Staff Publications

Staff Publications

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    'Staff publications' is the digital repository of Wageningen University & Research

    'Staff publications' contains references to publications authored by Wageningen University staff from 1976 onward.

    Publications authored by the staff of the Research Institutes are available from 1995 onwards.

    Full text documents are added when available. The database is updated daily and currently holds about 240,000 items, of which 72,000 in open access.

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    Microscopisch onderzoek van glauconiethoudende zanden bij Ellewoutsdijk - Borssele in de provincie Zeeland
    Schoute, J.F.T. ; Bisdom, E.B.A. ; Schoonderbeek, D. - \ 1992
    Wageningen : DLO-Staring Centrum (Rapport / DLO-Staring Centrum 233) - 41
    constructie - funderingen - pedologie - grondmechanica - bodemmicromorfologie - tunnels - nederland - zeeland - zeeuwse eilanden - construction - foundations - pedology - soil mechanics - soil micromorphology - tunnels - netherlands - zeeland - zeeuwse eilanden
    Surface sealing and hydraulic conductances under varying-intensity rains
    Giménez, D. ; Dirksen, C. ; Miedema, R. ; Eppink, L.A.A.J. ; Schoonderbeek, D. - \ 1992
    Soil Science Society of America Journal 56 (1992)1. - ISSN 0361-5995 - p. 234 - 242.
    crusts - hydraulic conductivity - infiltration - pedology - rain - relationships - runoff - seepage - simulation - soil - soil micromorphology - korsten - hydraulisch geleidingsvermogen - infiltratie - pedologie - regen - relaties - oppervlakkige afvoer - kwel - simulatie - bodem - bodemmicromorfologie
    In the past, investigations on surface seals developing under simulated rains usually were performed with uniform rainfall intensities. Recent studies, however, showed that varying-intensity rains affect erosion and volumes of runoff. We conducted a study on surface sealing under varying-intensity rains using physical and morphological methods. Four 1-h-duration rainfall patterns were used: S1, S2, S3 and S4, with mean rainfall intensities of 83, 69, 65, and 51 mm h-1, respectively, and highest intensities of 148, 120, 111, and 100 mm h-1, respectively. Two experiments were performed in triplicate: (i) in packed soil columns, pressure heads at 1-cm depth were measured, and runoff (Rt) and wash sediment (St) collected at short time intervals during S1, S3, and S4 patterns; and (ii) packed shallow soil flumes were successively exposed to 10, 15, 30, 40, and 60 min of S2 and S4 patterns, and the surface was then characterized by micromorphological analysis of thin sections (S2) and top-view photographs (S2 and S4). The largest differences between rainfall patterns occurred during the intensity peaks (10–30 min): at the end of these periods, measured surface seal hydraulic conductances (β) attained values of 0.80, 0.25, and 0.51 h-1 for S1, S3, and S4, respectively. These relative β values are thought to be due to partially open surfaces as a result of microrill erosion (S1), complete sealing without erosion (S3), and incomplete sealing (S4). Presented Rt, St, and morphological data support these conclusions. After 5 min of the intensity peaks of S2, surface seals attained maximum observed thickness and minimum macroporosity (>30 µm). Planar voids (>500 µm) were eliminated at this point. Under continuing rain, erosion reduced the seal thickness and increased macroporosity, mainly as planar voids
    Root-soil contact of maize, as measured by a thin-section technique. 2. Effects of soil compaction.
    Kooistra, M.J. ; Schoonderbeek, D. ; Boone, F.R. ; Veen, B.W. ; Noordwijk, M. van - \ 1992
    Plant and Soil 139 (1992). - ISSN 0032-079X - p. 119 - 129.
    maize - pedology - plant development - plant physiology - pore volume - porosity - roots - soil compaction - soil density - soil micromorphology - zea mays
    Root-soil contact of maize, as measured by a thin-section technique. 1. Validity of the method
    Noordwijk, M. van; Kooistra, M.J. ; Boone, F.R. ; Veen, B.W. ; Schoonderbeek, D. - \ 1992
    Plant and Soil 139 (1992). - ISSN 0032-079X - p. 109 - 118.
    maize - pedology - plant development - plant physiology - roots - soil micromorphology - soil structure - zea mays
    A method to construct artificial soil cores from field soil with a reproducible structure.
    Didden, W.A.M. ; Marinissen, J.C.Y. ; Kroesbergen, B. - \ 1991
    Agriculture, Ecosystems and Environment 34 (1991). - ISSN 0167-8809 - p. 329 - 333.
    pedologie - poriënvolume - porositeit - bodembiologie - bodemdichtheid - bodemmicromorfologie - pedology - pore volume - porosity - soil biology - soil density - soil micromorphology
    Soil formation in a Quaternary terrace sequence of the Allier, Limange, France. Macro- and micromorphology, particle size distribution, chemistry.
    Jongmans, A.G. ; Feijtel, T.C.J. ; Miedema, R. ; Breemen, N. van; Veldkamp, A. - \ 1991
    Geoderma 49 (1991). - ISSN 0016-7061 - p. 215 - 239.
    frankrijk - pedologie - bodemvorming - bodemmicromorfologie - france - pedology - soil formation - soil micromorphology
    Structuurveranderingen door toevoeging van kleimineralen aan lemig zand
    Schoonderbeek, D. ; Schoute, J.F.T. - \ 1990
    Wageningen : Staring Centrum (Rapport / Staring Centrum 120) - 23
    keileemgronden - kleimineralen - verbetering - leemgronden - pedologie - zand - bodembacteriën - bodemverbeteraars - bodemmicromorfologie - bodemstructuur - boulder clay soils - clay minerals - improvement - loam soils - pedology - sand - soil bacteria - soil conditioners - soil micromorphology - soil structure
    Trachytic pumice weathering, Massif Central, France: geochemistry and micromorphology.
