F.<br />

2005. Karter<strong>in</strong>g van de grondwaterdynamiek met behulp<br />

van geo-<strong>in</strong>formatie van hoge resolutie. Strom<strong>in</strong>gen 11/1:<br />

pp: 27-42.<br />

GEBREMESKEL, S., LIU, Y.B., DE SMEDT, F.,<br />

HOFFMANN, L. & PFISTER, L. 2005. Analys<strong>in</strong>g the<br />

effect of climate changes on streamflow us<strong>in</strong>g statistically<br />

downscaled GCM scenarios. Int. J. River Bas<strong>in</strong><br />

Management 2(4): 271-280.<br />

HUYGENS, D., BOECKX, P., GODOY, R., OYARZUN,<br />

C. & VAN CLEEMPUT, O. 2005. Aggregate <strong>and</strong> soil<br />

organic carbon dynamics <strong>in</strong> south Chilean Andisols.<br />

Biogeosciences 2:159-174.<br />

HUYGENS, D., BOECKX, P., VERMEULEN, J., DE<br />

PAEPE, X., PARK, A., BARKER, S., PULLAN, C. &<br />

VAN CLEEMPUT, O. 2005. Advances <strong>in</strong> coupl<strong>in</strong>g a<br />

commercial total organic carbon analyzer with an isotope<br />

ratio mass spectrometer to determ<strong>in</strong>e the isotopic signal of<br />

the total dissolved nitrogen pool. Rapid Communications<br />

<strong>in</strong> Mass Spectrometry 19:1-7.<br />

- 17 -


PUBLICATIONS<br />

KANYANKOGOTE, P., VAN RANST, E., VERDOODT,<br />

A. & BAERT, G. 2005. Effet de la lave trachybasaltique<br />

broyée sur les propriétés chimiques de sols de climat<br />

tropical humide. Etude et Gestion des Sols, 12(4):301-311.<br />

KRAVCHENKO, I.K., SEMENOV, V.M.,<br />

KUZNETSOVA, T.V., BYKOVA, S.A., DULOV, L.E.,<br />

PARDINI, D., GISPERT, M., BOECKX, P., VAN<br />

CLEEMPUT, O. & GALCHENKO, V.F. 2005.<br />

Physicochemical <strong>and</strong> Biological Factors Affect<strong>in</strong>g<br />

Atmospheric Methane Oxidation <strong>in</strong> Gray Forest Soils.<br />

Microbiology 74:216-220.<br />

LIU, Y. B., GEBREMESKEL, S., DE SMEDT, F.,<br />

HOFFMANN, L. & PFISTER, L. 2004. Simulation of<br />

flood reduction by natural river restoration us<strong>in</strong>g a<br />

distributed hydrological model. Hydrology <strong>and</strong> Earth<br />

System Sciences, 8(6): 1129-1140.<br />

LIU, Y.B., BATELAAN, O., DE SMEDT, F.,<br />

POOROVA, J. & VELCICKA, L., 2005. Automated<br />

calibration applied to a GIS-based flood simulation model<br />

us<strong>in</strong>g PEST. Van Alphen, J., van Beek, E., & Taal, M.<br />

(eds.), Floods, from Defence to Management, Taylor &<br />

Francis Group, London: 317-326.<br />

LIU, Y.B., YI, Y., BATELAAN, O. & DE SMEDT, F.,<br />

2005. Assess<strong>in</strong>g grid size effects on runoff <strong>and</strong> flow<br />

response us<strong>in</strong>g a GIS-based hydrologic model. In S.N. Li<br />

& V. Tao (eds.), Proceed<strong>in</strong>gs of the 13th International<br />

Conference on Geo<strong>in</strong>formatics, Toronto, Canada, Sept. 17-<br />

19, 2005, F050: 1-8.<br />

MAHINGA, J.C., VAN RANST, E. & BAERT, G. 2005.<br />

L<strong>and</strong> suitability assessment for sugarcane cultivation <strong>in</strong><br />

"Herois de Caxito" (Angola). Tropicultura 23(2) : 77-84.<br />

MANDIRINGANA, O.T., MNKENI, P.N.S., MKILE, Z.,<br />

VAN AVERBEKE, W., VAN RANST, E. &<br />

VERPLANCKE, H. 2005. M<strong>in</strong>eralogy <strong>and</strong> fertility status<br />

of selected soils of the Eastern Cape Prov<strong>in</strong>ce, South<br />

Africa. Comm. <strong>in</strong> Soil Science <strong>and</strong> Plant Analysis, 36 :<br />

2431-2446.<br />

MEES, F., STOOPS, G., VAN RANST, E., PAEPE, R. &<br />

VAN OVERLOOP, E. 2005. The nature of zeolite<br />

occurrences <strong>in</strong> deposits of the Olduvai Bas<strong>in</strong>, northern<br />

Tanzania. Clays <strong>and</strong> Clay M<strong>in</strong>erals, 53(6) : 659-673.<br />

RWETABULA, J. & DE SMEDT, F. 2005. L<strong>and</strong>use <strong>and</strong><br />

<strong>l<strong>and</strong></strong> cover mapp<strong>in</strong>g of the Simiyu catchment (Tanzania)<br />

us<strong>in</strong>g remote sens<strong>in</strong>g techniques. From Pharaohs to<br />

Geo<strong>in</strong>formatics. Cairo, Egypt, April 16-21, 2005, TS27.1:<br />

16 pp.<br />

TAM, V.T., DE SMEDT, F. & BATELAAN, O. 2004.<br />

Estimation of underground rivers <strong>in</strong> a tropical karst area by<br />

way of a multithematic study. In: G. Demarée, M. de<br />

Dapper, & J. Alex<strong>and</strong>re (eds.), Proceed<strong>in</strong>gs Second<br />

International Conference on Tropical Climatology,<br />

Meteorology, <strong>and</strong> Hydrology, Brussels, 13-14 September<br />

2001, Royal Meteorological Institute & Royal Academy of<br />

Overseas Sciences, Brussels, Belgium: 231-244.<br />

TANG, H. & VAN RANST, E. 2005. Is highly <strong>in</strong>tensive<br />

agriculture environmentally susta<strong>in</strong>able A case study<br />

from Fugou county. Ch<strong>in</strong>a. Journal of Susta<strong>in</strong>able<br />

Agriculture 25(3) : 91-102.<br />

VAN LOOY K., SEVERYNS, J., JOCHEMS, H. & DE<br />

SMEDT F, 2005. Predict<strong>in</strong>g patterns of riparian forest<br />

restoration. Large Rivers Vol. 15, No. 1-4, Arch.<br />

Hydrolbiol. Suppl. 155/1-4: 373-390.<br />

VAN RANST, E. & VAN ROMPAEY, K. 2005.<br />

Monitor<strong>in</strong>g atmospheric deposition <strong>and</strong> soil water to assess<br />

nutrient replenishment <strong>in</strong> forest soils. In : Proc. Conf. on<br />

"Management, Use <strong>and</strong> Protection of Soil Resources".<br />

Sofia, Bulgaria. Publish Scie Set – Eco (ISBN : 954-749-<br />

058-3):45-48.<br />

VAN VOSSELEN, A., VERPLANCKE, H. & VAN<br />

RANST, E. 2005. Assess<strong>in</strong>g water consumption of banana<br />

: traditional versus modell<strong>in</strong>g approach. Agricultural Water<br />

Management, 74:201-218.<br />

VERDOODT, A., VAN RANST, E., YE, L. &<br />

VERPLANCKE, H. 2005. A daily multi-layered water<br />

balance to predict water <strong>and</strong> oxygen availability <strong>in</strong> tropical<br />

cropp<strong>in</strong>g systems. Soil Use <strong>and</strong> Management, 21 : 312-<br />

321.<br />

VERDOODT, A. & VAN RANST, E., 2006.<br />

Environmental assessment tools for multi-scale <strong>l<strong>and</strong></strong><br />

<strong>resources</strong> <strong>in</strong>formation systems. A case study of Rw<strong>and</strong>a.,<br />

Agriculture, Ecosystems <strong>and</strong> Environment 114,:170-184.<br />

XU, X., BOECKX, P., VAN CLEEMPUT, O. &<br />

INUBUSHI, K. 2005. M<strong>in</strong>eral nitrogen <strong>in</strong> a rhizosphere<br />

soil <strong>and</strong> <strong>in</strong> st<strong>and</strong><strong>in</strong>g water dur<strong>in</strong>g rice (Oryza sativa L.)<br />

growth : effect of hydroqu<strong>in</strong>one <strong>and</strong> dicy<strong>and</strong>iamide.<br />

Agriculture, Ecosystems <strong>and</strong> Environment 109:107-117.<br />

ZINCK, J.A., BERROTERÁN, J.L., FARSHAD, A.,<br />

MOAMENI, A., WOKABI, S. & VAN RANST, E., 2005.<br />

La sustentabilidad agrícola : un análisis jerárquico. Gaceta<br />

Ecologica, 76:53-72.<br />

TACK, F.M.G., VANHAESEBROECK, Th., VERLOO,<br />

M.G., VAN ROMPAEY, K. & VAN RANST, E. 2005.<br />

Mercury basel<strong>in</strong>e levels <strong>in</strong> Flemish soils (Belgium).<br />

Environmental Pollution, 134:173-179.<br />

- 18 -


PUBLICATIONS<br />

SELECTED BIBLIOGRAPHY<br />

INTRODUCTION TO SOIL SCIENCE : SOILS OF<br />

THE TROPICS, 2005<br />

Bernard P.K. Yerima & E. Van Ranst<br />

Trafford Publish<strong>in</strong>g, Victoria, BC, Canada<br />

ISBN 1-4120-5853 -8 (417 pp.)<br />

MAJOR SOIL CLASSIFICATION SYSTEMS USED<br />

IN THE TROPICS : SOILS OF CAMEROON, 2005<br />

Bernard P.K. Yerima & E. Van Ranst<br />

Trafford Publish<strong>in</strong>g, Victoria, BC, Canada<br />

ISBN 1-4120-5789 -2 (295 pp.)<br />

Explanatory notes on the contents of the two books.<br />

In the develop<strong>in</strong>g countries like Cameroon, the availability<br />

of appropriate textbooks on the soil science discipl<strong>in</strong>e is<br />

very limited <strong>and</strong> when available their acquisition by most<br />

students is limited by prohibitive costs. Moreover, most of<br />

these books make many assumptions, which a beg<strong>in</strong>ner <strong>in</strong><br />

soil science would f<strong>in</strong>d difficult to follow. Further, <strong>in</strong> most<br />

cases these books are strongly oriented towards soils of the<br />

temperate regions so that most of the materials presented <strong>in</strong><br />

form of examples have little relevance for students work<strong>in</strong>g<br />

