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Prikladnaya Mekhanika i Tekhnicheskaya Fizika, 2012, Volume 53, Issue 6, Pages 159–167
(Mi pmtf1432)
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This article is cited in 2 scientific papers (total in 2 papers)
Thermoelastic model for the descent of avalanches and landslides
A. D. Chernyshov Voronezh State University of Engineering Technologies, Voronezh, 394000, Russia
Abstract:
A wedge-shaped mass of snow or soil on a flat mountain slope is simulated in a connected formulation by a thermoelastic medium acted upon by gravity, a uniform surface load, and a heat flux. An exact solution of the problem of equilibrium of the mass is obtained. Two criteria for the descent of an avalanche or a landslide are derived from the conditions of impossibility of equilibrium. This result can be used to predict soil landslides and the descent of avalanches in the mountains.
Keywords:
wedge-shaped mass, thermoelastic medium, avalanche.
Received: 06.09.2010 Revised: 16.12.2011
Citation:
A. D. Chernyshov, “Thermoelastic model for the descent of avalanches and landslides”, Prikl. Mekh. Tekh. Fiz., 53:6 (2012), 159–167; J. Appl. Mech. Tech. Phys., 53:6 (2012), 940–947
Linking options:
https://www.mathnet.ru/eng/pmtf1432 https://www.mathnet.ru/eng/pmtf/v53/i6/p159
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Abstract page: | 27 | Full-text PDF : | 8 |
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