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Determining the thermal properties of rocks as functions of temperature

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Soviet Mining Aims and scope

Conclusions

  1. 1.

    The instantaneous heat source method permits joint measurement of the thermophysical coefficients of rocks as functions of temperature.

  2. 2.

    For the rocks investigated, the coefficients of thermal conductivity and thermal diffusivity declined with increase in temperature.

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Literature Cited

  1. M. V. Kulakov, Problems of Thermal Conductivity with a Heat Source, Heat Transfer, and Mass Transfer, [in Russian], Minsk (1962).

  2. E. D. Devyatkova, A. V. Petrov, I. A. Smirnov, and B. Ya. Moizhes, Fizika tverdodo tela,2, No. 4 (1960).

  3. L. Ya. Markovskii, D. L. Orshanskii, and V. P. Pryanishnikov, Chemical Electrothermics [in Russian], Moscow, Goskhimizdat (1952).

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Authors
  1. A. P. Dmitriev
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  2. L. S. Kuzyaev
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  3. G. N. Dobrovol'skii
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Additional information

Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 3, pp. 138–141, May–June, 1965

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Dmitriev, A.P., Kuzyaev, L.S. & Dobrovol'skii, G.N. Determining the thermal properties of rocks as functions of temperature. Soviet Mining Science 1, 290–292 (1965). https://doi.org/10.1007/BF02501970

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  • DOI: https://doi.org/10.1007/BF02501970

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