<strong>in</strong> the tropical environment. The purpose of writ<strong>in</strong>g these<br />

text books was to address the above problems.<br />

The first book<br />

“Introduction to Soil<br />

Science: Soils of the<br />

Tropics” is a general soil<br />

science textbook, which<br />

addresses the basic soil<br />

science pr<strong>in</strong>ciples with<br />

emphasis on tropical<br />

soils. This comprehensive<br />

text comb<strong>in</strong>es both the<br />

basic pr<strong>in</strong>ciples of soil<br />

science. It bridges the gap<br />

between the ma<strong>in</strong> soil<br />

classification systems<br />

used <strong>in</strong> the tropics to<br />

enable a better underst<strong>and</strong><strong>in</strong>g of developments <strong>in</strong> soils by a<br />

wider public, <strong>and</strong> is necessary for undergraduate <strong>and</strong><br />

beg<strong>in</strong>n<strong>in</strong>g graduate students <strong>in</strong> the tropics. It covers <strong>in</strong><br />

great detail a broad spectrum of the elements of soil<br />

science, to <strong>in</strong>clude: the morphological, <strong>physical</strong> <strong>and</strong><br />

chemical properties, soil form<strong>in</strong>g processes, soil<br />

classification, <strong>and</strong> special aspects of soil science such as<br />

soil biology, soil fertility, soil <strong>and</strong> water conservation <strong>and</strong><br />

management, which are unavoidable <strong>in</strong> the cont<strong>in</strong>uum from<br />

basic to applied soil science pr<strong>in</strong>ciples.<br />

This book comb<strong>in</strong>es a basic soil science text with an<br />

applied approach. It is thus very essential for many users<br />

who need a text that is both fundamental <strong>and</strong> practical. The<br />

book is designed with the hope <strong>and</strong> desire that it will be<br />

equally useful to undergraduates <strong>and</strong> graduates,<br />

professional soil scientists, ecologists, environmentalists,<br />

agriculturists, <strong>and</strong> many others <strong>in</strong>terested <strong>in</strong> or <strong>in</strong>volved<br />

with the <strong>l<strong>and</strong></strong>. With the ever <strong>in</strong>creas<strong>in</strong>g world population<br />

<strong>and</strong> the need for fertile soils to grow the necessary food to<br />

susta<strong>in</strong> this population, a good underst<strong>and</strong><strong>in</strong>g of soil<br />

science is necessary to live <strong>in</strong> our environment <strong>and</strong> derive<br />

the basic necessities from it without destroy<strong>in</strong>g it.<br />

The second book “Major<br />

Soil Classification<br />

Systems Used <strong>in</strong> the<br />

Tropics: Soils of<br />

Cameroon” reviews the<br />

major soil classification<br />

systems used <strong>in</strong> the tropics.<br />

This has special<br />

implications for<br />

application <strong>in</strong> Cameroon<br />

where all the three soil<br />

classification systems<br />

(U.S.D.A. Soil Taxonomy,<br />

World Reference Base for<br />

Soil Resources (WRB) <strong>and</strong><br />

the French CPCS soil classification system) are used to<br />

document works on soils. Because of the fact that most<br />

works on soils have been reported at any given time <strong>in</strong> only<br />

one or two of the above soil classification systems, this<br />

book provides a rough table of equivalence, so that work<br />

reported <strong>in</strong> any of the three classification systems can be<br />

valorized.<br />

For better underst<strong>and</strong><strong>in</strong>g of the soils of Cameroon, the<br />

factors of soil formation (climate, vegetation, geology,<br />

geomorphology, hydrology, relief, time <strong>and</strong> human<br />

<strong>in</strong>fluence) which have helped for shape the development of<br />

these soils <strong>in</strong> Cameroon are exam<strong>in</strong>ed. Additionally, the<br />

soil form<strong>in</strong>g processes, which have shaped or <strong>in</strong>fluenced<br />

the development of soils <strong>in</strong> Cameroon are also exam<strong>in</strong>ed.<br />

The logical sequence is to follow up with the discussion of<br />

the soils found <strong>in</strong> Cameroon. The approach here was to<br />

look at the distribution of the soils <strong>in</strong> Cameroon <strong>and</strong> how<br />

they have developed, <strong>and</strong> their morphological, <strong>physical</strong>,<br />

chemical, m<strong>in</strong>eralogical, <strong>and</strong> hydrological properties. The<br />

last section on each soil addresses the management of the<br />

specific soil, their limitations <strong>and</strong> use potentials for<br />

agricultural <strong>and</strong> other uses.<br />

Some of the soils, such as the high shr<strong>in</strong>k/swell clay soils<br />

of North Cameroon, the very deep <strong>and</strong> red soils that<br />

occupy most of the area south of Ngaoundere, the soils<br />

developed from volcanic materials <strong>in</strong> the South-West,<br />

West <strong>and</strong> North-West prov<strong>in</strong>ces, which constitute great<br />

natural <strong>resources</strong> for agriculture <strong>in</strong> Cameroon, were treated<br />

- 19 -


PUBLICATIONS<br />

<strong>in</strong> greater detail. The salt affected soils <strong>in</strong> North Cameroon<br />

<strong>and</strong> soils with (petro)pl<strong>in</strong>thite, which pose a great<br />

impediment to agricultural practice, were also treated <strong>in</strong><br />

greater detail.<br />

In order to give the book the depth it requires, most of the<br />

works carried out especially by the Belgian, Dutch, <strong>and</strong><br />

French soil scientists <strong>and</strong> the FAO experts who have made<br />

a great contribution to the soil science discipl<strong>in</strong>e <strong>in</strong> the<br />

tropics <strong>and</strong> <strong>in</strong> Cameroon <strong>in</strong> particular were consulted. So<br />

was also the contribution by the Cameroon soil scientists.<br />

In 1978 the Work<strong>in</strong>g Group on L<strong>and</strong> Use <strong>and</strong> Rural<br />

Resources of the European Communities proposed that a<br />

Soil Map of EEC countries be prepared us<strong>in</strong>g the data<br />

already collected by FAO for the compilation of a Soil<br />

Map of Europe. It was also proposed that the EEC should<br />

<strong>in</strong>vite Professor R. Tavernier, Chairman of the Soil<br />

Correlation Centre at Ghent University, who was then<br />

already <strong>in</strong> possession of an up-to-date soil map of all EEC<br />

<strong>and</strong> many East-European countries, to oversee the<br />

preparation of such a map.<br />

This book is aimed at serv<strong>in</strong>g as a textbook for courses on<br />

soil formation, classification <strong>and</strong> <strong>l<strong>and</strong></strong> utilization <strong>in</strong><br />

Cameroon <strong>and</strong> as a reference for agricultural scientists,<br />

environmentalists, researchers, teachers, agronomists,<br />

policy makers <strong>and</strong> development workers <strong>in</strong>terested <strong>in</strong> the<br />

tropics, especially Cameroon.<br />

SOIL ATLAS OF EUROPE, 2005<br />

European Soil Bureau Network<br />

European Communities, Luxembourg<br />

ISBN 92-894-8120-x (128 pp.)<br />

The late Prof. Em. Dr. R. Tavernier<br />

1st Director of the International Tra<strong>in</strong><strong>in</strong>g Centre<br />

for Post-Graduate Soil Scientists<br />

The launch event of the European Soil Atlas, organised by<br />

the European Commission's Jo<strong>in</strong>t Research Centre (JRC),<br />

the European Soil Bureau Network (ESBN) <strong>and</strong> the<br />

Department of Environment, Food <strong>and</strong> Rural Affairs<br />

(DEFRA), took place on October 18, 2005 <strong>in</strong> London.<br />

The Atlas, which was formally launched by Lord Bach of<br />

Lutterworth, the Parliamentary Under-Secretary (Lords)<br />

for Susta<strong>in</strong>able Farm<strong>in</strong>g <strong>and</strong> Food at DEFRA, is an<br />

important step <strong>in</strong> creat<strong>in</strong>g further awareness of the<br />

importance of soils.<br />

The publication by the European Commission of the first<br />

ever "Soil Atlas of Europe" is the result of many years of<br />

collaboration between European soil scientists of over 40<br />

national soil surveys <strong>and</strong> soil science <strong>in</strong>stitutions<br />

cooperat<strong>in</strong>g across Europe.<br />

Follow<strong>in</strong>g the decision taken <strong>in</strong> 1978 to prepare a Soil Map<br />

of EEC countries an Advisory Panel with representatives<br />

from each member state was convened. S<strong>in</strong>ce most of the<br />

exist<strong>in</strong>g maps had been prepared before 1974 it was<br />

decided to update them us<strong>in</strong>g more recently acquired<br />

<strong>in</strong>formation. The Soil Map of the EEC countries at scale<br />

1:1,000,000, accompanied by an explanatory text, was<br />

published <strong>in</strong> 1985 <strong>and</strong> was the culm<strong>in</strong>ation of more than 30<br />

years' work.<br />

The European Soil Bureau Network (ESBN), which jo<strong>in</strong>s<br />

soil <strong>in</strong>stitutions throughout cont<strong>in</strong>ental Europe, cont<strong>in</strong>ued<br />

the activities by br<strong>in</strong>g<strong>in</strong>g together soil <strong>in</strong>formation<br />

collected <strong>in</strong> separate European countries, us<strong>in</strong>g very<br />

different methodologies, st<strong>and</strong>ards <strong>and</strong> scientific<br />

backgrounds, <strong>in</strong>to one s<strong>in</strong>gle geographic <strong>in</strong>formation<br />

system. Lengthy transnational sessions between border<strong>in</strong>g<br />

countries have resulted <strong>in</strong> a common fully harmonised soil<br />

geographical database of Europe at a nom<strong>in</strong>al scale of<br />

1:1,000,000. This database has allowed production of the<br />

maps that are at the heart of the new "Soil Atlas of<br />

Europe".<br />

- 20 -


PUBLICATIONS<br />

The Atlas compiles exist<strong>in</strong>g <strong>in</strong>formation on different soil<br />

types <strong>in</strong> easily underst<strong>and</strong>able maps cover<strong>in</strong>g the entire<br />

