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Soil Mechanics and Foundation Engineering

, Volume 36, Issue 6, pp 228–232 | Cite as

Effect of heat-and-mass transfer in rocks on the mechanism of the collapse of spoil banks on slopes

  • G. M. Eremin
Construction on Permafrost

Abstract

Experimental and computational data are presented on the variation in thermophysical and filtration properties of rock material in a spoil bank as a function of its lump size. The influence exerted by heat-and-mass transfer on the development of weakened zones with subsequent saturation of the rock ahead of the sort prism (“basin”), and the ejection of liquefied masses onto the slope in the last stage are indicated.

Keywords

Rock Mass Rock Material Weakened Zone Rock Layer Freeze Rock 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. 1.
    P. N. Panyukov, V. V. Rokevskii, V. V. Istomin, and A. M. Gal'perin,Geomechanics of Waste Operations in Quarries [in Russian], Nedra, Moscow (1972).Google Scholar
  2. 2.
    É. B. Krasnosel'skii, G. V. Kalabin, B. K. Ovodenko, G. M. Eremin, et al.,Spoil Banks on Mountain Slopes [in Russian], Nauka, Leningrad (1975).Google Scholar
  3. 3.
    N. S. Ivanov,Heat-and-mass transfer in frozen rocks [in Russian], Nauka, Moscow (1969).Google Scholar

Copyright information

© Kluwer Academic/Plenum Publishers 2000

Authors and Affiliations

  • G. M. Eremin

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