Regularities of changes in the stress-strain state of rocks in the slope zone
Authors:
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- 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.
References
- Ломтадзе В.Д. Инженерная геология. Инженерная геодинамика. Л.: Недра, 1977. 479 с.
- Постоев Г.П, Классификация оползней по механизму нарушения равновесия массива пород // Изучение режима экзогенных геологических процессов в районах хозяйственного освоения / ВСЕГИНГЕО. М., 1988. С.52-64.
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