Abstract:To simulate the progressive failure process of the slope in water level fluctuation and rainfall conditions,a coupled fluid flow and stress computation model of dual media is established based on continuum-medium distinct element method. It contains solid calculation model,pore hydromechanical coupling model and fissure hydromechanical coupling model. Solid calculation model could reflect failure regularity of the geologic body,also could simulate the process from continuum to discontinuum. Pore hydromechanical coupling model could calculate the location of phreatic surface conveniently. Fissure hydromechanical coupling model could avoid convergence problem caused by isolated fissure. Considering the final states of the water level fluctuation and rainfall,the waterhead distribution caused by fissure seepage and water level fluctuation in reservoir are regarded as the variable boundary condition,thus implementing the coupling analysis for pore and fissure seepage flow field. Typical example computational results show that a coupled fluid flow and stress computation model of dual media based on continuum-medium distinct element method is very effective for the analysis of reservoir ancient landslide.
刘 洋,李世海,刘晓宇. 基于连续介质离散元的双重介质渗流应力耦合模型[J]. 岩石力学与工程学报, 2011, 30(5): 951-959.
LIU Yang,LI Shihai,LIU Xiaoyu. COUPLED FLUID FLOW AND STRESS COMPUTATION MODEL OF DUAL MEDIA BASED ON CONTINUUM-MEDIUM DISTINCT ELEMENT METHOD. , 2011, 30(5): 951-959.
YAN F Z,XU R C. Deformation behavior of ancient landslides on Qingjiang River after impoundment of the reservoir[C]// Proceedings of the 6th Symposium on Rock Mechanics and Engineering. [S.l.]:[s.n.],2000:543-546.
Your browse does not support frame!