European Union <strong>and</strong> border<strong>in</strong>g countries, <strong>and</strong> illustrates<br />

vividly the great diversity of European soil. The Atlas<br />

dedicates a large section to the global dimension of soil<br />

protection, <strong>in</strong>clud<strong>in</strong>g a number of plates cover<strong>in</strong>g the<br />

Mediterranean Countries, the Northern Circumpolar<br />

Countries (Eurasia, Green<strong>l<strong>and</strong></strong>, North-America) <strong>and</strong> the<br />

globe. The Atlas also uses specific maps to illustrate<br />

threats such as soil erosion, the decl<strong>in</strong>e of organic matter,<br />

soil seal<strong>in</strong>g by hous<strong>in</strong>g <strong>and</strong> <strong>in</strong>frastructure, etc.<br />

The Atlas is <strong>in</strong>tended to be a step towards rais<strong>in</strong>g public<br />

awareness on the importance <strong>and</strong> the key role of soil for<br />

many human activities <strong>and</strong> for the survival of ecosystems.<br />

Not only climate change, but also desertification <strong>and</strong> loss<br />

of biodiversity are strongly affect<strong>in</strong>g soils globally, mak<strong>in</strong>g<br />

the Atlas relevant to much larger community of<br />

stakeholders <strong>in</strong>volved <strong>in</strong> the implementation of the three<br />

"Rio Conventions" <strong>and</strong> allow<strong>in</strong>g the exploration of<br />

possible synergies among <strong>in</strong>ternational agreements towards<br />

global soil protection.<br />

The Atlas is <strong>in</strong>tended not only for the specialized reader<br />

but also for the general public, aim<strong>in</strong>g to "bridge the gap"<br />

between soil science, policymak<strong>in</strong>g <strong>and</strong> public knowledge.<br />

By address<strong>in</strong>g a non-specialized audience, the Atlas will<br />

<strong>in</strong>crease public awareness <strong>and</strong> underst<strong>and</strong><strong>in</strong>g of the<br />

diversity of soils <strong>and</strong> of the need to protect this precious<br />

resource.<br />

In November 2005, the Soil Atlas of Europe has been<br />

awarded the prestigious "GOLDEN SICKLE" prize at the<br />

2005 Agrokomplex International Agricultural <strong>and</strong> Food<br />

Fair held <strong>in</strong> Nitra <strong>in</strong> the Slovak Republic.<br />

In his book, Mr. Rahman<br />

gives an overview of<br />

Bangladeshi soils, <strong>in</strong>clud<strong>in</strong>g<br />

floodpla<strong>in</strong> soils, piedmont<br />

pla<strong>in</strong> soils, soils of<br />

miscellaneous sediment<br />

deposits, peat-bas<strong>in</strong>-soils, acid<br />

sulphate soils, terrace soils<br />

<strong>and</strong> hill soils. The book<br />

conta<strong>in</strong>s the list of soil series,<br />

the areas they cover <strong>in</strong> square<br />

miles, <strong>and</strong> their broad<br />

physiography, <strong>and</strong> adds an overview of the major soils of<br />

the Upazillas. About 70 pages of appendices give profile<br />

descriptions <strong>and</strong> chemical compositions of representative<br />

soils of the different regions.<br />

Published by Darpon Publications, Dhaka, Bangladesh<br />

MAPPING OF THE SOIL<br />

Jean-Paul Legros<br />

Science Publishers, Enfield, NH, USA<br />

ISBN 1-57808-363-x<br />

This book presents mapp<strong>in</strong>g methods relevant to the soil<br />

mantle <strong>and</strong> considers recent advances made <strong>in</strong> the<br />

discipl<strong>in</strong>e through the use of GIS, databases, multicriteria<br />

analysis, fuzzy set theory <strong>and</strong> computer modell<strong>in</strong>g. It is<br />

divided <strong>in</strong>to ten chapters that discuss methodological<br />

foundations, different phases of the work, computer<br />

process<strong>in</strong>g, applications, exercises, <strong>and</strong> current state of the<br />

art <strong>in</strong> various countries.<br />

The Atlas has a nom<strong>in</strong>al cost of 25 €. Formal distribution<br />

will be through the Office of Official Publications of the<br />

European Communities (OPOCE) <strong>in</strong> Luxembourg.<br />

For further <strong>in</strong>formation, please visit the JRC website :<br />

http://eusoils.jrc.it/projects/soil_atlas/ <strong>in</strong>dex.htmlr<br />

SOILS OF BANGLADESH<br />

M. Rezaur Rahman<br />

Darpon Publications, Dhaka, Bangladesh<br />

ISBN 984-32-2258-x<br />

Eric Van Ranst<br />

Member of ESBN<br />

Mr. Rezaur Rahman obta<strong>in</strong>ed an M.Sc. degree <strong>in</strong> Soil<br />

Science from the University of Dhaka (1957), <strong>and</strong> an<br />

M.Sc. degree <strong>in</strong> Soil Science (Soil Survey <strong>and</strong> L<strong>and</strong><br />

Classification) at the International Tra<strong>in</strong><strong>in</strong>g Centre for<br />

Post-Graduate Soil Scientists, Ghent University (1966). He<br />

was a consultant <strong>in</strong> many projects funded by UNDP, ADB,<br />

etc. <strong>and</strong> expert/consultant for FAO.<br />

- 21 -


SOILS AND MAPS<br />

WOSSAC (World Soil Survey Archive <strong>and</strong><br />

Catalogue)<br />

<strong>in</strong>formation. There are currently many thous<strong>and</strong> volumes <strong>in</strong><br />

store <strong>in</strong> the process of be<strong>in</strong>g classified <strong>and</strong> archived.<br />

WOSSAC <strong>in</strong> Use<br />

The WOSSAC Archive can be of enormous assistance for<br />

a range of applications <strong>and</strong> activities, from national <strong>and</strong><br />

regional strategic <strong>l<strong>and</strong></strong> plann<strong>in</strong>g, to manag<strong>in</strong>g development<br />

<strong>and</strong> relief efforts, to the conduct of academic research.<br />

WOSSAC conta<strong>in</strong>s a huge wealth of unique reports, maps,<br />

manuscripts, photographs <strong>and</strong> albums cover<strong>in</strong>g scores of<br />

countries around the world over a period of many decades.<br />

It is clear that the services provided by WOSSAC have the<br />

potential to secure extremely costly data from loss, <strong>and</strong><br />

thereby to ensure that the <strong>in</strong>tended benefits of soil <strong>studies</strong><br />

are realised. This is especially the case for <strong>studies</strong> <strong>in</strong> less<br />

developed countries where the data storage <strong>in</strong>frastructure<br />

<strong>and</strong> data ma<strong>in</strong>tenance may be unsuited for the long term<br />

stor<strong>in</strong>g of large quantities of data.<br />

Mission<br />

The mission of the World Soil Surveys Archive <strong>and</strong><br />

Catalogue (WOSSAC) is to provide a secure home for soil<br />

survey reports <strong>and</strong> maps produced by British companies<br />

<strong>and</strong> surveyors overseas <strong>in</strong> the last 80 years <strong>in</strong> 250<br />

countries, with a view to ensur<strong>in</strong>g their endur<strong>in</strong>g<br />

availability <strong>and</strong> protection.<br />

Background<br />

Large numbers of substantial soil surveys have been made<br />

worldwide by British companies over the past 80 years,<br />

ma<strong>in</strong>ly funded by development assistance donors,<br />

represent<strong>in</strong>g some 250 countries. A rough estimate, almost<br />

certa<strong>in</strong>ly on the low side, is that such surveys number many<br />

thous<strong>and</strong> <strong>and</strong> by today's prices would have cost well over<br />

£200 million. This is an extremely valuable bank of<br />

<strong>in</strong>ternational data about soils, their nature, properties <strong>and</strong><br />

potential use.<br />

This large body of <strong>in</strong>formation about world soils is now <strong>in</strong><br />

grave danger of becom<strong>in</strong>g lost, destroyed or generally<br />

unavailable as the orig<strong>in</strong>al donor fund<strong>in</strong>g agencies have<br />

been subject to reorganisation, <strong>and</strong> the companies that<br />

produced the surveys have been acquired, merged,<br />

downsized or closed down, <strong>and</strong> the soil surveyors<br />

themselves are now retir<strong>in</strong>g or deceased.<br />

There is no current organised resource-base detail<strong>in</strong>g what<br />

exists, <strong>in</strong> what state or how available it is. Therefore at the<br />

behest of the British Society of Soil Sciences (BSSS) <strong>and</strong><br />

with the full support of the International Union of Soil<br />

Sciences (IUSS) <strong>and</strong> the Tropical Agriculture Association<br />

(TAA), the National Soil Resources Institute (NSRI)<br />

located at Cranfield University has undertaken to<br />

catalogue, archive <strong>and</strong> manage this important body of<br />

These services are extremely important for academics,<br />

researchers, development organisation, <strong>and</strong> ultimately for<br />

those people liv<strong>in</strong>g <strong>in</strong> studied areas. WOSSAC therefore<br />

offers a excellent example or model for data security <strong>and</strong><br />

shar<strong>in</strong>g <strong>and</strong> is clearly the most important Internet <strong>resources</strong><br />

for soil survey data.<br />

Longer Term Developments<br />

It is known that significant archives of soil survey reports<br />

stimulated by other countries exist with<strong>in</strong> the USA, the<br />

Nether<strong>l<strong>and</strong></strong>s, France <strong>and</strong> the Food <strong>and</strong> Agriculture<br />

Organisation (FAO). A future long-term aim of WOSSAC<br />

is therefore to establish l<strong>in</strong>ks with these other world<br />

databases to create a World Database of Soil Surveys. To<br />

achieve this aim fund<strong>in</strong>g will be sought from the major<br />

fund<strong>in</strong>g agencies to support the ongo<strong>in</strong>g development of<br />