    Veldkamp, A. ; Jongmans, A.G. - \ 1990
    Chemical Geology 84 (1990)1/4. - ISSN 0009-2541 - p. 145 - 147.
    andepts - andosols - basalt - klimaat - overstromingen - frankrijk - landschap - natuurlijke hulpbronnen - pedologie - bodemvorming - bodemmicromorfologie - vulkanische lava - vulkanische gesteenten - vulkanische gronden - verwering - andepts - andosols - basalt - climate - floods - france - landscape - natural resources - pedology - soil formation - soil micromorphology - volcanic lava - volcanic rocks - volcanic soils - weathering
    Micromorphology and mineralogy of weathering and neoformation phenomena in a quaternary terrace sequence of the Allier, Limagne, France.
    Jongmans, A.G. ; Doesburg, J.D.J. van; Breemen, N. van - \ 1990
    Chemical Geology 84 (1990)1/4. - ISSN 0009-2541 - p. 83 - 85.
    andepts - andosols - frankrijk - pedologie - bodemmicromorfologie - vulkanische gronden - andepts - andosols - france - pedology - soil micromorphology - volcanic soils
    Geochemical and mineralogical discontinuities in a stone-line containing soil profile in Araracuara, Colomian amazones.
    Moura, M.L. ; Kroonenberg, S.B. - \ 1989
    In: Stone - lines : journee d'etude, Bruxelles, 24 mars 1987 = Stone - lines : studiedag, Brussel, 24 maart 1987 / Alexandre, J., Symoens, J.J., - p. 93 - 95.
    colombia - erosie - geologie - pedologie - bodemmicromorfologie - verwering - colombia - erosion - geology - pedology - soil micromorphology - weathering
    Identification of clay coatings in an older Quaternary Terrace of the Allier, Limagne, France.
    Feijtel, T.C.J. ; Jongmans, A.G. ; Doesburg, J.D.J. van - \ 1989
    Soil Science Society of America Journal 53 (1989). - ISSN 0361-5995 - p. 876 - 882.
    andepts - andosols - frankrijk - pedologie - bodemmicromorfologie - vulkanische gronden - andepts - andosols - france - pedology - soil micromorphology - volcanic soils
    Micromorfologisch en bodemfysisch onderzoek in het kader van de vergelijkende analyse van het functioneren van ecosystemen bij een vorm van "gangbare" en "geintegreerde" akkerbouw op de Dr. H.J. Lovink-hoeve (N.O.P.) : een tussentijds verslag
    Vos, E.C. ; Kooistra, M.J. - \ 1988
    Wageningen : STIBOKA (Rapport / Stichting voor Bodemkartering nr. 2054) - 55
    alternatieve landbouw - horizonten - hydraulisch geleidingsvermogen - infiltratie - landevaluatie - biologische landbouw - pedologie - zaaibedbereiding - kwel - bodemdegradatie - bodemmicromorfologie - bodemstructuur - bodemgeschiktheid - bodemkarteringen - grondbewerking - nederland - flevoland - noordoostpolder - alternative farming - horizons - hydraulic conductivity - infiltration - land evaluation - organic farming - pedology - seedbed preparation - seepage - soil degradation - soil micromorphology - soil structure - soil suitability - soil surveys - tillage - netherlands - flevoland - noordoostpolder
    Toepassing van een internationaal micromorfologisch beschrijvingssysteem op tien grote slijpplaten van kleimonsters uit Nederland en Belgie
    Bisdom, E.B.A. - \ 1987
    Wageningen : STIBOKA (Rapport / Stichting voor Bodemkartering nr. 1850) - 56
    zware kleigronden - monolietpreparatie - pedologie - bodemmicromorfologie - slijpplaatje preparatie - clay soils - monolith preparation - pedology - soil micromorphology - thin section preparation
    Kleimineralogisch onderzoek van enkele kwartaire en tertiaire afzettingen
    Breeuwsma, A. ; Balkema, W. ; Zwijnen, R. - \ 1987
    Wageningen : STIBOKA (Rapport / Stichting voor Bodemkartering no. 1980) - 21
    zware kleigronden - monolietpreparatie - pedologie - bodemmicromorfologie - slijpplaatje preparatie - clay soils - monolith preparation - pedology - soil micromorphology - thin section preparation
    Micromorfologische publikaties verzameld door Dr. Ir. A. Jongerius = Micromorphological publications collected by Dr. Ir. A. Jongerius
    Yegeren, J.G.C. van; Schoonderbeek, D. ; Naber, G. ; Jongerius, A. - \ 1987
    Wageningen : STIBOKA (Rapport / Stichting voor Bodemkartering nr. 1982) - ISBN 9789032702250
    bibliografieën - nederland - pedologie - bodemmicromorfologie - bibliographies - netherlands - pedology - soil micromorphology
    Micromorphology, pedogenesis and soil classification in a catena of soils in Chuka, Kenya
    Manzanares, P. - \ 1987
    Wageningen : Landbouwuniversiteit Wageningen - 92
    kenya - pedologie - bodemmicromorfologie - bodemkarteringen - kenya - pedology - soil micromorphology - soil surveys
    Soil morphology and soil water movement.
    Bouma, J. ; Kooistra, M.J. - \ 1987
    In: Soil Micromorphology: Proceedings of the Seventh International Working-Meeting on Soil Micromorphology, Paris, 1985 - p. 507 - 511.
    pedologie - bodemmicromorfologie - infiltratie - hydraulisch geleidingsvermogen - kwel - bodem - scheurvorming - opzwellen - krimp - pedology - soil micromorphology - infiltration - hydraulic conductivity - seepage - soil - cracking - swelling - shrinkage
    Soil formation, microstructure and physical behaviour of Late Weichselian and Holocene Rhine deposits in the Netherlands
    Miedema, R. - \ 1987
    Agricultural University. Promotor(en): L.J. Pons, co-promotor(en): F.F.R. Koenigs. - S.l. : S.n. - 339
    kleimineralen - zware kleigronden - klimaat - overstromingen - geologie - landschap - nederland - pedologie - rivieren - sediment - bodemvorming - bodemmicromorfologie - verwering - glaciale perioden - holoceen - postglaciale perioden - kwartair - rijn - clay minerals - clay soils - climate - floods - geology - landscape - netherlands - pedology - rivers - sediment - soil formation - soil micromorphology - weathering - glacial periods - holocene - postglacial periods - quaternary - river rhine

