岩土力学 ›› 2020, Vol. 41 ›› Issue (1): 315-324.doi: 10.16285/j.rsm.2018.2227

• 数值分析 • 上一篇    下一篇

饱和多孔热弹性介质中Rayleigh波 传播特性分析

周凤玺1,柳鸿博1,蔡袁强2   

  1. 1. 兰州理工大学 土木工程学院,甘肃 兰州 730050;2. 浙江工业大学 建筑工程学院,浙江 杭州 310014
  • 收稿日期:2018-12-07 修回日期:2019-04-28 出版日期:2020-01-13 发布日期:2020-01-05
  • 通讯作者: 柳鸿博,男,1994年生,硕士研究生,主要从事多孔介质中的波动特性等方面的研究。E-mail: lhb_0803@163.com E-mail:geolut@163.com
  • 作者简介:周凤玺,男,1979年生,博士,教授,主要从事岩土力学及复合材料结构力学等方面的研究工作。
  • 基金资助:
    国家自然科学基金(No. 51978320,No. 11962016)。

Analysis of propagation characteristics of Rayleigh waves in saturated porothermoelastic media

ZHOU Feng-xi1, LIU Hong-bo1, CAI Yuan-qiang2   

  1. 1. School of Civil Engineering, Lanzhou University of Technology, Lanzhou, Gansu 730050, China; 2. School of Civil Engineering and Architecture, Zhejiang University of Technology, Hangzhou, Zhejiang 310014, China
  • Received:2018-12-07 Revised:2019-04-28 Online:2020-01-13 Published:2020-01-05
  • Supported by:
    This work was supported by the National Natural Science Foundation of China (51978320, 11962016).

摘要: 基于多孔介质理论和广义的热弹性模型,研究了饱和多孔热弹性介质中Rayleigh波(R波)的传播特性。以考虑流-固耦合的饱和多孔介质波动方程和连续性方程及考虑热-弹耦合的广义热弹性基本方程出发,建立了饱和多孔介质的热?流?固耦合弹性波动模型。通过引入势函数并结合自由透水及绝热的边界条件,经过理论推导最终给出了饱和多孔热弹性介质中R波的弥散特征方程。利用数值算例分析了孔隙率、渗透系数、热膨胀系数、初始温度和松弛时间等热物理参数对R波的波速和特征衰减的影响。结果表明:孔隙率的增加将引起R波的波速下降,但使得R波的特征衰减反而增大;R波的波速随着渗透系数的增大先不变,再急剧增大,最后趋于稳定,其特征衰减随着渗透系数的增加先增大后减小,最后趋于稳定;热膨胀系数的增大将引起R波波速的增大,但对其特征衰减的影响较小;初始温度的增加导致R波波速的小幅上升,而对其特征衰减影响不大;松弛时间对R波波速和特征衰减几乎无影响。

关键词: 饱和多孔介质, 热弹性, Rayleigh波, 波速, 衰减

Abstract: Based on the theory of porous media and the generalized thermoelasticity model, the propagation characteristics of Rayleigh wave (R wave) in saturated porothermoelastic media are studied in this paper. A thermal-fluid-solid elastic wave coupled model of saturated porous medium is established by considering the fluid-solid coupling wave equations for saturated porous medium, continuity equation and the generalised thermoelastic basic equations. By introducing the potential function and combining the boundary conditions of free water permeability and adiabatic, the diffusion characteristic equation of R wave in saturated porous thermoelastic medium is derived theoretically. The effects of thermophysical parameters such as porosity, permeability coefficient, thermal expansion coefficient, initial temperature and relaxation time on the wave velocity and characteristic attenuation of R wave are analyzed by numerical examples. The results show that the increase of porosity causes the decrease of R wave velocity, but results in an increase in its characteristic attenuation. With the increase of the permeability coefficient, the R wave velocity first remains constant, then increases sharply, and finally stabilizes; and its characteristic attenuation first increases and then decreases, and finally tends to be stable. The increase of thermal expansion coefficient causes the increase of R wave velocity, but has no effect on the characteristic attenuation; the increase of initial temperature leads to slight increase of R wave velocity, but has little impact on its characteristic attenuation; the relaxation time has almost no effect on both the velocity and the characteristic attenuation of R wave.

Key words: saturated porous medium, thermoelasticity, Rayleigh wave, wave velocity, character attenuation

中图分类号: TU 435
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