WOSSAC <strong>and</strong> to establish its l<strong>in</strong>ks with other such major<br />

databases.<br />

Publicis<strong>in</strong>g WOSSAC<br />

It is very important to draw the WOSSAC project to the<br />

attention of the soil science community. We would<br />

welcome any assistance <strong>in</strong> this matter that can be offered.<br />

One practical means to achieve this is to pr<strong>in</strong>t off copies of<br />

the WOSSAC poster :<br />

(http://www.wossac.com/downloads/wossac_poster.pdf)<br />

<strong>and</strong> to display it. Also, if there are <strong>in</strong>dividuals or<br />

organisations who you th<strong>in</strong>k would be <strong>in</strong>terested <strong>in</strong> our<br />

work – please let us (wossac@cranfield.ac.uk), or them<br />

know.<br />

E. Van Ranst<br />

- 22 -


SOILS AND MAPS<br />

THE SOIL MAPS OF AFRICA<br />

European Digital Archive of Soil Maps -<br />

EuDASM<br />

http://eusoils.jrc.it/esdb_archive/EuDASM/Africa.<strong>in</strong>dex.ht<br />

m<br />

Soil maps are the build<strong>in</strong>g blocks of most current soil<br />

<strong>in</strong>formation. The user of present-day, derived <strong>in</strong>formation<br />

should have easy access to the source material, if only to<br />

assess the reliability of the derived material.<br />

But, <strong>in</strong> many countries, soil maps are be<strong>in</strong>g lost because of<br />

lack of proper attention to storage <strong>and</strong> retrieval, often<br />

compounded by a loss of <strong>in</strong>stitutions that have been<br />

responsible for the acquisition <strong>and</strong> ma<strong>in</strong>tenance of soil <strong>and</strong><br />

<strong>l<strong>and</strong></strong> <strong>resources</strong> data. This problem is acute <strong>in</strong> develop<strong>in</strong>g<br />

<strong>and</strong> transitional countries where valuable data, currently<br />

only available on paper, must be digitized before they are<br />

lost forever.<br />

In Africa, though not only <strong>in</strong> Africa, this type of<br />

<strong>in</strong>formation is rapidly be<strong>in</strong>g lost; much is already lost. The<br />

digitization of the African maps will enable the African<br />

countries to recover <strong>and</strong> re-use their soil <strong>in</strong>formation.<br />

Translation of soil <strong>in</strong>formation from paper maps <strong>and</strong><br />

reports <strong>in</strong>to digital format is a prerequisite of the next step<br />

- the development of a digital <strong>in</strong>formation system on soil<br />

<strong>and</strong> terra<strong>in</strong> that may be drawn upon for manifold<br />

applications.<br />

The maps (1920s-1990s) have been scanned <strong>and</strong> are<br />

available at the European Digital Archive of soil maps<br />

(EuDASM). They can be searched by country, year, scale<br />

or keyword. The maps can be viewed <strong>and</strong> downloaded as<br />

JPG.<br />

E. Van Ranst<br />

PROJECT PROFILES<br />

ENVASSO – ENVironmental ASsessment<br />

of Soil for mOnitor<strong>in</strong>g<br />

March, 2006 – March, 2008<br />

Funded by : European Commission DG RTD Framework Programme 6<br />

Project collaborators: Marc KIBBLEWHITE, Robert JONES (Cranfield<br />

University, United K<strong>in</strong>gdom); Sigi HUBER (Umweltbundesamt GMBH,<br />

Austria); D. ARROUAYS (INRA, France); Ra<strong>in</strong>er BARITZ<br />

(Bundesanstalt fuer Geowisschenschaften und Rohstoffe, Germany);<br />

Erika MICHELI (Szent Istvan University, Hungary) supported by 32<br />

additional partners drawn from all 25 EU member states among which<br />

Eric VAN RANST <strong>and</strong> Ann VERDOODT (Laboratory of Soil Science,<br />

UGent, Belgium)<br />

Soil is a vital non-renewable resource essential to human<br />

life <strong>and</strong> the ecosystems that support this. It represents<br />

much of the natural capital available to European Citizens.<br />

Increas<strong>in</strong>gly, soil is recognised as a habitat <strong>in</strong> its own right<br />

as well as a foundation to others. Liv<strong>in</strong>g soil systems<br />

susta<strong>in</strong> delivery of hugely valuable ecosystem services<br />

(biodiversity, clean air <strong>and</strong> water, food security <strong>and</strong><br />

cultural heritage, etc).<br />

European policy is that soil protection should be brought<br />

up to the same level as that for air <strong>and</strong> water. Better<br />

scientific <strong>in</strong>formation about soil systems <strong>and</strong> their<br />

distribution is needed to ensure that soil is managed well at<br />

all levels (local, regional <strong>and</strong> cont<strong>in</strong>ental) as part of the<br />

susta<strong>in</strong>able achievement of strategic European goals (c.f.<br />

Lisbon Objectives). The “Soil Thematic Strategy” focuses<br />

on the characterisation <strong>and</strong> monitor<strong>in</strong>g of different soil<br />

threats recognized with<strong>in</strong> Europe as a basis for soil policies<br />

ensur<strong>in</strong>g soil protection. There is a strong dem<strong>and</strong> for a set<br />

of well-founded pr<strong>in</strong>ciples <strong>and</strong> theory, processes <strong>and</strong> tools<br />

for establish<strong>in</strong>g <strong>and</strong> ma<strong>in</strong>ta<strong>in</strong><strong>in</strong>g common criteria <strong>and</strong><br />

<strong>in</strong>dicators for the characterisation of European soils.<br />

ENVASSO – ENVironmental ASsessment of Soil for<br />

monitor<strong>in</strong>g project applies a holistic approach to soil<br />

protection through the robust <strong>and</strong> defensible selection of<br />

criteria, thresholds <strong>and</strong> <strong>in</strong>dicators based on harmonised<br />

approaches to soil <strong>in</strong>formation. This approach is<br />

encompassed through the consideration of real, exist<strong>in</strong>g<br />

data <strong>and</strong> approaches to soil monitor<strong>in</strong>g, <strong>and</strong> data storage<br />

<strong>and</strong> <strong>in</strong>terpretation across all Member States. The ma<strong>in</strong><br />

objectives of the project are the design <strong>and</strong> test<strong>in</strong>g of a<br />

s<strong>in</strong>gle, <strong>in</strong>tegrated, EU-wide <strong>and</strong> operational set of<br />

measurable criteria <strong>and</strong> <strong>in</strong>dicators. They will provide the<br />

scientific basis to populate a harmonised comprehensive<br />

European soil <strong>and</strong> <strong>l<strong>and</strong></strong> <strong>in</strong>formation system. These<br />

objectives will be realised by 5 core partners supported by<br />

32 additional partners ensur<strong>in</strong>g the maximum impact to<br />

enhance soil protection at the European level.<br />

New scientific underst<strong>and</strong><strong>in</strong>g of soil functionality will be<br />

comb<strong>in</strong>ed with expertise on the characterisation <strong>and</strong><br />

assessment of soil profiles, lead<strong>in</strong>g to recommendations<br />

that are operationally feasible <strong>and</strong> robust. Tak<strong>in</strong>g full<br />

account of exist<strong>in</strong>g, modified or new survey <strong>and</strong> database<br />

<strong>in</strong>itiatives, formal protocols, procedures, tools <strong>and</strong><br />

implementation recommendations will be developed for<br />

the collection, collation <strong>and</strong> report<strong>in</strong>g of harmonised soil<br />

European-wide <strong>in</strong>formation. ENVASSO will distil this<br />

- 23 -


PROJECT PROFILES<br />

knowledge <strong>and</strong> expertise <strong>in</strong>to testable methodologies, a<br />

tested prototype of a work<strong>in</strong>g database, <strong>and</strong> of Procedures<br />

<strong>and</strong> Protocols for Harmonised Soil Assessment.<br />

<strong>resources</strong> database for Rw<strong>and</strong>a enable us to develop a<br />

scientifically sound Great Lakes Area SOTER database<br />

from the detailed, semi-detailed <strong>and</strong> reconnaissance soil<br />

maps <strong>and</strong> the abundant morphological <strong>and</strong> analytical soil<br />

profile data.<br />

SOTER mapp<strong>in</strong>g is similar to <strong>l<strong>and</strong></strong> systems or<br />

physiographic soil mapp<strong>in</strong>g but with stronger emphasis on<br />

the terra<strong>in</strong>-soil relationship. A SOTER unit represents a<br />

unique comb<strong>in</strong>ation of terra<strong>in</strong> <strong>and</strong> soil characteristics; the<br />

methodology identifies areas of <strong>l<strong>and</strong></strong> with a dist<strong>in</strong>ctive<br />

pattern of <strong>l<strong>and</strong></strong>form, lithology, surface form, slope, parent<br />

material <strong>and</strong> soil. The work will consist of :<br />

Establish<strong>in</strong>g pilot zones to test the proposed approaches to monitor<strong>in</strong>g<br />

<strong>and</strong> <strong>in</strong>dicators <strong>and</strong> the efficacy of the database specification<br />

A. Verdoodt<br />

SOIL AND TERRAIN DATABASE OF<br />

CENTRAL AFRICA (THE GREAT LAKES<br />

AREA : D.R. CONGO, BURUNDI AND<br />

RWANDA)<br />

Oct 1, 2005 – Jun 1, 2006<br />

Funded by : Food <strong>and</strong> Agricultural Organisation<br />

Project collaborators: Eric VAN RANST, Ann VERDOODT, Johan VAN<br />

DE WAUW, Clémence GOYENS (Laboratory of Soil Science, UGent,<br />

Belgium); Geert BAERT (Hogeschool Gent, Belgium); David DENT,<br />

V<strong>in</strong>cent VAN ENGELEN (ISRIC, The Nether<strong>l<strong>and</strong></strong>s); Max Alonso<br />

FERNANDEZ, Johan LAVREAU (Royal Museum for Central Africa,<br />

Belgium)<br />

This project will result <strong>in</strong> a st<strong>and</strong>ardized soil <strong>and</strong> terra<strong>in</strong><br />

(SOTER) database for the central part of the African<br />

cont<strong>in</strong>ent, i.e. the Great Lakes Area compris<strong>in</strong>g the<br />

Democratic Republic Congo (scale 1:2 M), <strong>and</strong> Rw<strong>and</strong>a<br />

