It is established by the author's research that in the Selenga River delta the layered-alluvial humic soils of the soil formation primary trunk were formed at the pulsing mode of the floodplain conditions as a result of the climatic condition cyclic changes in the region. The morphogenetic and physical-chemical properties of the studied soils are considered.
delta Selenga, soils, morphology, properties, climate cyclicity
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