Abstract
A technique is presented for determining the thermo-gradient coefficient of moist rocks by the method of graphic differentiation. The thermogradient and temperature coefficients of the rocks of the Tkibuli-Shaori deposits have been determined. These coefficients are shown to vary depending on the natural temperature and moisture content of the rocks.
References
А. В. Лыков. Тепломассообмен. М., 1978.
Ш. И. О н и а н и, Ю. Р. К с о в р е л и. Сб. «Труды Международного симпозиума*.
Катовице, 1980.
This work is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License.
Copyright (c) 2021 Sh. I. Oniani, O. A. Lanchava, I. R. Ksovreli
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