会议专题

NUMERICAL SIMULATION OF DYNAMIC RESPONSES IN TRANSVERSELY ISOTROPIC FLUID-SATURATED ELASTIC SEABED UNDER WAVE ACTIONS

The seabed is assumed to be transversely isotropic fluid-saturated elastic porous medium. Based on the anisotropy theory and Biot dynamic consolidation equations, this paper has established a 3D-dynamic seabed model in u-w-p form and defined anisotropic indicators ζα, ζβ, m for the first time. The governing equations are solved by the Wilson-θ finite element program of DSFEM, and the numerical model is verified by test results. The computation results indicate that the amplitude of the pore water pressure decays more quickly with higher wave heights, shorter wave periods, or in shallower water depths.

transversely isotropic seabed wave action dynamic equation finite element pore water pressure

Zhou-Yuan HENG Wang-Yong HE Sun ZHI Chen-Ming WEI

School of Civil and Architecture Engineering, Central South University, Changsha, China School of Water Conservancy, Changsha University of Science and Technology, Changsha, China

国际会议

International Symposium on Geoenvironmental Engineering(国际环境岩土工程研讨会

杭州

英文

462-466

2009-09-08(万方平台首次上网日期,不代表论文的发表时间)