期刊文献+

固体颗粒不可压缩时饱和局部非均匀土孔压动态响应分析

The dynamic analysis of pore pressure response in the saturated local inhomogeneous soil as solid grain being incompressible
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摘要 为了分析微细观非均质结构对土体宏观力学特性的影响,本文基于有关局部非均质土波动理论的最新研究成果,推导了不考虑固体颗粒压缩性时,能描述局部结构对孔压增长和消散过程影响的动力学模型。针对周期荷载作用下的一维饱和土层,获得了孔隙水压分布的解析解。分别以松弛时间和荷载频率为变量,定量分析了这两参数对孔隙水压发展的影响趋势,并确定这两者影响孔压发展的敏感区间。 For analyzing the influence of the micro-mesoscopic inhomogeneous structures on the macroscopic mechanical property, based on the latest wave motion theory about the local inhomogeneous soil , the dynamic modelof which could describe the influence of the local structure on the pore pressure dynamic response as the solid grain is incompressible. By using this model, the analytical solution of the pore pressure is achieved in theone-dimensional saturated soil layer bearing periodic load. Treating the relaxation time and the load frequency as variables, the influence trends of which in the pore pressure are analysed quantitatively, and the sensitive range ofthem are determined.
出处 《地震工程与工程振动》 CSCD 北大核心 2013年第1期178-183,共6页 Earthquake Engineering and Engineering Dynamics
基金 中科院"百人计划"择优支持项目 中科院重要方向性项目的支持(No.kzcxz-yw-150)
关键词 局部非均匀土 固体颗粒不可压缩 孔隙水压力 松弛时间 荷载频率 saturated local inhomogeneous soil incompressible solid grain pore pressure the relaxation time loading frequency
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参考文献7

  • 1Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid. I. Low-frequency range [ J ]. J. Acoust Soc, Amer, 1956a, 28 : 168 - 178. 被引量:1
  • 2Biot M A. Theory of propagation of elastic waves in a fluid-saturated porous solid. II. Low-frequency range[ J]. J. Acoust. Soc. Amer, 1956b, 28: 179 - 191. 被引量:1
  • 3Wei C, Muraleetharan K K. Acoustical characterization of fluid-saturated porous media with local heterogeneities: theory and application. [ J]. international Journal of Solids and Structures,2006, 43 : 982 - 1008. 被引量:1
  • 4Dvorkin J,Nur A. Dynamic poroelastieity: A unified model with the squirt and the Biot mechanisms [ J]. Geophysics, 1993, 58:524 -533. 被引量:1
  • 5Pride S R, Berryman J G. Linear dynamics of double-porosity dual-permeability materials : I . Governing equations and acoustic attention[ J]. Phys Rev, 2003a, E68, 036603. 被引量:1
  • 6Pride S R, Berryman J G. Linear dynamics of double-porosity dual-permeability materials: II. Fluid transport equations [ J ]. Phys Rev. 2003b, E68. 036604. 被引量:1
  • 7曹华峰,韦昌富.饱和局部非均匀土的孔隙水压力动态响应分析[J].岩土力学,2013,34(4):933-940. 被引量:2

二级参考文献24

  • 1THEVANAYAGAM S,SHENTHAN T,MOHAN S,et al.Undrained fragility of clean sand,silty sand and sandysilts[J].J.Geotech.Geoenviron.Engrg.,ASCE,2000,128(10):849-859. 被引量:1
  • 2TOKIMATSU K,MIZUNO H,KAKURAI M.Buildingdamage associated with geotechnical problems[J].Soilsand Foundations,1996,36(Supp.):219-234. 被引量:1
  • 3YOUD T L,BARDET J P,KOCAELI B J D.Turkeyearthquake of August 17,1999 Reconnaissance Report[R].[S.l.]:Earthquake Engineering Research Institute,2001. 被引量:1
  • 4TANAKA Y.The 1995 Great Hanshin Earthquake andliquefaction damage at reclaimed lands at Kobe Port[J].Offshore and Ploar Engrg.,2000,10(1):15-25. 被引量:1
  • 5CARRARO J A,BANDINI P,SALGADO R.Li-quefaction resistance of clean and nonplastic silty sandsbased on cone peneteation resistance[J].Geotech Geo-environ.Engrg.,ASCE,2003,129(11):965-976. 被引量:1
  • 6BIOT M A.Theory of propagation of elastic waves in afluid-saturated porous solid.I.Low-frequency range[J].Acoust Soc.Amer.,1956,28:168-178. 被引量:1
  • 7BIOT M A.Theory of propagation of elastic waves in afluid-saturated porous solid.Ⅱ.Low-frequency range[J].Acoust.Soc.Amer.,1956,28:179-191. 被引量:1
  • 8DVORKIN J,NUR A.Dynamic poroelasticity:A unifiedmodel with the squirt and the Biot mechanisms[J].Geophysics,1993,58:524-533. 被引量:1
  • 9DVORKIN J,RICHARD N,NUR A.The squirt-flowmechanism:Macroscopic description[J].Geophysics,1994,59:428-438. 被引量:1
  • 10MAVKO G,NUR A.Melt squirt in asthenosphere[J].Geophysics.Res.,1975,80:1444-1448. 被引量:1

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