Temperature deformations of frozen soils caused by rapid changes in temperature


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Abstract

The results of the study of the temperature deformations for different types of frozen soils due to rapid temperature variations in cooling–heating cycles have been described. The difference in the patterns of the temperature deformation for step-like and single variations of temperature has been established. The dependence of the temperature deformation of frozen soil on the soil type, the total moisture, and the number of the cooling–heating cycles has been studied.

About the authors

S. S. Volokhov

Department of Geology

Author for correspondence.
Email: volokhov@geol.msu.ru
Russian Federation, Moscow, 119991

I. N. Nikitin

Department of Geology

Email: volokhov@geol.msu.ru
Russian Federation, Moscow, 119991

D. S. Lavrov

LLC GeoProject Survey

Email: volokhov@geol.msu.ru
Russian Federation, Moscow, 111024

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