期刊文献+

基于逐步扩大网格法的饱和无限地基动力分析 被引量:2

DYNAMIC ANALYSIS FOR INFINITE SATURATED FOUNDATION BASED ON GRADUAL ENLARGEMENT MESH METHOD
原文传递
导出
摘要 饱和无限地基的动力分析是研究结构与饱和土共同作用的基础。当用有限区域模拟饱和无限地基时,将在人工截取的边界上发生波的反射,导致模拟失真。该文基于远置人工边界的原理,采用逐步扩大网格法的思想来解决这一问题。并通过算例验证了该方法的精度。该方法避免了饱和介质中其他人工边界实施上的繁琐,并且避开了其它人工边界存在的大角度入射情况以及稳定性问题等不确定因素,可以用于饱和介质中其他人工边界条件的检验工作。 Dynamic analysis of infinite saturated foundation is required to study the saturated soil-structure interaction. If infinite saturated foundation is simulated by a finite region, wave reflection will take place on the artificial intercepted boundary. Adopting remote artificial boundaries, this problem is solved by gradual enlargement mesh. The method is verified through an example. With gradual enlargement mesh method, not only the difficulty of implementation on other artificial boundary can be avoided, but also some uncertain factors in other artificial boundary such as boundary stability and large angle incidence and so on can be avoided, so it can be used to check other artificial boundary.
出处 《工程力学》 EI CSCD 北大核心 2010年第4期149-152,184,共5页 Engineering Mechanics
基金 中国农业大学科研启动基金项目(2007016) 国家科技支撑项目(2006BAJ04B03-002)
关键词 饱和无限地基 逐步扩大网格法 动力分析 人工边界 波动 infinite saturated soil foundation gradual enlargement mesh method dynamic analysis artificial boundary wave motion
  • 相关文献

参考文献11

  • 1Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid: I. Low-frequency range [J]. Journal of the Acoustical Society of American, 1956, 28(2): 168- 178.
  • 2Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid: II. Higher frequency range [J]. Journal of the Acoustical Society of American, 1956, 28(2): 179- 191.
  • 3Biot M A. Mechanics of deformation and acoustic propagation in porous media [J]. Journal of Applied Physics, 1962, 33(4): 1482- 1498.
  • 4Degrande G, De Roeck G. An absorbing boundary condition for wave propagation in saturated poroelastic media-Part I: Formulation and efficiency evaluation [J] Soil Dynamics and Earthquake Engineering, 1993, 12: 411-421.
  • 5Degrande G, De Roeck G An absorbing boundary condition for wave propagation in saturated poroelastic media-Part II: Finite element formulation [J]. Soil Dynamics and Earthquake Engineering, 1993, 12: 423 -432.
  • 6Akiyoshi T, Sun X, Fuchida K. General absorbing boundary conditions for dynamic analysis of fluid-saturated porous media [J]. Soil Dynamics and Earthquake Engineering, 1998, 17: 397-406.
  • 7吴德伦,张建华.饱和孔隙介质中波动分析的加权吸收边界条件[J].岩土工程学报,1997,19(4):57-65. 被引量:5
  • 8陈少林,廖振鹏.多次透射公式在衰减波场中的实现[J].地震学报,2003,25(3):272-279. 被引量:13
  • 9贺向丽,李同春.无限域波动问题的局部非协调网格法[J].振动工程学报,2006,19(1):124-127. 被引量:2
  • 10贺向丽,李同春,任灏.基于逐步扩大网格法的重力坝地震响应分析[C].第17届全国结构工程学术会议,北京,2008.

二级参考文献22

  • 1廖振鹏.局部透射边界的精度[J].地震工程与工程振动,1993,13(3):1-6. 被引量:13
  • 2陈少林.[D].中国地震局工程力学研究所,2002.146~147.
  • 3廖振鹏.近场波动的数值模拟[J].力学进展,1997,27(2):193-216. 被引量:65
  • 4Liao Zhenpeng. 2001. Transmitting boundary and radiation condition at infinity[J] SCIENCE IN CHINA (Series E), 44(2): 177-186.
  • 5Simon B R, Zienkiewicz O C, Paul D K. 1984. An analytical solution for the transient response of saturated porous elastic solidsl[J]. Int J Numer Anal Methods Geomech , 8:381-398.
  • 6Wolf J P, Song C. 1996. Finite-Element Modelling of Unbounded Media[M]. John WILEY, SONS, Chi Chesper.
  • 7Chen J. 1994. Time domain fundamental solution to Blot's complete equations of dynamic poroelasticity part I: Two-dimensional solution[J]. Int J Solids Struct, 31(10): 1 447-1 490.
  • 8Clayton R, Engquist B. 1977. Absorbing boundary conditions for acoustic and elastic wave equations[J]. Bull Seism Soc Amer, 67:1 529-1 540.
  • 9Givoli D, Keller J B. 1990. Non-reflecting boundary conditions for elastic waves[J]. Wave Motion, 12:261-279.
  • 10Higdon R L. 1987. Numerical absorbing boundary conditions for the wave equation[J]. Math Comput, 49:65-90.

共引文献17

同被引文献17

引证文献2

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