The curves of crack relative length lib and crack growth time t of granite were gained under compressive stresses state according to subcritical crack growth parameters and crack stability growth equation by double-to...The curves of crack relative length lib and crack growth time t of granite were gained under compressive stresses state according to subcritical crack growth parameters and crack stability growth equation by double-torsion constant displacement load relaxa- tion method.The relations between crack relative length and the crack growth time were discussed under different stresses and different crack lengths.The results show that there is a turning point on curve of crack relative length//b and crack growth time of granite.The slope of curve is small when crack relative length is less than the vertical coordinate of the point,and crack grows stably in this case.Cracks grow,encounter and integrate catastro- phically when crack relative length is more than the vertical coordinate of the point,and there is not a gradual stage from crack stability growth to crack instability growth,i.e.rock mass instability is sudden.The curves of crack relative length lib and crack growth time t of granite move to right with decrease of stress σ_1 or crack length a,which implies that limit time increases consequently.The results correspond to practicality.展开更多
This paper mainly observed and analyzed the character of shear-wave splitting in rock specimens while they were in the critical state of rupture. The rock specimens for study are made of Laizhou marble from Shandong, ...This paper mainly observed and analyzed the character of shear-wave splitting in rock specimens while they were in the critical state of rupture. The rock specimens for study are made of Laizhou marble from Shandong, China. A series of records were obtained from two rock specimens when they were in the critical state of rupture. The result shows that, in the critical state just before rock rupture, there may be the phenomenon of rise and fall in the time delay of shear-wave splitting, even though the load was kept constant. That is to say, the time delay of shear-wave splitting may have a falling process before rock rupture.展开更多
基金China Postdoctoral Science Foundation(20060400264)CSU Postdoctoral Science Foundationthe National Nature Science Foundation of China(50490274)
文摘The curves of crack relative length lib and crack growth time t of granite were gained under compressive stresses state according to subcritical crack growth parameters and crack stability growth equation by double-torsion constant displacement load relaxa- tion method.The relations between crack relative length and the crack growth time were discussed under different stresses and different crack lengths.The results show that there is a turning point on curve of crack relative length//b and crack growth time of granite.The slope of curve is small when crack relative length is less than the vertical coordinate of the point,and crack grows stably in this case.Cracks grow,encounter and integrate catastro- phically when crack relative length is more than the vertical coordinate of the point,and there is not a gradual stage from crack stability growth to crack instability growth,i.e.rock mass instability is sudden.The curves of crack relative length lib and crack growth time t of granite move to right with decrease of stress σ_1 or crack length a,which implies that limit time increases consequently.The results correspond to practicality.
基金the Science and Technology Activity B on Study-abroad Return Scholar of Non-Education System.
文摘This paper mainly observed and analyzed the character of shear-wave splitting in rock specimens while they were in the critical state of rupture. The rock specimens for study are made of Laizhou marble from Shandong, China. A series of records were obtained from two rock specimens when they were in the critical state of rupture. The result shows that, in the critical state just before rock rupture, there may be the phenomenon of rise and fall in the time delay of shear-wave splitting, even though the load was kept constant. That is to say, the time delay of shear-wave splitting may have a falling process before rock rupture.
