HAN Gang, ZHAO Qi-hua, PENG She-qin. In-situ stress field evolution of deep fracture rock mass at dam area of Baihetan hydropower station[J]. 2011, 32(S1).
HAN Gang, ZHAO Qi-hua, PENG She-qin. In-situ stress field evolution of deep fracture rock mass at dam area of Baihetan hydropower station[J]. 2011, 32(S1).DOI:
formation time and evolution trend of deep fracture is analysed. Combined with deep fractures characteristic,tectonic evolution
valley evolution and near surface action theory
the formation and evolution process are summarized by stress field change and strain energy release with numerical simulation. The results show that: deep fractures in-situ stress field is fundamentally changed after vertical unloading; but deep fractures are not formed in this in-situ stress environment; the primary reason of deep fractures formation is lateral unloading and residual tensile stress caused by difference resilience; the formation time of deep fractures is about after Ⅲ terraces appearance