Abstract
Since the regularities of phase transformation, in particular, liquid and vaporous moisture in the “soil–air–water body” system are poorly elucidated, we tried to solve this challenge taking into account the given initial prerequisites and assumptions. The patterns of evaporation (condensation) from the surface of homogenous fresh and saline water bodies and heterogeneous porousfissured soils saturated-unsaturated by underground liquid solution as well as the features of equiphase moisture transfer in unsaturated soils and phase transition in air are considered.
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