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STATE,ISSUES AND RELEVANT RECOMMENDATIONS FOR SECURITY RISK MANAGEMENT OF CHINA¢S UNDERGROUND ENGINEERING
THERMO-HYDRO-MECHANO-CHEMICAL COUPLING STUDIES ON EXCAVATION DAMAGE ZONE IN CRYSTALLINE ROCKS
VALIDATION FOR ROCK BLOCK STABILITY AND ITS APPLICATION TO ROCK SLOPE STABILITY EVALUATION USING DDA METHOD
NUMERICAL SIMULATION ON ASYMMETRIC DEFORMATION OF DEEP SOFT ROCK ROADWAY IN KONGZHUANG COAL MINE
NEW COMPUTATION METHOD FOR SOIL FOUNDATION SETTLEMENTS
STABILITY ANALYSIS OF ROCKY SLOPE BASED ON SLOPE STRUCTURES
ANALYSIS OF GROUND SETTLEMENTS OF OVERLENGTH PIPE AND BOX CULVERT ADVANCING UNDER AIRPORT TAXIWAY
STABILITY ANALYSIS OF YUANMO HIGHWAY SLOPE UNDER INTENSIVE RAINFALL
EXPERIMENTAL STUDY ON DAMPING CHARACTERISTICS OF ROCKUNDER CYCLIC LOADING
ON PROBABILITY MODEL OF PHYSICO-MECHANICAL PARAMETERS OF QUASI-BRITTLE MATERIALS AND ASSOCIATED MECHANICAL FAILURE BEHAVIORS
STUDY ON ELASTOPLASTIC DAMAGE MODEL OF UNSATURATED ROCK MASS AND ITS APPLICATION
PARALLEL NUMERICAL SIMULATION OF SEEPAGE IN FRACTURED ROCK MASS BASED ON STATISTIC MODEL
KRIGING INTERPOLATION MESHLESS METHOD BASED ON FINITE COVERS AND ITS APPLICATION TO CRACK PROPAGATION
RESEARCH ON PIPING MECHANISM IN SANDY SOILS BASED ON DISCRETE ELEMENT THEORY
Using particle flow code(PFC) based on discrete element theory and combining with the small-scale model tests,the piping in sandy soils is simulated with fluid-solid coupling. The porosity of sample,fluid velocity,contact number of particles,pathway of movable particles and loss fraction of eroded particles and so on are traced and recorded in the analytical model. The results show that the movable particles are eroded gradually;and the fluid velocity and porosity of sample increase gradually with the increase of water head;the permeability of sample changes,which will be influenced greatly by the response of fluid velocity and water head. The results reveal that the geometric and hydraulic features of system change dynamically and nonlinearly,which disclose their interactive behaviors during piping. The results also show that the loss fraction of eroded particles decreases along the seepage flow path;the small particles remove randomly;and the leak passages of piping are formed randomly when piping,which are the outcome of the complicated interactions between water and soil. The violent fluctuation of contact number of movable particles shows the violent motion of small particles during piping;and the stress field of soils is not influenced by particle erosion fundamentally. The availability and rationality of the proposed numerical method is verified by comparing the numerical solutions with the results of relevant physical model tests. The results are valuable to further probing into the piping mechanism in sandy soils.
MODEL EXPERIMENT STUDY ON INFLUENCES OF REINFORCEMENT ON INTERVALS OF ROCK BOLTS IN SURROUNDING ROCK UNDER EXPLOSIVE WAVES
INFLUENTIAL FACTORS OF ACOUSTIC EMISSION LOCATION EXPERIMENT OF ROCK UNDER UNIAXIAL COMPRESSION
RESEARCH ON VIBRATION INDUCED BY DYNAMIC UNLOADING OF IN-SITU STRESS IN ASYMMETRICAL GEOSTRESS FIELD
REALIZATION OF PAN JIAZHENG¢S EXTREMUM PRINCIPLE WITH OPTIMIZATION METHODS
WAVE-INDUCED DYNAMIC RESPONSE OF SEABED AROUND SUBMARINE PIPELINE
EXPERIMENTAL STUDY ON MECHANO-HYDRO-CHEMICAL COUPLING PROCESS IN CRACKED ROCKS
DAMAGE MODEL FOR UNSATURATED STRUCTURAL LOESS UNDER CYCLIC LOADING
PHYSICAL SIMULATION STUDY ON DEFORMATION AND FAILURE RESPONSE OF AN ANTI-INCLINED SLOPE DURING EXCAVATION
RESEARCH ON NONLINEAR DYNAMIC WARNING FOR HIGH SLOPES BASED ON PROGRESSIVE EVOLUTION PROCESS
STUDY ON DYNAMIC RESPONSE OF PILE BASED ON COMPLEX STIFFNESS TRANSFER MODEL OF RADIAL MULTIZONE PLANE STRAIN
STUDY ON NONLINEAR VISCOELASTO-PLASTIC CREEP MODEL OF ROCK AND ITS PARAMETER IDENTIFICATION
EXPERIMENTAL STUDY ON RHEOLOGICAL BEHAVIORS OF WANZHOU RED SANDSTONE IN THREE GORGES RESERVOIR AREA
Many approximately horizontal slip surface landslides are found in Jurassic red strata in Wanzhou of the Three Gorges Reservoir area. However,the formation mechanism of these landslides is not clear. In order to discover the causes of these landslides,experiments on rheological behaviors were performed on the sandstone of Erchengyan landslide bedrock in Wanzhou with triaxial creep test machine RLM–2000. Before the specimen failure,there is an accelerated creep stage,which lasts for about 8 h;this course is similar to the failure of deformation of some approximately horizontal slip surface landslides. Tautochrone of test data indicates this kind of rock is close to linear viscoelasto-plastic materials. Burgers model is used to fit the curves;and the three-dimensional constitutive relationship of Burgers model and its parameters are obtained. The results show that the proposed rheological Burgers model can exactly express the rheological characteristics of Jurassic red strata in Wanzhou. It can also describe the mechanism of the approximately horizontal slip surface landslides occurring in Jurassic red strata in Wanzhou. There is a nearly linear relationship between the creep strain rate and time in the beginning of accelerative creep stage. And the creep strain rate behaves closely to exponential growth with time in the last stage of accelerative creep. The accelerative creep shows highly nonlinear characteristics;and the creep strain rate displays a discontinuous form,which occurs in jumps change. Furthermore,the experimental results reveal the long-term strength of the rock is only 44 percent of the peak strength in triaxial tests. This conclusion is very helpful for the research on the mechanism and prevention of the horizontal slip surface landslides.
STUDY ON FORMATION MECHANISM AND STABILITY EVALUATION OF BADASHAN LANDSLIDE GROUP IN QINGHAI PROVINCE
INFLUENCE OF SEEPAGE ON STABILITY OF EARTH-ROCK DAM IN PLAIN AREA UNDER SEISMIC LOADING