Physical simulation of coal-gas two-phase flow migration in coal and gas outburst process
Centrifuge model test study on key hazard-inducing factors of deep toppling deformation and disaster patterns of counter-tilt layered rock slopes
Mechanical behaviors of basalt at Baihetan hydropower station and simulation with Hoek-Brown constitutive model
Field test analysis of instability mechanisms of high gas coal seams induced by hydraulic slotting
Study on the influence of in-situ stresses on dynamic fracture behaviors of cracks#br#
Study on failure precursors and seismogenic mechanisms of a large landslide based on moment tensor analysis
Experimental study on dynamic strength characteristics of water-saturated coal under true triaxial static-dynamic combination loadings
Experimental study on static fracturing mechanical characteristics of marble after cyclic impact loading
Study on the fracture propagation mechanisms of shale under tension
Study on surrounding rock control of roadways in deep coal mines based on roof cutting and pressure release technology by directional tensile blasting #br#
Bursting failure behavior of coal and response of acoustic and electromagnetic emissions
Discrete element simulation study on the influence of microstructure heterogeneity on the creep characteristics of granite
Based on discrete element method,a heterogeneous model considering the crystal size distribution was established by combining the grain-based model and parallel-bonded stress corrosion model. Through the comparative analysis of laboratory test and numerical simulation results,the applicability and reliability of the method of creep mechanical properties of granite were verified,and it is revealed that the heterogeneity caused by the crystal size distribution has significant influence on creep failure time,steady creep rate,number of microcracks and long-term strength. The main research conclusions are as follows:(1) The smaller the heterogeneity index,the more homogeneous the rock is,and the higher the uniaxial compressive strength and long-term strength are. The ratio of the long-term strength to the uniaxial compressive strength is about 0.70. (2) Under the same stress,the larger the heterogeneity index,the smaller the creep failure time is. Under the same driving stress ratio,the creep rate of the rock decreases and the creep failure time increases with increasing the heterogeneity index. (3) The development of microcracks is roughly divided into three stages including slow expansion,constant velocity expansion and accelerated expansion. The number of intergranular tensile microcracks is most and then intragranular tensile microcracks,followed by intergranular shear microcrack. (4) The microstructure of rock plays a controlling role in failure mode,and microcracks are preferred in the process of expansion. When the model is homogeneous,the failure mode exhibits cleft breakage. when the heterogeneity increases,the failure mode transforms to shear failure. The expansion of microcracks originates from crystal grain boundary with an obvious“bypassing core”phenomenon,that is,the feldspar with larger grain size has obvious influence on microcrack propagation and failure mode. The larger the rock heterogeneity,the more obvious the phenomenon is.
Analysis of energy evolution and damage characteristics of mudstone under cyclic loading and unloading
Research on the characteristics of hysteretic curves and damping ratio of frozen-thawed soils under cyclic subway loading
A large-strain nonlinear consolidation model of saturated soft soils stabilized by the vacuum-surcharge combined preloading method
Experimental study and numerical simulation of an alternating vacuum preloading method for strengthening hydraulic fill super soft soils#br#
Study on microstructure and macro-mechanical properties of paleosol under dry-wet cycles
Model tests of evaluation behaviors of the elastic wave velocity during the failure process of soil slopes due to rainfall
Radial consolidation theory for prefabricated vertical drain combined with vacuum preloading#br#