<strong>and</strong> Burundi (scale 1:1 M).<br />

In these countries, natural <strong>resources</strong> <strong>in</strong>formation is not<br />

easily accessible, sometimes miss<strong>in</strong>g <strong>and</strong> often not <strong>in</strong> a<br />

st<strong>and</strong>ard format. This is a constra<strong>in</strong>t on national, regional<br />

<strong>and</strong> <strong>in</strong>ternational plann<strong>in</strong>g <strong>and</strong> decision mak<strong>in</strong>g on<br />

development <strong>and</strong> the environment.<br />

The currently available, harmonised, digital soils<br />

<strong>in</strong>formation cover<strong>in</strong>g the area is the Soil Map of the World<br />

(FAO-Unesco 1974) at a scale of 1:5 M. Of the total area<br />

of the three countries - 2.3 million km 2 - only 0.4 million<br />

has been surveyed. Now, less than 1 per cent of the area<br />

has soil <strong>in</strong>formation <strong>in</strong> digital format but this will exp<strong>and</strong><br />

to 15 per cent over the com<strong>in</strong>g years by jo<strong>in</strong>t Belgian-DRC<br />

digitis<strong>in</strong>g activities.<br />

The ongo<strong>in</strong>g check<strong>in</strong>g of exist<strong>in</strong>g natural <strong>resources</strong> data of<br />

DR Congo <strong>and</strong> the recent f<strong>in</strong>alisation of a digital natural<br />

. Gather<strong>in</strong>g the relevant, exist<strong>in</strong>g soil <strong>and</strong> terra<strong>in</strong> data<br />

. Creation of physiographic maps of the region based<br />

on satellite data (SRTM)<br />

. Creation of lithological maps of the region us<strong>in</strong>g<br />

exist<strong>in</strong>g geological maps at different scales<br />

. Generalis<strong>in</strong>g the spatial soil data at 1:1 M or 1:2 M<br />

scale <strong>and</strong> select<strong>in</strong>g relevant soil profiles<br />

. Harmonis<strong>in</strong>g the soil data us<strong>in</strong>g the SOTER<br />

guidel<strong>in</strong>es<br />

. Compilation of the SOTER database compris<strong>in</strong>g the<br />

harmonised spatial <strong>and</strong> tabular data<br />

A. Verdoodt<br />

A STRATEGY FOR REVIVING<br />

THE VITAL BREADBASKET OF THE<br />

DEMOCRATIC REPUBLIC OF CONGO<br />

THROUGH INTEGRATED SOIL<br />

FERTILITY MANAGEMENT COUPLED TO<br />

RESILIENT GERMPLASM<br />

IN CASSAVA-BASED SYSTEMS<br />

01/09/2005-31/08/2010<br />

Funded by VLIR-UDC<br />

Promoter(s) : Prof. R. Merckx (KULeuven) <strong>and</strong> Prof. P. Boeckx (UGent)<br />

The project aims primarily at improv<strong>in</strong>g food security <strong>in</strong><br />

the DRC by <strong>in</strong>troduc<strong>in</strong>g improved soil fertility<br />

management systems that also susta<strong>in</strong> the natural resource<br />

base. While a significant amount of research <strong>in</strong> this area is<br />

part of the proposal, a strong emphasis is on restor<strong>in</strong>g the<br />

communication channels between research community <strong>and</strong><br />

extension agents <strong>and</strong>/or farmers <strong>and</strong> on enhanc<strong>in</strong>g the<br />

capacity to carry out state-of-the-art <strong>and</strong> relevant research<br />

by the Congolese research community. The chosen<br />

approach relies on adaptation of proven solutions to the<br />

problem of degraded soil fertility <strong>and</strong> at the same time<br />

rebuilds capacity <strong>in</strong> DRC to revamp research <strong>in</strong> these<br />

areas. F<strong>in</strong>ally, the project implementation builds on longestablished<br />

partnerships <strong>and</strong> proven work<strong>in</strong>g relations<br />

between the project <strong>in</strong>itiators <strong>and</strong> aims at capitaliz<strong>in</strong>g on<br />

earlier <strong>in</strong>vestments i.e. by VLIR.<br />

P. Boeckx<br />

- 24 -


COMMUNICATIONS RECEIVED<br />

NOMINATIONS-APPOINTMENTS<br />

Prof. Dr. E. Van Ranst is elected as Vice-Chairman of the<br />

Class of Natural <strong>and</strong> Medical Sciences of the Royal<br />

Academy for Overseas Sciences for 2006. In 2007, he will<br />

be Chairman.<br />

PROMOTIONS-AWARDS<br />

Ph.D promotions<br />

Dr. A. Ariv<strong>in</strong> Rivaie (M.Sc. Soil Science<br />

<strong>and</strong> Eremology, 1998) obta<strong>in</strong>ed a Ph.Ddegree<br />

<strong>in</strong> Soil Science from Massey<br />

University, New Zea<strong>l<strong>and</strong></strong>, with a<br />

dissertation on Phosphorous fertilizer<br />

response of second-rotation P<strong>in</strong>us radiata<br />

St<strong>and</strong>s on an Allophanic soil <strong>and</strong> a Pumice soil. Follow<strong>in</strong>g<br />

his Ph.D. promotion, Dr. A. Ariv<strong>in</strong> Rivaie resumed his<br />

work at the Indonesian Centre for Estate Crop Research<br />

<strong>and</strong> Development (ICECRD) <strong>in</strong> Bogor, Indonesia.<br />

Soil Science, 1975), Prof. Dr. Zulkifli Hj. Shamsudd<strong>in</strong>,<br />

Prof. Dr. Hj. Shamshudd<strong>in</strong> Jusop (M.Sc. Soil Science,<br />

1981, Ph.D., 1982), Dr. Ghulam Mohammed B<strong>in</strong> Hashim,<br />

<strong>and</strong> Dr. Sharifudd<strong>in</strong> B<strong>in</strong> Abdul Hamid. These awards were<br />

given <strong>in</strong> view of their passion <strong>and</strong> contribution to the<br />

society <strong>and</strong> soil science.<br />

OBITUARY<br />

Ms. Baeyens-Claessens conveyed to us the news of the<br />

death of her husb<strong>and</strong> Lode Baeyens. Mr. Lode Baeyens<br />

was born <strong>in</strong> Antwerp (Belgium) on March 5, 1921. He<br />

obta<strong>in</strong>ed a degree <strong>in</strong> agriculture from the KULeuven <strong>in</strong><br />

1952 <strong>and</strong> the M.Sc. <strong>in</strong> Soil Science at the ITC-Ghent <strong>in</strong><br />

1970. At the blessed age of almost 85 years, follow<strong>in</strong>g a<br />

courageously carried disease, Mr. Baeyens died on<br />

February 13, 2005.<br />

Dr. Shahla Mahmoodi <strong>in</strong>formed us about the death of Dr.<br />

Mohamad Hassan Banaei. Mr. Banaei was born <strong>in</strong> Iran<br />

on June 5, 1938. He obta<strong>in</strong>ed a B.Sc. degree <strong>in</strong> Geology<br />

from the University of Teheran. In 1970, he obta<strong>in</strong>ed the<br />

M.Sc. degree (Lic. Soil Suvey) at the ITC-Ghent. He was<br />

the deputy director of the Soil <strong>and</strong> Water Research Institute<br />

<strong>in</strong> Iran. Mr. Banaei died on February 7, 2006<br />

CAREER MOVES<br />

Dr. Mvondo Ze (M.Sc. Soil Science, 1979, <strong>and</strong> Ph.D.,<br />

1990) has been appo<strong>in</strong>ted as the Vice-Dean of Academic<br />

Affairs <strong>in</strong> the Faculty of Science, Dschang University,<br />

Cameroon.<br />

VISITORS<br />

Prof. Em. Keith Smith of the School of Geosciences,<br />

University of Ed<strong>in</strong>gburgh, UK. An even<strong>in</strong>g of discussion<br />

<strong>and</strong> reflection of climate change.<br />

NEWS FROM THE MALAYSIAN<br />

SOCIETY OF SOIL SCIENCE (MSSS)<br />

The Malaysian Society of Soil Science recently awarded<br />

six persons to the MSSS Fellow Award, which carries the<br />

title "FMSoil". They are : Prof. Dr. Wan Sulaiman B<strong>in</strong><br />

Wan Harun, Dr. E. Pushparajah (Ph.D., 1977), Mr. Chew<br />

Poh Soon, Dr. Wan Mohamed Noord<strong>in</strong> Wan Daud (M.Sc.<br />

Dr. Hari Eswaran br<strong>in</strong>gs the news of the<br />

decease of Dr. Jawahar Lal Sehgal. Dr.<br />

Sehgal was born <strong>in</strong> 1937 <strong>in</strong> Ludhiana,<br />

India. Dr. Sehgal obta<strong>in</strong>ed an M.Sc. degree<br />

<strong>in</strong> Agriculture from Punjab. In 1967, he<br />

obta<strong>in</strong>ed an M.Sc. degree at ITC-Ghent.<br />

Also <strong>in</strong> Ghent, he accomplished his Ph.D.<br />

research <strong>in</strong> 1970. Dr. Sehgal was active as<br />

a soil specialist, noteably <strong>in</strong> Iraq as well as<br />

<strong>in</strong> his native country at the Department of<br />

Soils at Punjab University <strong>and</strong> as Director<br />

of the National Bureau of Soil Survey <strong>and</strong><br />

L<strong>and</strong> Use Plann<strong>in</strong>g (Indian Council of<br />

Agricultural Research) <strong>in</strong> Nagpur. Dr.<br />

Sehgal passed away on April 11, 2006.<br />

LETTER FROM AFRICA<br />

Dear Professors, former <strong>and</strong> actual students,<br />

In September 2005 my son, wife <strong>and</strong> me left<br />

Belgium for Ug<strong>and</strong>a. One year after graduat<strong>in</strong>g from the<br />

MSc course PLR, I have found the job I was hop<strong>in</strong>g for.<br />

- 25 -


COMMUNICATIONS RECEIVED<br />

The Belgian NGO "Broederlijk Delen" is send<strong>in</strong>g me out to<br />

enforce the Ug<strong>and</strong>an ngo Kiima Foods.<br />

Kiima Foods is a local NGO based <strong>in</strong> Kasese that<br />

supports 17 farmer groups, which compromise around 400<br />

house holds, throughout the Kasese District. Our farmers<br />

are situated at the footslope of the Southern end of the<br />

Rwenzori Mounta<strong>in</strong>s. The ma<strong>in</strong> cash crops are p<strong>in</strong>eapple,<br />

