Summary
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1.
During roadway drivage in the permafrost zone, the yield of fine dust fractions increases with falling temperature and we therefore observe an increase in the dust-formation intensity.
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2.
The increase in dust-formation intensity is due to a change in the frozen rock's physicomechanical properties (hardness, brittleness, viscosity and moisture content).
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3.
The authors' empirical equations can be used for forecasting the dust-formation intensity during mining of different zones and horizons with different geocryological conditins, so as to calculate the optimal ventilation conditions.
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Literature Cited
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V. N. Vorotin, L. D. Voronina, and A. D. Bagrinovskii, Handbook of the Planning and Practice of Dust Suppression in Metal Mines [in Russian], Moscow, Gosgortekhizdat (1961).
Z. A. Narsesova, Phase Composition of Ground Water during Freezing and Thawing, Laboratory Research on Frozen Soils, No. 1 [in Russian], Moscow, Izd. AN SSSR (1953).
L. S. Burshtein and L. N. Kurochkin, Study of the Physico-mechanical properties of frozen bedrock. In Symposium: “Thermal and Mechanical Processes in the Mining of Minerals in Rocks” [in Russian], Moscow, “Nauka” (1965).
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Additional information
ZabNII, Chita. Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 4, pp. 121–125, July–August, 1967.
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D'yakov, V.V., Voronov, E.T. Intensity of dust formation under permafrost conditions. Soviet Mining Science 3, 414–417 (1967). https://doi.org/10.1007/BF02497568
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DOI: https://doi.org/10.1007/BF02497568