On dispersive propagation of surface waves in patchy saturated porous media

被引:11
|
作者
Zhang, Yu [1 ,2 ,5 ]
Xu, Yixian [3 ,4 ,5 ]
Xia, Jianghai [3 ,5 ]
Ping, Ping [3 ]
Zhang, Shuangxi [1 ,2 ]
机构
[1] Wuhan Univ, Sch Geodesy & Geomat, Wuhan 430079, Peoples R China
[2] Minist Educ, Key Lab Geospace Environm & Geodesy, Wuhan 430079, Peoples R China
[3] China Univ Geosci, Inst Geophys & Geomat, Wuhan 430074, Hubei, Peoples R China
[4] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Hubei, Peoples R China
[5] China Univ Geosci, Subsurface Multiscale Imaging Lab, Wuhan 430074, Hubei, Peoples R China
基金
中国国家自然科学基金;
关键词
Surface wave; Patchy saturation; Dispersion; Attenuation; FREQUENCY ACOUSTIC PROPERTIES; PARTIAL GAS SATURATION; RAYLEIGH-WAVES; SOLID INTERFACE; POROELASTIC MEDIUM; ATTENUATION; FLUID; ROCKS;
D O I
10.1016/j.wavemoti.2014.07.007
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
Frequency-dependent velocity and attenuation for Rayleigh-wave propagation along a vacuum/patchy saturated porous medium interface are investigated in the low frequency band (0.1-1000 Hz). Conventional patchy saturation models for compressional waves are extended to account for Rayleigh wave propagation along a free surface. The mesoscopic interaction of fluid and solid phases, as a dominant loss mechanism in patchy saturated media, significantly affects Rayleigh-wave propagation and attenuation. Researches on the dispersion characteristics at low frequencies with different gas fractions in patchy saturated media also demonstrate a strong correlation between the Rayleigh-wave mode and the fast compressional wave. Especially, the strongest attenuation with the maximum value of 1/Q for Rayleigh waves are obtained in the frequency range of 1-200 Hz. Numerical results show that the significant dependence of velocity and attenuation on frequencies and gas fractions presents a distinctive dynamical response of Rayleigh waves in the time domain. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:1225 / 1236
页数:12
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