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Mathematical modeling of heat and moisture transfer in the seasonal thawing of frozen soils

✍ Scribed by P. P. Permyakov; P. G. Romanov; A. V. Stepanov

Publisher
Springer US
Year
1989
Tongue
English
Weight
301 KB
Volume
57
Category
Article
ISSN
1573-871X

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## Abstract Mongolia has an arid and cold climate due to its geographical settings of inland and mid‐latitude highlands. The soil moisture varies seasonally, depending mainly on the balance of precipitation and evapotranspiration as well as on winter soil‐freezing and spring snowmelt. Soil moisture