Double-porosity rock model and squirt flow in the laboratory frequency band

被引:31
作者
Ba Jing [1 ]
Cao Hong [1 ]
Yao Fengchang [1 ]
Nie Jianxin [2 ]
Yang Huizhu [3 ]
机构
[1] PetroChina, Res Inst Petr Explorat & Dev, Beijing 1000084, Peoples R China
[2] Beijing Inst Technol, State Key Lab Explos Sci & Technol, Beijing 100081, Peoples R China
[3] Tsinghua Univ, Inst Seism Explorat, Beijing 100084, Peoples R China
关键词
double-porosity rock; pseudo-spectral method; self-affine fractal; microscopic scale; mesoscopic scale;
D O I
10.1007/s11770-008-0036-0
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Biot theory research has been extended to the multi-scale heterogeneity in actual rocks. Focused on laboratory frequency bandwidth studies, we discuss the relationships between double-porosity and BISQ wave equations, analytically derive the degeneration method for double-porosity's return to BISQ, and give three necessary conditions which the degeneration must satisfy. By introducing dynamic permeability and tortuosity theory, a full set of dynamic double-porosity wave equations are derived. A narrow band approximation is made to simplify the numerical simulation for dynamic double-porosity wavefields. Finally, the pseudo-spectral method is used for wave simulation within the laboratory frequency band (50 kHz). Numerical results have proved the feasibility for dynamic double-porosity's description of squirt flow and the validity of the quasi-static approximation method.
引用
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页码:261 / 276
页数:16
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