<strong>in</strong> the valley, <strong>and</strong> coffee on the mounta<strong>in</strong> slopes. Untill<br />

present, Kiima Foods has been active <strong>in</strong> strengthen<strong>in</strong>g the<br />

farmers <strong>in</strong>to functional groups <strong>and</strong> secondly, the groups<br />

<strong>in</strong>to cooperatives, where farmers can sell their products at<br />

more stable prices. Cooperation between farmers, record<strong>in</strong>g<br />

<strong>and</strong> market orientation has been the mayor focus of Kiima<br />

Foods. Now they have reached a turn<strong>in</strong>g po<strong>in</strong>t at which<br />

they need to <strong>in</strong>crease yields to commercial <strong>and</strong> stable<br />

figures <strong>and</strong> try to manufacture some products, like wet<br />

coffee process<strong>in</strong>g <strong>and</strong> dry<strong>in</strong>g – cann<strong>in</strong>g p<strong>in</strong>eapple. For<br />

several years now, some of the p<strong>in</strong>eapple farmers are<br />

fac<strong>in</strong>g yield decreases due to a k<strong>in</strong>d of fungus <strong>in</strong>fection. If<br />

cooperation proceeds well, we hope to identify the fungus<br />

with the help of a Belgian student of the Hogeschool<br />

Ghent who is comm<strong>in</strong>g <strong>in</strong> August – September 2006 for<br />

her Master-thesis.<br />

Besides support<strong>in</strong>g farmers, Kiima Foods also<br />

setted up a secondary farmers school <strong>and</strong> a buss<strong>in</strong>ess<br />

school for farmer children who cannot pay (higher) school<br />

fees. Start<strong>in</strong>g from March I will teach the subject Soil<br />

Science for two hours per week. The farmers school also<br />

conta<strong>in</strong>s farm<strong>l<strong>and</strong></strong>, that is used for own food supply <strong>and</strong><br />

some experimental fields. On one field we are <strong>in</strong>stall<strong>in</strong>g a<br />

drip-irrigation system <strong>in</strong> the hope to bridge the dry season<br />

<strong>in</strong> Kasese. If the system performs well, we can <strong>in</strong>troduce<br />

irrigation techniques at some farmers groups. In May –<br />

August the farmers school will be equiped with a small soil<br />

laboratory <strong>and</strong> climatic station. The British High<br />

Commission <strong>in</strong> Kampala agreed to support our laboratory -<br />

climatic station <strong>and</strong> we will be able to analyse pH(H 2O),<br />

pH(KCl), EC, soil texture, soil water content (general) <strong>and</strong><br />

soil water content at wilt<strong>in</strong>g po<strong>in</strong>t. The climatic station<br />

will record ra<strong>in</strong>fall, humidity, max. <strong>and</strong> m<strong>in</strong>. temperature<br />

<strong>and</strong> water transpiration from a class-A evaporation pan.<br />

At this stage, the laboratory will ma<strong>in</strong>ly function as a<br />

learn<strong>in</strong>g tool for the students. At a later stage we hope to<br />

exp<strong>and</strong> the laboratory so we can provide farmers (<strong>and</strong> if<br />

possible plantation managers) with detailed soil advises.<br />

Next time I hope to <strong>in</strong>form you whether the<br />

<strong>in</strong>stallation of the lab <strong>and</strong> climatic station proceeded well<br />

<strong>and</strong> if we managed to f<strong>in</strong>d a solution of the fungus<br />

<strong>in</strong>fections. I wish everybody good luck with their carreers<br />

or study time.<br />

Best regards,<br />

Nikolas Bosscher, M.Sc. Physical L<strong>and</strong> Resources, 2004<br />

ALUMNI SAY GOODBYE TO PROF.<br />

LANGOHR<br />

Some people always stay young, <strong>and</strong> as many<br />

know Roger Langohr is one of them. Nevertheless he<br />

reached the DOOR which separates what he likes from<br />

what he is supposed to do : he officially retired on 1 st of<br />

October 2005. A small group of former ITC students<br />

decided <strong>in</strong> August 2004 to mark this milestone.<br />

Encouraged by the enthusiasm of the fellows contacted<br />

<strong>and</strong> with the precious help of Viviane, Roger Langohr’s<br />

wife, they managed to schedule a surprise week-end for the<br />

23-25 September 2005 <strong>in</strong> the Ardennes, only 10 km from<br />

one of Roger’s favourite ITC excursion po<strong>in</strong>ts : the raised<br />

bogs with their p<strong>in</strong>go traces close to Eupen <strong>in</strong> SE<br />

Belgium. Believe it or not, for once they managed to get<br />

Roger speechless when he found 11<br />

alumni <strong>and</strong> familiy that had come<br />

from as far as France, Hungary,<br />

Ire<strong>l<strong>and</strong></strong>, Norway, Portugal,<br />

Switzer<strong>l<strong>and</strong></strong> <strong>and</strong> obviously<br />

Belgium. Each of them learned to<br />

read the book of nature, <strong>and</strong> found<br />

out that soil sections have to be<br />

deep <strong>and</strong> large <strong>and</strong> that a good study has to go from field<br />

to micro scale, without ignor<strong>in</strong>g the meso scale. They were<br />

also told that small is beautiful, <strong>and</strong> realised that when<br />

Roger becomes enthusiastic the def<strong>in</strong>ition of SMALL<br />

takes a new mean<strong>in</strong>g! Last but not least <strong>in</strong> that<br />

microenvironment, where FREEDOM was more than<br />

important, they benefited from an <strong>in</strong>comparable scientific<br />

<strong>and</strong> human altruism radiated from Roger. As a<br />

consequence they felt that this last week-end of September<br />

2005 was a modest attempt to express their s<strong>in</strong>cere<br />

gratitude for the time they could gravitate around him <strong>and</strong><br />

for shar<strong>in</strong>g his scientific <strong>and</strong> human experience.<br />

On Saturday even<strong>in</strong>g Roger Langohr’s scientific<br />

“children” formed a commission to evaluate his<br />

professional activities <strong>and</strong> decide if he was allowed to<br />

retire or not.<br />

- 26 -


COMMUNICATIONS RECEIVED<br />

First of all an overview was given of Roger’s<br />

curriculum vitae with several of the anecdotes <strong>and</strong> a good<br />

highlight of many th<strong>in</strong>gs he has done <strong>and</strong> also of those<br />

that he has not (yet) accomplished! This was followed by a<br />

slideshow illustrat<strong>in</strong>g Roger <strong>in</strong> several aspects of his career<br />

such as teach<strong>in</strong>g, student excursions, conferences, parties<br />

etc.<br />

were will<strong>in</strong>g to travel with their family up to 2000 km to<br />

celebrate his retirement.<br />

To avoid any misunderst<strong>and</strong><strong>in</strong>g Roger had partly<br />

retired from Ghent University at the date of 1 st of October<br />

2005, but he will certa<strong>in</strong>ly not retire as a SCIENTIST. As<br />

we expected he will cont<strong>in</strong>ue with follow<strong>in</strong>g up his many<br />

projects <strong>and</strong> the ideas he has launched with passion.<br />

We hope Roger will keep this enthusiasm for<br />

many more years <strong>and</strong> we are look<strong>in</strong>g forward to the many<br />

more meet<strong>in</strong>gs, discussions <strong>and</strong> field visits to come!<br />

Roger’s Scientific Children<br />

(communicated by J. Becze-Deák)<br />

Those who wish to see a few images of this meet<strong>in</strong>g can<br />

visit the follow<strong>in</strong>g Internet page :<br />

http://fr.pg.photos.yahoo.com/ph/juditbd/my_photos<br />

"The Commission": Anne Gebhardt (France), Kai Fechner (Belgium),<br />

Carole Ampe (Belgium), Yannick Devos (Belgium), Jari<br />

H<strong>in</strong>sch Mikkelsen (Belgium), Tore Sveistrup (Norway), Diego<br />

Angelucci (Portugal), Judit Becze-Deák (Switzer<strong>l<strong>and</strong></strong>), Ersébet<br />

Horváth (Hungary) <strong>and</strong> not on the picture : Geertrui Louwagie (Ire<strong>l<strong>and</strong></strong>),<br />

Hans Mestdagh (Belgium)<br />

F<strong>in</strong>ally, the commission raised a number of pedoquestions.<br />

Some examples are :<br />

1) How do you know if a new student has entered <strong>in</strong> The<br />

Corridor Correct answer: Rogers coffee cup has been<br />

cleaned (background <strong>in</strong>formation: Roger’s cup is always<br />

black on the <strong>in</strong>side from years of coffee dr<strong>in</strong>k<strong>in</strong>g).<br />

2) What is the easiest way to catch Roger Correct<br />

answer: You dig a profile <strong>and</strong> he will surely jump <strong>in</strong>to it.<br />

(NO background <strong>in</strong>formation needed).<br />

3) How do you know if an undisturbed sample for soil<br />

micromorphology is sufficiently wrapped up Correct<br />

answer: you can play football with it.<br />

After a short deliberation, the <strong>in</strong>ternational<br />

scientific jury agreed that Roger Langohr may retire with<br />

the degree of summa cum laude as the most sympathetic<br />

promoter, testified <strong>in</strong> the GOLDEN KNIFE diploma he<br />

received. The proclamation was followed by an European<br />

surprise buffet.<br />

After two memorable days <strong>in</strong> the Ardennes, Roger<br />

could return home know<strong>in</strong>g that his presence at the Ghent<br />

University over more than 3 decades meant more than just<br />

scientific supervision. It also created friendships across<br />

<strong>in</strong>ternational borders, valued to such an extent that people<br />

