Abstract
A method of evaluating the stress-strain state of frozen soils, which takes into account the existence of elastoviscoplastic and temperature deformations over time under variable external effects, is described.
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References
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Additional information
Translated from Osnovaniya, Fundamenty i Mekhanika Gruntov, No. 4, pp. 10–13, July–August, 1997.
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Gerasimov, A.S. Thermorheological model of a frozen-soil continuum. Soil Mech Found Eng 34, 110–115 (1997). https://doi.org/10.1007/BF02465942
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DOI: https://doi.org/10.1007/BF02465942