Evolution of the soil profile as factor and effect biological evolution
Abstract
Defined especially the transformation of the soil profile over time according to changes in ecological community of the region and the mechanism of reverse protsesa, the presence of dominant dynamic elementary and general pochvoformiruyuschih processes, namely humus accumulation, carbonation, decomposition and leaching of MgO, Al2O3 and Fe2O3, SiO2 accumulation and CaO. You can distinguish the main evolutionary trend - Climatogenic steppe formation: the offensive zone on the steppe steppe.
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