Regularities of changes in the stress-strain state of rocks in the slope zone
Authors:
About authors
- VSEGINGEO
Abstract
Removal of a part of rocks during the formation of natural slopes and artificial slopes leads to a decrease in the coefficient of lateral pressure in the near-slope zone and to a decrease in horizontal stresses in the adjacent two zones of the soil mass. This leads to an increase in deformations and, as a result, to subsidence due to plastic deformation and microshifts of structural bonds. At a number of sites, as a result of changes in the stress-strain state of rocks in the near-slope zone, accidents have been noted.
Область исследования:
(Archived) Development regularities of technogenic and geological processes and phenomena
Funding:
None
Similar articles
Challenges of engineering and geological research of the territory of Irkutsk
2003 I. I. Verkhozin, A. V. Samusenko, S. P. Nikiforov
Cryogenesis of lithogenic basis of landscapes in the North-East of Russia and prevention of its negative manifestations
2003 N. V. Ukhov
Groundwater regime in southern Transbaikalia and its impact on the stability of frost-affected bases of structures
2003 P. I. Salnikov