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About the Genesis of Soil Salinity in the Western Part of the Transbaikal Region

机译:关于跨贝加尔湖地区西部土壤盐分的成因

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摘要

Salt-affected soils in the Transbaikal region are mainly represented by hydromorphic and semihydromorphic soil groups.Automorphic salt-affected soils are less frequent and do not occupy considerable areas.Salt-affected soils are confined to steppe and dry steppe ecosystems that occupy intermontane depressions.The geography and genesis of salt-affected soils in the westrn part of theTransbaikal region are discussed.It is argued that soil salinization is favored by the cryoarid climate in combination with the presence of permafrost,uneven surface topography,and the impact of saline ground water on the soil profile.
机译:跨贝加尔湖地区的盐渍土主要表现为水溶和半水溶土类群,自体盐渍土较少见且不占较大面积,盐渍土仅限于草原和干旱草原生态系统,这些生态系统位于山间洼地。讨论了特贝加尔河地区西部受盐分影响的土壤的地理和成因。研究认为,冻土气候,多年冻土,不平坦的地势和盐水对地下水的影响,有利于土壤盐碱化。在土壤剖面上。

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