    Dutch Late Weichselian braided river deposits and Holocene meandering river deposits of the Rhine have been studied and compared. Cross sections demonstrate the lateral and vertical variations of the Late Weichselian sediments. Soil mapping of these deposits, even on a very detailed scale, proves very difficult. Best results have been obtained with a legend based on hydrology enabling the distinction of topo-hydrosequences of well drained brown soils, imperfectly drained mottled soils and poorly drained grey soils.

    Advanced soil formation and notably the dramatic processes in the Late Weichselian period (decalcification, clay illuviation, pseudogleying, periglacial formation of a highly reoriented, very dense microstructure) have caused clay mineralogical, chemical and physical changes in the Late Weichselian soils.

    The well drained and imperfectly drained Late Weichselian soils have an argillic horizon (Alfisols, Luvisols), occasionally with very low base saturation (Ultisols, Acrisols) and with strong subsequent pseudogleying in the imperfectly drained soils. The Holocene soils demonstrate decalcification and biogenic homogenization as well as some gleying according to their drainage position. These soils are classified as Inceptisols (Cambisols), occasionally as Mollisols (Phaeozems).

    Less favourable physical characteristics and behaviour (soil strength, structure stability and tillage behaviour) of the Late Weichselian soils and soil material is quantitatively documented. Differences with the Holocene soils and soil material are statistically highly significant and are caused by differences in texture, content, quality and distribution of organic matter and the highly reoriented, very dense microstructure.

    Use as permanent grassland or ley in the crop rotation is recommended to increase levels of biological activity. This seems the only remedy for the imperfectly and poorly drained Late Weichselian soils that are compacted by natural soil forming processes not counteracted by biological activity. Very recently improved drainage of large areas of Late Weichselian imperfectly drained soils has increased the saturated hydraulic conductivity to noncritical levels through increased earthworm activity to some metres depth.

    Lichtmicroscopie, beeldanalyse en elektronenmicroscopie van met zware metalen verontreinigde grondmonsters uit kolomproeven
    Bisdom, E.B.A. - \ 1986
    Wageningen : STIBOKA (Rapport / Stichting voor Bodemkartering no. 1959) - 46
    zware metalen - uitspoelen - pedologie - bodem - bodemmicromorfologie - heavy metals - leaching - pedology - soil - soil micromorphology
    Handbook for soil thin section description
    Bullock, P. ; Fedoroff, N. ; Jongerius, A. - \ 1985
    Albrighton : Waine - ISBN 9780905184098 - 152
    pedologie - bodemmicromorfologie - slijpplaatje preparatie - monolietpreparatie - handboeken - pedology - soil micromorphology - thin section preparation - monolith preparation - handbooks
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