期刊文献+

Scattering wave field around a cavity with circular cross-section embedded in saturated soil using boundary element method 被引量:3

Scattering wave field around a cavity with circular cross-section embedded in saturated soil using boundary element method
下载PDF
导出
摘要 Based on Biot’s theory and considering the properties of a cavity,the boundary integral equations for the numerical simulation of wave scattering around a cavity with a circular cross-section embedded in saturated soil are obtained using integral transform methods.The Cauchy type singularity of the boundary integral equation is discussed.The effectiveness of the properties of soil mass and incident field on the dynamic stress concentration and pore pressure concentration around a cavity is analyzed.Our results are in good agreement with the existing solution.The numerical results of this work show that the dynamic stress concentration and pore pressure concentration are influenced by the degree of fluid–solid coupling as well as the pore compressibility and water permeability of saturated soil.With increased degree of fluid–solid coupling,the dynamic stress concentration improves from 1.87 to 3.42 and the scattering becomes more significant.With decreased index of soil mass compressibility,the dynamic stress concentration increases and its maximum reaches 3.67.The dynamic stress concentration increases from 1.64 to 3.49 and pore pressure concentration improves from 0.18 to 0.46 with decreased water permeability of saturated soil. Based on Biot's theory and considering the properties of a cavity, the boundary integral equations for the numerical simulation of wave scattering around a cavity with a circular cross-section embedded in saturated soil are obtained using integral transform methods. The Cauchy type singularity of the boundary integral equation is discussed. The effectiveness of the properties of soil mass and incident field on the dynamic stress concentration and pore pressure concentration around a cavity is analyzed. Our results are in good agreement with the existing solution. The numerical results of this work show that the dynamic stress concentration and pore pressure concentration are influenced by the degree of fluid-solid coupling as well as the pore compressibility and water permeability of saturated soil. With increased degree of fluid-solid coupling, the dynamic stress concentration improves from 1.87 to 3.42 and the scattering becomes more significant. With decreased index of soil mass compressibility, the dynamic stress concentration increases and its maximum reaches 3.67. The dynamic stress concentration increases from 1.64 to 3.49 and pore pressure concentration improves from 0.18 to 0.46 with decreased water permeability of saturated soil.
出处 《Journal of Central South University》 SCIE EI CAS 2013年第11期3296-3304,共9页 中南大学学报(英文版)
基金 Projects(50969007,51269021) supported by the National Natural Science Foundation of China Projects(20114BAB206012,20133ACB20006) supported by the Natural Science Foundation of Jiangxi Province of China
关键词 saturated soil boundary integral equations wave scattering dynamic stress concentration Green's function 饱和土层 横截面 边界元法 圆形 动应力集中 边界积分方程 孔隙压力 波场
  • 相关文献

参考文献19

  • 1LEE V W, KARL J. Diffraction of elastic plane P waves by circular underground unlined tunnels [J]. European Earthquake Engineering, 1993, 6(1): 29 -36.
  • 2EL-AKILY N, DATTA S K. Response of a circular cylindrical shell to disturbances in a half-space [J]. Earthquake Engineering andStructural Dynamics, 1980, 8: 469-477.
  • 3BlOT M A. Theory of propagation of elastic waves in a fluid saturated porous solid. 1. Low frequency range [J]. Journal of the Acoustical Society of America, 1956, 28(2): 168-178.
  • 4BIOT M A. Theory of propagation of elastic waves in a fluid saturated porous solid. If. Higher frequency range [J]. Journal of the Acoustical Society of America, 1956, 28(2): 179 -191.
  • 5DERESIEWICZ H, RICE J T. The effect of boundaries on wave propagation in a liquid-filled porous solid [J]. Bulletin of the Seismological Society of America, 1962, 52(3): 595-625.
  • 6STOLL R D, BRYAN G M. Wave attenuation in saturated sediments [J]. Journal of tile Acoustical Society of America, 1970, 47(5), 1440-1447.
  • 7STOLL R D. Theoretical aspects of sound transmission in sediments [J]. Journal of the Acoustical Society of America. 1980, 68(5), 1341-1350.
  • 8NORRIS A N. Stoneley-wave attenuation and dispersion in permeable formations [J]. Geophysics, 1989, 54(3), 330-341.
  • 9HAMILTON E L. Sound attenuation as a function of depth in the seafloor [J]. Journal of the Acoustical Society of America. 1976, 59: 528 -535.
  • 10MEI C C, SI B I, CAI D Y. Scattering of simple harmonic waves by a circular cavity in a fluid-filled treated poro-elastic medium [J]. Wave Motion, 1984, 6(3): 265-278.

同被引文献26

引证文献3

二级引证文献3

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部