Self-similar solution of the thawing soil problem (Q1123778)
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scientific article; zbMATH DE number 4110392
| Language | Label | Description | Also known as |
|---|---|---|---|
| English | Self-similar solution of the thawing soil problem |
scientific article; zbMATH DE number 4110392 |
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Self-similar solution of the thawing soil problem (English)
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1988
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A mathematical model of phase transitions in frozen soils containing unfrozen water is proposed. It is shown that phase transitions in frozen soils always occupy an extended zone. The problem of the interaction of frozen rock with a salt solution is solved on the assumption that the interface between the solution and the frozen rock is permeable both for the liquid and for the dissolved impurity.
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phase transitions
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frozen soils
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unfrozen water
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salt solution
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