Abstract
Western Siberia is an important base for oil and gas production. The main number of deposits are arranged on bulk soils that violate the thermal regime of rocks and cause the development of a variety of engineering and geological processes and phenomena. The paper presents the results of determining the thermophysical characteristics of bulk soils selected at four fields in Western Siberia. Thermotechnical calculations were carried out to determine the depth of seasonal thawing and an assessment was made of the influence of the thermophysical properties of bulk soils on the change in thickness of the seasonally thawed layer.
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