- 27 -


MEETINGS<br />

FUTURE MEETINGS<br />

May 8-11, 2006 : ISPRS Mid-term Symposium 2006 :<br />

"Remote Sens<strong>in</strong>g : From Pixels to Processes", Enschede,<br />

THE NETHERLANDS. Information : website :<br />

http://www.itc.nl/isprsc7/symposium2006/; e-mail :<br />

isprsc7@itc.nl<br />

May 14-19, 2006 : 14th Conference of ISCO of<br />

International Soil Conservation Organisation (ISCO),<br />

Marrakech, MOROCCO. Information : website :<br />

http://www.swcs.org/en/<strong>in</strong>ternational/isco/isco_2006.cfm;<br />

e-mail : isco2006@wanadoo.net.ma<br />

May 18-22, 2006 : 2 nd International Tra<strong>in</strong><strong>in</strong>g Workshop<br />

Towards the Integration of Biosal<strong>in</strong>e Irrigated Agriculture,<br />

Matarey-Cairo, EGYPT. Information : http://www.drcegypt.com;<br />

e-mail : saai54@hotmail.com<br />

May 22-26, 2006 : International Soil Meet<strong>in</strong>g on Soils<br />

Susta<strong>in</strong><strong>in</strong>g Life on Earth (Manag<strong>in</strong>g Soil <strong>and</strong> Technology),<br />

Urfa, TURKEY. Information : website :<br />

http://www.toprak.org.tr; e-mail : <strong>in</strong>fo@toprak.org.tr.<br />

June 3-7, 2006 : 43 rd Annual Meet<strong>in</strong>g of the Clay M<strong>in</strong>erals<br />

Society, Oleron Is<strong>l<strong>and</strong></strong>, FRANCE. Information :<br />

http://www.c2s-organisation.com/gfacms06; e-mail :<br />

sab<strong>in</strong>e.petit@hydrasa.univ-poitiers<br />

June 13-16, 2006 : 5 th European Congress on Regional<br />

Geoscientific Cartography <strong>and</strong> Information Systems,<br />

Barcelona, SPAIN. Information : website :<br />

http://www.icc.es/econgeo2006/home.html; e-mail :<br />

econgeo2006@icc.es<br />

June 19-22, 2006 : 11 th International Conference on<br />

Ground Penetrat<strong>in</strong>g Radar, Columbus, OH, USA.<br />

Information : website : http://gpr.osu.edu/<br />

June 25-30, 2006 : Biogeomon 2006 on Biogechemistry,<br />

ecosystems, isotopen, monitor<strong>in</strong>g, Santa Cruz, CA, USA.<br />

Information : website :<br />

http://www3.villanova.edu/conferences/biogeomon2006<br />

June 26-29, 2006 : BIOCOMP 06 : International<br />

Conference on Bio-Informatics <strong>and</strong> Computational<br />

Biology, Las Vegas, NV, USA. Information : e-mail :<br />

budak@sabanciuniv.edu<br />

June 26-30, 2006 : 5 th International Congress on<br />

Environmental Geotechnics, Cardiff, Wales, UK.<br />

Information : website : http://www.grc.cf.ac.uk/5iceg/<br />

July 1-8, 2006 : IVth International Symposium on<br />

Deteriorated Volcanic Soils, Morelia, MEXICO.<br />

Information : website : http://www.isvo06.org/<br />

July 4-7, 2006 : Second Global Workshop on Digital Soil<br />

Mapp<strong>in</strong>g, Rio De Janeiro, BRAZIL. Information :<br />

website :<br />

http://www.digitalsoilmapp<strong>in</strong>g.org/DSM_2006_Brazil.html<br />

; e-mail : mendonca@cnps.embrapa.br<br />

July 5-7, 2006 : Accuracy 2006, 7 th International<br />

Symposium on Spatial Accuracy Assessment <strong>in</strong> Natural<br />

Resources <strong>and</strong> Environmental Science, Lisbon,<br />

PORTUGAL. Information : website : http://2006.spatialaccuracy.org;<br />

e-mail : mcpereira@igeo.pt<br />

July 9-15, 2006 : 18 th World Congress of Soil Science,<br />

Philadelphia, Pennsylvania, USA. Information : website :<br />

http://www.18wcss.org; e-mail : suttech@soils.org<br />

July 14-21, 2006 : XXVI International<br />

Workshop/Symposium on Rapid Methods <strong>and</strong> Automation<br />

<strong>in</strong> Microbiology, Manhattan, KS, USA. Information :<br />

website :<br />

http://www.dce.ksu.edu/dce/cl/rapidmethods/2006; e-mail :<br />

dfung@ksu.edu<br />

July 16-21, 2006 : Zeolite '06, 7th International<br />

Conference on the Occurrence, Properties, <strong>and</strong> Utilization<br />

of Natural Zeolites, Socorro, NM, USA. Information :<br />

http://www.ees.nmt.edu/Zeolite06<br />

July 22-26, 2006 : SWCS International Conference on<br />

Environmental Management, Colorado, USA. Information<br />

: website :<br />

http://www.SWCS.org/en/SWCS_<strong>in</strong>ternational_conference<br />

s/<br />

July 23-26, 2006 : 8th International Conference on<br />

Precision Agriculture <strong>and</strong> Other Precision Resources<br />

Management, M<strong>in</strong>neapolis, MN, USA. Information :<br />

website : http://www.precision.agri.umn.edu/Conference;<br />

e-mail : conferences3@cce.umn.edu<br />

July 24-26, 2006 : 4 th world Congress of Computers <strong>in</strong><br />

Agriculture, Or<strong>l<strong>and</strong></strong>o, FL, USA, Information :<br />

http://www.wcca2006.org/<strong>in</strong>dex.htm; e-mail :<br />

mcknight@asabe.org.<br />

July 31-August 2, 2006 : Model<strong>in</strong>g Phosphorus Transport<br />

<strong>in</strong> Agroecosystems : Jo<strong>in</strong><strong>in</strong>g Users, Developers, <strong>and</strong><br />

Scientists, Ithaca, NY, USA. Information :<br />

http://www.sera17.ext.vt.edu/P_Model<strong>in</strong>g/; e-mail :<br />

nonelson@ksu.edu<br />

August 4-6, 2006 : International Conference on Physical<br />

Model<strong>in</strong>g <strong>in</strong> Geotechnics, HONGKONG. Information :<br />

website : http://www.icpmg2006.ust.hk; e-mail :<br />

stse@ust.hk<br />

August 7-9, 2006 : International Confrence on the Future<br />

of Agriculture : Science, Stewardship, <strong>and</strong> Susta<strong>in</strong>ability,<br />

Sacramento, CA, USA. Information :<br />

- 28 -


MEETINGS<br />

http://www.dce.ksu.edu/dce/conf/ag&environment/; e-mail<br />

: ellen@ksu.edu<br />

August 28-September 3, 2006 : 17 th Triennial Conference<br />

on International Soil Tillage Research Organisation<br />

(ISTRO), Kiel, GERMANY. Information : website :<br />

http://www.istro.org <strong>and</strong> http://www.soils.unikiel.de/istro.htm;<br />

e-mail : b.vogt@soils.uni-kiel.de<br />

September 3-8, 2006 : IAMG06 –International Congress<br />

for Mathematical Geology "Quantitative Geology from<br />

Multiple Sources", Liège, BELGIUM. Information :<br />

website : http://www.geomac.ulg.ac.be/iamg06; e-mail :<br />

geomac@ulg.ac.be<br />

September 4-7, 2006 : Agroenviron 2006 : 5th<br />

International Symposium on the Agricultural Environment,<br />

Ghent, BELGIUM. Information : website :<br />

http://users.ugent.be/~jvdestee/agroenviron/<strong>in</strong>dex.html; e-<br />

mail : joke.v<strong>and</strong>esteene@UGent.be<br />

September 6-10, 2006 : 10 th International Congress of the<br />

International Association of Eng<strong>in</strong>eer<strong>in</strong>g Geologist <strong>and</strong> the<br />

Environment, Nott<strong>in</strong>gham, UK. Information : website :<br />

http://ww.iaeg2006.com<br />

September 12-15, 2006 : ESSC 2006 International<br />

Conference on "Soil <strong>and</strong> Water Conservation under<br />

Chang<strong>in</strong>g L<strong>and</strong> Use", Lleida, Catalonia, SPAIN.<br />

Information : website :<br />

http://www.udl.es/serveis/sedai/sigtel/ESSC2006.html; e-<br />

mail : fundacio@700.udl.es<br />

September 19-25, 2006 : highLAND2006-Symposium,<br />

Mekelle, ETHIOPIA. Information : website :<br />

http://www.kuleuven.be/lbh; e-mail :<br />

jean.poesen@geo.kuleuven.be,<br />

mekelle.university@ethionet.et,<br />

seppe.deckers@biw.kuleuven.be<br />

September 19-22, 2006 : XX Argent<strong>in</strong>ean Congress of Soil<br />

Science, Salta, ARGENTINA. Information : website :<br />

http://www.suelos.org.ar; e-mail : fgarcia@<strong>in</strong>pofos.org<br />

October 4-6, 2006 : Lysimeter-Workshop,<br />

Neuherberg/München, GERMANY, Information : website<br />

: http://www.gsf.de/lysimeter-workshop; e-mail :<br />

sascha.reth@gsf.de<br />

October 4-6, 2006 : IV International Conference on Soft<br />

Soil Eng<strong>in</strong>eer<strong>in</strong>g, Vancouver, CANADA. Information :<br />

website : http://ravenweb.civil.ualberta.ca/icsse<br />

October 11-13, 2006 : A workshop organized by the Soil<br />

<strong>and</strong> Water Conservation Society on Manag<strong>in</strong>g Agricultural<br />

L<strong>and</strong>scapes for Environmental Quality, West<strong>in</strong> Crown<br />

Center Hotel, Kansas City, Missouri, USA. Information :<br />

http://www.swcs.org/en/swcs_<strong>in</strong>ternational_conferences/m<br />

anag<strong>in</strong>g_agricultural_<strong>l<strong>and</strong></strong>scapes<br />

November 6-11, 2006 : X National <strong>and</strong> II International Soil<br />

