Zobrazeno 1 - 10
of 65
pro vyhledávání: '"kleimineralen"'
Publikováno v:
International journal of earth sciences, 89(1), 154-169. Springer
International Journal of Earth Science 89 (2000)
International Journal of Earth Science, 89, 154-169
International Journal of Earth Science 89 (2000)
International Journal of Earth Science, 89, 154-169
At the Pliocene-Pleistocene transition, major changes occurred in the Rhine system: Climatic cooling, extension of the drainage area into the Alps and a marine regression. We studied the geochemistry, clay mineralogy and micromorphology of several se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::198b4a5dabf58cbcd20ea4413f29d722
https://doi.org/10.1007/s005310050323
https://doi.org/10.1007/s005310050323
Publikováno v:
Geoderma 98 (2000)
Geoderma, 98, 61-82
Geoderma, 98, 61-82
We studied a chronosequence of three soils developed on andesitic lavas in humid tropical Costa Rica, in order to investigate mineralogical development and to evaluate the importance of time versus other soil forming factors. Morphological, chemical,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9d01e8818bb65d43a685b9326199ac92
https://doi.org/10.1016/s0016-7061(00)00052-5
https://doi.org/10.1016/s0016-7061(00)00052-5
Publikováno v:
Soil Science Society of America Journal
Soil Science Society of America Journal, Soil Science Society of America, 1994, 58 (2), pp.494-502
Soil Science Society of America Journal 58 (1994)
Soil Science Society of America Journal, 58, 494-501
Soil Science Society of America Journal, Soil Science Society of America, 1994, 58 (2), pp.494-502
Soil Science Society of America Journal 58 (1994)
Soil Science Society of America Journal, 58, 494-501
The occurrence of 2:1 phyllosilicates in Andisols is variously ascribed to in situ pedogenic origin, aeolian addition, or the presence of hydrothermally altered rock fragments. We studied the origin of 2:1 phyllosilicates that occur in Holocene Haplu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::760fd51056dbcef9da89d04675812983
https://doi.org/10.2136/sssaj1994.03615995005800020035x
https://doi.org/10.2136/sssaj1994.03615995005800020035x
Publikováno v:
Gea : driemaandelijks tijdschrift van de Stichting Geologische Aktiviteiten voor Belangstellenden in de Geologie en Mineralogie. 27(3):77-83
In de mineralogie kent men een aantal aandachtsgebieden, zoals de ertsmineralogie, de mineralogie van metamorfe gesteenten, de kleimineralogie en de bodemmineralogie. De mineralogie van de oppervlaktegesteenten, oppervlaktedelfstoffen en bodems noemt
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dris___00893::b51f4f20f17b94dc6852a1e88f6d201b
Publikováno v:
Soil Science Society of America Journal. 58:494-501
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dris___00893::23340fa0132b899e6a0f5cb77ed73e16
Autor:
Hiemstra, T.
cum laude graduation (with distinction) Het in dit proefschrift ontwikkelde algemene raamwerk voor oppervlaktelading en ion adsorptie kan worden toegepast in wetenschap, technologie, en milieu. In het laatste deel van het proefschrift wordt aandacht
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::97bdcacb861f18e71cb10f3ea1382c6b
https://research.wur.nl/en/publications/surface-complexation-at-mineral-interfaces-multisite-and-charge-d
https://research.wur.nl/en/publications/surface-complexation-at-mineral-interfaces-multisite-and-charge-d
cum laude graduation (with distinction)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dris___00893::813ddcf8c79fb2b18833051fc144ea61
Autor:
Luykx, D.M.A.M., van Doesburg, J.D.J., Giesbers, M., Pinckaers, V.G.Z., van Raamsdonk, L.W.D., Immerzeel, J., Hoogenboom, L.A.P.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ce7c05d924594b0cfd15b81d4a72efef
https://research.wur.nl/en/publications/identificatie-van-kleimineralen
https://research.wur.nl/en/publications/identificatie-van-kleimineralen
The primary source of soil organic matter is plant debris of all kinds, such as dead roots, leaves and branches that enter into the soil and are then biologically decomposed at variable rates. Organic matter has many different important functions on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dris___00893::26de1563a64a57687caab3fe5ec89475