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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 />
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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 />
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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 />
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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 />
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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 />
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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 />
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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 />
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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 />
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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