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Mesoscopic fluid flow simulation in double-porosity rocks
Ba, Jing ; Nie, Jian-Xin ; Cao, Hong ; Yang, Hui-Zhu
2010-05-10 ; 2010-05-10
关键词WAVE-PROPAGATION POROUS-MEDIA SEISMIC ATTENUATION SATURATED ROCKS SLOW-WAVE FREQUENCY VELOCITY SQUIRT MODEL Geosciences, Multidisciplinary
中文摘要A discrete Fourier transform algorithm is designed to simulate mesoscopic fluid flow(MFF) in double-porosity rocks. Double-porosity equations with MFF are derived. Results from pseudo-spectral simulation show MFF transfers fast P waves and the first kind of slow P waves' energy to the second kind of slow P waves, and the Biot diffusive mode significantly attenuates the second kind of slow P waves' energy. We use a novel approach with a numerical grid method to solve the double-porosity wave equations. We conclude that the wavefield's attenuation should be attributed to a two-step mechanism: ( 1) MFF and ( 2) macroscopic Biot diffusion. Numerical estimations have shown that MFF in the double-porosity model can produce a high attenuation (0.32DB/10 m, 1/Q = 0.1083) in the seismic band (50 Hz).
语种英语 ; 英语
出版者AMER GEOPHYSICAL UNION ; WASHINGTON ; 2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA
内容类型期刊论文
源URL[http://hdl.handle.net/123456789/22512]  
专题清华大学
推荐引用方式
GB/T 7714
Ba, Jing,Nie, Jian-Xin,Cao, Hong,et al. Mesoscopic fluid flow simulation in double-porosity rocks[J],2010, 2010.
APA Ba, Jing,Nie, Jian-Xin,Cao, Hong,&Yang, Hui-Zhu.(2010).Mesoscopic fluid flow simulation in double-porosity rocks..
MLA Ba, Jing,et al."Mesoscopic fluid flow simulation in double-porosity rocks".(2010).
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