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• W25647785 abstract "Abstract The genesis of soils has been seen mostly as an autochthonistic process, that is, formation in situ . However, soil geomorphologists have recognized addition and loss of materials, for example, through eolian and colluvial processes, as a major contribution to allochthonistic soil formation. The most important characteristic of these soils is the lithological discontinuity, which separates the lower residual material from the upper allochthonic soil. The chapter deals with (1) developing a model joining the ideas of in situ formation and near-surface processes such as adding or removing material, (2) the pedogenetic processes in soils with lithological discontinuities, and (3) the effect of lithological discontinuities on physical and chemical properties of soils." @default.
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• W25647785 date "2013-01-01" @default.
• W25647785 modified "2023-09-24" @default.
• W25647785 title "Influence of Cover Beds on Soils" @default.
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• W25647785 doi "https://doi.org/10.1016/b978-0-444-53118-6.00003-9" @default.
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