Three-Dimensional Numerical Manifold Method Based on Viscoelastic Constitutive Relation

被引:5
作者
Wu, Yanqiang [1 ,2 ]
Chen, Guangqi [3 ]
Jiang, Zaisen [4 ]
Zhang, Hong [5 ]
Zheng, Lu [6 ]
Pang, Yajin [1 ]
Guo, Nannan [1 ]
Zhang, Long [7 ]
机构
[1] CEA, Monitoring & Applicat Ctr 1, Tianjin 300180, Peoples R China
[2] Univ Calif Los Angeles, Dept Earth Planetary & Space Sci, Los Angeles, CA 90085 USA
[3] Kyushu Univ, Dept Civil & Struct Engn, Fukuoka 8190379, Japan
[4] CEA, Inst Earthquake Forecasting, CEA Key Lab Earthquake Predict, Beijing 100036, Peoples R China
[5] Tongji Univ, Coll Civil Engn, Shanghai 200092, Peoples R China
[6] Fuzhou Univ, Coll Civil Engn, Fuzhou 350108, Peoples R China
[7] China Earthquake Adm, Inst Geophys, Beijing 100081, Peoples R China
基金
国家重点研发计划; 美国国家科学基金会;
关键词
Maxwell viscoelastic model; Discontinuous deformation; Three-dimensional numerical manifold method; Creep properties; Stress relaxation properties; SIMULATION; PROPAGATION; FLOW;
D O I
10.1061/(ASCE)GM.1943-5622.0001798
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to accurately and efficiently simulate the dynamic processes of coupled phenomena with viscoelastic, continuous and discontinuous deformations, a three-dimensional (3D) numerical manifold method combining Maxwell's viscoelasticity (3D-VisNMM) is proposed and implemented in this study. First, the matrix formulas of 3D-VisNMM are derived, and then its technique flowchart is presented. Second, four viscoelastic models, which represent creep characteristics, stress relaxation features, stress accumulation, and frictional deceleration, respectively, are used to verify the feasibility of 3D-VisNMM. The creep model shows that the simulated deformation at each time step is highly consistent with the analytical solution. The stress relaxation model shows that the accuracy of simulated stress mainly depends on the time step, that is, the range of the Relative Standard Deviation (RSD) is 0.3%-4.8%, which corresponds to a time length of 0.1-2.0 years. The gravity-driven stress accumulation model shows that the RSD between the simulated results and analytical solutions is less than 0.004%. The frictional deceleration simulation shows that the RSD of cumulative displacements and accelerations are less than 0.65% and 2.4%, respectively. All these numerical simulations show that 3D-VisNMM is suitable for analyzing viscoelastic deformations, stress relaxation, and frictional sliding issues in multitemporal scale (second-century) and multispatial scale (meter-hundred kilometers). Therefore, 3D-VisNMM has a good application prospect in Geoscience research.
引用
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页数:10
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