Temperature stresses in rock massif caused by stationary temperature field
About authors
- 1 — G.V. Plekhanov Saint Petersburg Mining Institute
- 2 — OJSC YaregaRuda
Abstract
The issues of determination of stresses in rock massif at its heating by high-temperature steam are considered. The obtained dependences for determining the temperature stresses correspond to both flat and volumetric stressed state of the rock massif.
Область исследования:
(Archived) Geomechanics
Funding:
None
Similar articles
Model of the influence of natural fracturing and blockiness on explosive destruction of rocks
2007 M. G. Menzhulin, D. V. Moldovan, Yu. N. Borisenko, O. E. Legkova
Regularities of stress distribution in the protective cover during mining of the massif of rich iron ores of KMA with laying of the excavated space
2007 D. A. Potemkin
Numerical modeling of the stress-strain state of the overpass tunnel lining in the zone of their mutual influence
2007 P. A. Demenkov
Justification of rational methods of opening and mining of IV horizon in conditions of Starobinskoe potassium salt deposit
2007 E. R. Kovalskiy, K. A. Bondarev