Science Congress on Soil : food security <strong>and</strong> poverty, La<br />

Mol<strong>in</strong>a, Lima, PERU. Information : website :<br />

http://www.lamol<strong>in</strong>a.edu.pe/suelos/default2.htm<br />

November 13-15, 2006 : IPI-ISSAS International<br />

Workshop on Soil Potassium <strong>and</strong> K fertilizer Management,<br />

Gu<strong>and</strong>ong Prov<strong>in</strong>ce, Zhuhai City, CHINA. Information :<br />

website : http://www.ipipotash.org; e-mail :<br />

Svetlana.Ivanova@uralkali.com<br />

November 22-25, 2006 : International Symposium on<br />

Balanced Fertilization for Susta<strong>in</strong>ability of Crop,<br />

Ludhiana, INDIA. Information : website :<br />

http://www.ipipotash.org/IPI_India_2006/<strong>in</strong>dex.html; e-<br />

mail : patricia.imas@iclfertilizers.com<br />

January 8-19, 2007 : Intensive Tra<strong>in</strong><strong>in</strong>g Course on Soil<br />

Micromorphology. Micromorfologia de Sòls, Barcelona,<br />

SPAIN. Information : website :<br />

http://www.ub.edu/geologia/english/facultat/map.htm; e-<br />

mail : rosa.poch@macs.udl.es, angelscanals@ub.edu<br />

April 21-23, 2007 : III Asian Confrence on Unsaturated<br />

Soils, Nanj<strong>in</strong>g, CHINA. Information : website :<br />

http://www.geohohai.com/english/unsat.htm.<br />

June 3-8, 2007 : I North American L<strong>and</strong>slide Conference –<br />

L<strong>and</strong>slides <strong>and</strong> Society : Integrated Science, Eng<strong>in</strong>eer<strong>in</strong>g,<br />

Management, <strong>and</strong> Mitigation, Vail, Colorado, USA.<br />

Information : website :<br />

http://www.m<strong>in</strong>es.edu/academic/geolgy/<strong>l<strong>and</strong></strong>slidevail2007/<br />

June 25-28, 2007 : IV International Conference on<br />

Earthquake Geotechnical Eng<strong>in</strong>eer<strong>in</strong>g, Thessaloniki,<br />

GREECE. Information : website : http://4icege.org.<br />

June 25-30, 2007 : 5 th International Congress of the<br />

European Society for Soil Conservation, Palermo, ITALY.<br />

Information : website : http://www.esscpalermocongress.it;<br />

e-mail : congressi@bibatour.it<br />

September 10-13, 2007 : 4 th International Confreences on<br />

Debris-Flow Hazards Mitigation : Mechanics, Prediction<br />

<strong>and</strong> Assessment (DFHM Conference), Chengdu, CHINA.<br />

Information : website : http://4thdfhm.imde.ac.cn<br />

October 21-24, 2007 : 10 th Australia New Zea<strong>l<strong>and</strong></strong><br />

Conference on Geomechanics. Brisbane, AUSTRALIA.<br />

Information : website : http://www.ccm.com.au/anzgeo/<br />

2008 : 20 th International Congress of Irrigation <strong>and</strong><br />

Dra<strong>in</strong>age (ICID), Lahore, PAKISTAN. Information :<br />

website : http://www.icid.org; e-mail :<br />

pakfloodcommission@hotmail.com<br />

April 13-18, 2008 : 5 th International Crop Science<br />

Congress, Jeju, KOREA. Information : website :<br />

http://www.cropscience2008.com<br />

- 29 -


MEETINGS<br />

August 23-31, 2008 : Eurosoil Congress, Vienna,<br />

AUSTRIA. Information : website :<br />

http://www.ecsss.net/events.htm<br />

October 5-9, 2009 : XVII International Conference on Soil<br />

Mechanics <strong>and</strong> Geotechnical Eng<strong>in</strong>eer<strong>in</strong>g, Alex<strong>and</strong>ria,<br />

EGYPT. Information : website : http://www.2009icsmgeegypt.org<br />

2010 : 19 th World Congress of Soil Science, AUSTRALIA<br />

1st announcement, April 2006<br />

Intensive Tra<strong>in</strong><strong>in</strong>g Course on Soil Micromorphology<br />

Micromorfologia de Sòls<br />

(Curs de Postgrau i d‟Extensió Universitària)<br />

Barcelona, 8-19 January 2007<br />

Universitat de Lleida Universitat de Barcelona Universiteit Gent<br />

------------------------------------------------------------------------------------------------------------------------------------------------------<br />

Venue:<br />

Dpt.Cristal·lografia, M<strong>in</strong>eralogia i Dipòsits M<strong>in</strong>erals, Facultat de Geologia<br />

Martí i Franquès s/n , 08028 Barcelona, Catalonia (Spa<strong>in</strong>)<br />

Fax : +34934021340; Phone: + 34934021345<br />

http://www.ub.edu/geologia/english/facultat/map.htm<br />

Organiz<strong>in</strong>g committee<br />

Prof. Dr. Rosa M. Poch UdL (co-director) rosa.poch@macs.udl.es<br />

Prof. Dr. Àngels Canals UB (co-director) angelscanals@ub.edu<br />

Prof. Dr. Georges Stoops UG<br />

Duration<br />

6 credits (60 lecture-hours)<br />

Themes<br />

Pr<strong>in</strong>ciples of m<strong>in</strong>eralogy <strong>and</strong> petrography, optical m<strong>in</strong>eralogy<br />

Submicroscopical <strong>and</strong> special techniques<br />

Mak<strong>in</strong>g th<strong>in</strong> sections<br />

Guidel<strong>in</strong>es for the description of th<strong>in</strong> sections of soils <strong>and</strong> regoliths<br />

Micromorphology of soil materials <strong>and</strong> identification of soil formation processes: carbonate-, gypsum- , <strong>and</strong> salt<br />

affected soils, volcanic soils, clay accumulation, hydromorphic soils, tropical <strong>and</strong> highly weathered soils, glacial <strong>and</strong><br />

periglacial processes.<br />

Micromorphometry <strong>and</strong> image process<strong>in</strong>g.<br />

Applications of micromorphology:<br />

Soil genesis <strong>and</strong> classification<br />

Agronomy: seal<strong>in</strong>g <strong>and</strong> crust<strong>in</strong>g, structure <strong>and</strong> porosity<br />

Archaeology<br />

Geomorphology <strong>and</strong> sedimentology<br />

M<strong>in</strong>eral weather<strong>in</strong>g<br />

Optional weekend excursion: Mediterranean soilscapes, soil genesis, sampl<strong>in</strong>g techniques<br />

Inscription fees<br />

420 €, <strong>in</strong>clud<strong>in</strong>g course material. Accomodation <strong>and</strong> weekend excursion are not <strong>in</strong>cluded.<br />

------------------------------------------------------------------------------------------------------------------------------------------------------------<br />

Ask the organiz<strong>in</strong>g committee for more <strong>in</strong>formation<br />

- 30 -


ADVANCED TRAINING AND RESEARCH OPPORTUNITIES<br />

UN INTERNATIONAL YEAR OF THE<br />

PLANET EARTH<br />

UNESCO is designated to organize activities to be<br />

undertaken dur<strong>in</strong>g the year, <strong>in</strong> collaboration with UNEP<br />

<strong>and</strong> other relevant United Nations bodies, the International<br />

Union of Geological Sciences <strong>and</strong> other Earth sciences<br />

societies <strong>and</strong> groups throughout the world. Member States<br />

are encouraged to use the Year to <strong>in</strong>crease awareness of<br />

the importance of Earth sciences <strong>in</strong> achiev<strong>in</strong>g susta<strong>in</strong>able<br />

development <strong>and</strong> promot<strong>in</strong>g local, national, regional <strong>and</strong><br />

<strong>in</strong>ternational action.<br />

- South America (without preference);<br />

The potential Belgian host units are those which are<br />

<strong>in</strong>volved <strong>in</strong> the research programmes <strong>and</strong> actions of the<br />

Federal Science Policy Office (http://www.belspo.be,<br />

rubriek "FEDRA").<br />

Applications are sent to the Federal Science Policy Office<br />

by the Belgian project leaders. The selection takes place<br />

once a year. Only complete <strong>and</strong> duly signed applications<br />

will be taken <strong>in</strong>to consideration.<br />

Check also l<strong>in</strong>ks at our webpage : http://www.plr.ugent.be<br />

The International Year of Planet Earth aims to demonstrate<br />

the great achievements made <strong>in</strong> the geosciences <strong>and</strong> to urge<br />

politicians <strong>and</strong> decision-makers to apply such knowledge<br />

for the benefit of humank<strong>in</strong>d.<br />

The International Year of Planet Earth is <strong>in</strong> fact the core<br />

year of a triennium, start<strong>in</strong>g <strong>in</strong> 2007 <strong>and</strong> clos<strong>in</strong>g by the end<br />

of 2009.<br />

National implementation of the Year of Planet Earth is<br />

essential for its success. Suggestions for develop<strong>in</strong>g<br />

national committees for the Year of Planet Earth can be<br />

downloaded from the Year's website :<br />

www.yearofplanetearth.org.<br />

Calls are open now for now for submitt<strong>in</strong>g <strong>in</strong>ternational<br />

project proposals on the outreach programme <strong>and</strong> on<br />

selected science themes.<br />

POSTDOC FELLOWSHIPS<br />

TO NON-EU RESEARCHERS<br />

The stimulation of <strong>in</strong>ternational mobility <strong>and</strong> the attraction<br />

of researcher from abroad is one of the priorities of the<br />

European Research Area.<br />

In this context <strong>and</strong> <strong>in</strong>tend<strong>in</strong>g to stimulate the S&T<br />

cooperation, the Federal Science Policy Office does<br />

implement a fellowship scheme for highly qualified<br />

researcher (i.e. postdoctoral level or equivalent experience)<br />

from specific regions, grant<strong>in</strong>g them an opportunity to<br />

work dur<strong>in</strong>g 6 to 12 months <strong>in</strong> a Belgian research team.<br />

- Eastern Europe (non-EU members), Caucasia <strong>and</strong><br />

Central Asia (New Independent States of the Former<br />

Soviet Union);<br />

- The non-European Mediterranean Region : Egypt,<br />

Jordan, Morocco, Tunesia, Turkey;<br />

- Central Africa : Burundi, Congo, Rw<strong>and</strong>a;<br />

- 31 -


INTERNATIONAL CENTRE FOR PHYSICAL LAND RESOURCES<br />

Ghent University<br />

Krijgslaan 281/S8<br />

B-9000 Gent<br />

Tel. : +32-9/2644618<br />

Fax : +32-9/2644991<br />

E-mail : PLRprog.adm@UGent.be<br />

Website : http://www.plr.ugent.be

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!