Summary
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1.
A calorimetric method can, in principle, be used to determine a physical constant of the rock—its specific surface energy of fragmentation.
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2.
Since the specific surface energy of fragmentation of a rock should not depend on the method of fragmentation, its value, found by the calorimetric method, can serve as the principal physical index of the rock's resistance to mechanical fragmentation.
Literature Cited
L. I. Baron, Yu. G. Konyashin, and Z. M. Kurbatov, The Crushabilities of Rocks [in Russian], Moscow, Izd. An SSSR (1963).
L. I. Baron, B. M. Loguntsov, and E. Z. Pozin, Determining the Properties of Rocks [in Russian], Moscow, Gosgortekhizdat (1962).
V. V. Rzhevskii and G. Ya. Novik, Basic Physics of Rocks [in Russian], Moscow, Nedra (1964).
Additional information
Mining Institute, Leningrad. Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 2, pp. 104–107, March–April, 1967.
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Michik, Y.M., Dolgov, K.A. Specific surface energy: A new index of rock crushability and its application to blasting calculations. Soviet Mining Science 3, 186–188 (1967). https://doi.org/10.1007/BF02497286
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DOI: https://doi.org/10.1007/BF02497286