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Manal A. Alnaimy, Ahmed S. Elrys, Martina Zelenakova, Katarzyna Pietrucha-Urbanik and Abdel-Rahman M. Merwad
Despite studies focusing on soil substrates (carbon and nitrogen) and heavy metal availability, the impact of diversified parent materials in arid alkaline regions has received little attention. To reveal the influence of parent material, we investigated...
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Evgeny Abakumov
Rendzinas in the taiga zone are intrazonal soils; moreover, all of their processes occur in ways that are different from podzolic soil formation, which is typical for the zonal taiga boreal ecosystem. At the same time, the habitats of carbonate soils are...
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Alessandra Musso, Dmitry Tikhomirov, Michael L. Plötze, Konrad Greinwald, Anne Hartmann, Clemens Geitner, Fabian Maier, Fanny Petibon and Markus Egli
Soil development and erosion are important and opposing processes in the evolution of high-mountainous landscapes, though their dynamics are not fully understood. We compared soil development between a calcareous and a siliceous chronosequence in the cen...
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Annamária Laborczi, Csaba Bozán, János Körösparti, Gábor Szatmári, Balázs Kajári, Norbert Túri, György Kerezsi and László Pásztor
Inland excess water is temporary water inundation that occurs in flat-lands due to both precipitation and groundwater emerging on the surface as substantial sources. Inland excess water is an interrelated natural and human induced land degradation phenom...
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Fang Yu, Boris Faybishenko, Allen Hunt, Behzad Ghanbarian
Pág. 1 - 13
Soil depth tends to vary from a few centimeters to several meters, depending on many natural and environmental factors. We hypothesize that the cumulative effect of these factors on soil depth, which is chiefly dependent on the process of biogeochemical ...
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Chaplot, V. Van Vliet-Lanoe, B. Walter, C. Curmi, P. Cooper, M.
Pág. 856 - 868
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