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Rayleigh波在饱和半空间中圆形洞室周围的散射

发布时间:2018-03-24 09:45

  本文选题:饱和半空间 切入点:圆形洞室 出处:《岩土力学》2017年08期


【摘要】:基于Biot的两相介质理论,采用间接边界积分方程法,求解了Rayleigh波在饱和半空间中圆形洞室周围的二维散射问题,分析了入射波频率、孔隙率、边界渗透条件和洞室埋深等参数对地表位移幅值、洞室表面和地表孔隙水压力的影响。研究结果表明,由于圆形洞室的存在,饱和半空间地表位移幅值和地表孔隙水压被明显放大:在透水条件下,水平和竖向位移最大值分别比自由场放大了10.1倍和11.2倍;在不透水条件下,水平和竖向位移最大值分别比自由场放大了12.0倍和9.6倍,地表孔隙水压力放大了2.1~3.0倍。地表位移和孔隙水压力最大值均出现在入射波近端洞室边界附近。随着Rayleigh波入射频率的增大和洞室埋深的增加,地表位移幅值的放大作用有所减小。在相同孔隙率条件下,当入射频率为1.0时,洞室表面孔隙水压力最大;当入射频率为2.0时,洞室表面孔隙水压力最小,洞室表面最大孔隙水压力出现在洞室顶部。
[Abstract]:Based on Biot's two-phase medium theory and indirect boundary integral equation method, the two-dimensional scattering problem of Rayleigh wave around a circular cavity in saturated half-space is solved. The incident wave frequency and porosity are analyzed. The effects of boundary permeation conditions and cave depth on the surface displacement amplitude, pore water pressure on the surface of the cavern and the surface pore water pressure are studied. The amplitude of surface displacement and surface pore water pressure in saturated half-space are obviously enlarged: the maximum horizontal and vertical displacement are 10.1 and 11.2 times larger than those of free field under permeable condition, respectively, and in impermeable condition, the maximum value of horizontal displacement and vertical displacement is 11.2 times larger than that of free field, respectively. The maximum horizontal and vertical displacement are 12.0 and 9.6 times larger than the free field, respectively. The surface pore water pressure increases by 2.1 ~ 3.0 times. The maximum surface displacement and pore water pressure appear near the boundary of the cavern near the incident wave. With the increase of the incidence frequency of the Rayleigh wave and the increase of the buried depth of the cavity, the surface displacement and pore water pressure are increased. Under the same porosity, when the incident frequency is 1.0, the pore water pressure of the cavity surface is the largest, and when the incident frequency is 2.0, the pore water pressure of the cavity surface is the smallest. The maximum pore water pressure on the surface of the cavern appears at the top of the cave.
【作者单位】: 天津大学建筑工程学院;天津大学天津市土木工程结构及新材料重点实验室;天津城建大学天津市软土特性与工程环境重点实验室;
【基金】:国家自然科学基金项目(No.51378348)~~
【分类号】:P315.9

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