Zobrazeno 1 - 10
of 278
pro vyhledávání: '"N. van Breemen"'
Autor:
E. Buis, Jeroen M. Schoorl, Bertrand Boeken, N. van Breemen, A. Veldkamp, Arnaud Temme, A.G. Jongmans
Publikováno v:
Geoderma 156 (2010) 3-4
Geoderma, 156(3-4), 363-371
Geoderma, 156(3-4), 363-371
In semi-arid areas vegetation is scarce and often dominated by individual shrubs on raised mounds. The processes of formation of these mounds are diverse and still debated. Often, shrub mound formation is directly related to the formation of vegetati
Autor:
N. van Breemen
Publikováno v:
Acid Sulfate Weathering
Acid sulfate weathering: proceedings of a symposium sponsored by the divisions S-9, S-2, S-5, and S-6 of the Soil Science Society of America in Fort Collins, Colorado, 5-10 Aug. 1979
Acid sulfate weathering: proceedings of a symposium sponsored by the divisions S-9, S-2, S-5, and S-6 of the Soil Science Society of America in Fort Collins, Colorado, 5-10 Aug. 1979. Wiley
Acid sulfate weathering: proceedings of a symposium sponsored by the divisions S-9, S-2, S-5, and S-6 of the Soil Science Society of America in Fort Collins, Colorado, 5-10 Aug. 1979
Acid sulfate weathering: proceedings of a symposium sponsored by the divisions S-9, S-2, S-5, and S-6 of the Soil Science Society of America in Fort Collins, Colorado, 5-10 Aug. 1979. Wiley
Acid sulfate soils form when potentially acid pyritic marshes are drained and tidal influence decreases, either naturally or by man. During oxidation of pyrite to ferrous sulfate, ferric oxide, or jarosite and sulfuric acid, the supply of O2 is ratel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e019e124da6662fc2a9f1dd26bafe9a8
https://doi.org/10.2136/sssaspecpub10.c6
https://doi.org/10.2136/sssaspecpub10.c6
Publikováno v:
Pulleman, M M; Six, J; van Breemen, N; & Jongmans, A G. (2005). Soil organic matter distribution and microaggregate characteristics as affected by agricultural management and earthworm activity. European Journal of Soil Science, 56(4), 453-467. UC Davis: Retrieved from: http://www.escholarship.org/uc/item/3j90p3jk
European Journal of Soil Science 56 (2005) 4
European Journal of Soil Science, 56(4), 453-467
European Journal of Soil Science 56 (2005) 4
European Journal of Soil Science, 56(4), 453-467
Stable microaggregates can physically protect occluded soil organic matter (SOM) against decomposition. We studied the effects of agricultural management on the amount and characteristics of microaggregates and on SOM distribution in a marine loam so
Publikováno v:
Biogeochemistry. 62:253-275
Soil weathering can be an important mechanism to neutralize acidity in forest soils. Tree spe- cies may differ in their effect on or response to soil weathering. We used soil mineral data and the natu- ral strontium isotope ratio 87 Sr/ 86 Sr as a tr
Autor:
Hans Kros, Albert Tietema, H. Oene, R. van Veeren, P. Hofschreuder, J.J.M. de Klein, D. van Dam, N. van Breemen, Rien Aerts, Oene Oenema, Marcel R. Hoosbeek, Carolien Kroeze, W. de Vries
Publikováno v:
Nutrient Cycling in Agroecosystems. 66:43-69
This study focuses on the uncertainties in the ‘fate’ of nitrogen (N) in the Netherlands. Nitrogen inputs into the Netherlands in products, by rivers, and by atmospheric deposition, and microbial and industrial fixation of atmospheric N2 amount t
Autor:
T. M. Corton, Reiner Wassmann, R. S. Lantin, H. H. van Laar, Martin J. Kropff, H. A. C. Denier van der Gon, N. van Breemen, E. Aduna
Publikováno v:
Proceedings of the National Academy of Sciences of the United States of America 99 (2002) 19
Proceedings of the National Academy of Sciences of the United States of America, 99(19), 12021-12024
Proceedings of the National Academy of Sciences of the United States of America, 99(19), 12021-12024
Microbial production in anoxic wetland rice soils is a major source of atmospheric CH 4, the most important non-CO 2 greenhouse gas. Much higher CH 4 emissions from well managed irrigated rice fields in the wet than in the dry season could not be exp
Autor:
Christine L. Goodale, Keith Paustian, Kate Lajtha, Sybil P. Seitzinger, Elizabeth W. Boyer, Marlen Eve, N. van Breemen, Bernd Mayer Mayer, Gilles Billen, Norbert A. Jaworski, Robert W. Howarth, D. van Dam, Knute J. Nadelhoffer
Publikováno v:
Biogeochemistry. 57:267-293
To assess the fate of the large amounts of nitrogen (N) brought into the environment by human activities, we constructed N budgets for sixteen large watersheds (475 to 70,189 km 2 ) in the northeastern U.S.A. These watersheds are mainly forested (48-
Autor:
N. van Breemen, P.S.J. Verburg
Publikováno v:
Forest Ecology and Management, 129, 31-39
Forest Ecology and Management 129 (2000)
Forest Ecology and Management 129 (2000)
Model predictions on the response of soil processes to global warming are mostly inferred from small-scale laboratory studies. In this study, a forested catchment in southern Norway was enclosed by a greenhouse and experimentally manipulated by incre
Autor:
Erik Karltun, Lars Nyberg, N. van Breemen, A. Nordgren, L. Tau Strand, Hannu Mannerkoski, O. Wahlberg, Roger D. Finlay, Gunnhild Riise, Tommy Magnusson, A.G. Jongmans, Kevin Bishop, Ulla S. Lundström, Jon Petter Gustafsson, Reiner Giesler, Hannu Ilvesniemi, P.A.W. van Hees, A. Bergelin, Mats Olsson, Mike Starr, P.-A. Melkerud, D. C. Bain
Publikováno v:
Geoderma 94 (2000)
Geoderma, 94, 335-353
Geoderma, 94, 335-353
Advances in understanding the podzolisation process resulting from a multidisciplinary study at three coniferous forest soils in the Nordic countries
Publikováno v:
Geoderma, 94, 91-107
Geoderma 94 (2000)
Geoderma 94 (2000)
This paper reviews the major mechanisms proposed to explain podzolization. These include the production of organic acids that form soluble complexes with aluminium/iron thereby enhancing weathering, followed by illuviation by precipitation/adsorption