Mesoscopic fluid flow simulation in double-porosity rocks

作者: Jing Ba , Jian-Xin Nie , Hong Cao , Hui-Zhu Yang

DOI: 10.1029/2007GL032429

关键词:

摘要: [1] 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 transfers fast P waves and the first kind of slow waves' energy second waves, Biot diffusive mode significantly attenuates energy. We use a novel approach numerical grid method solve wave equations. conclude that wavefield's attenuation should be attributed two-step mechanism: (1) (2) macroscopic diffusion. Numerical estimations have shown model can produce high (0.32DB/10 m, 1/Q = 0.1083) seismic band (50 Hz).

参考文章(20)
José M. Carcione, Hans B. Helle, Nam H. Pham, White's model for wave propagation in partially saturated rocks: Comparison with poroelastic numerical experiments Geophysics. ,vol. 68, pp. 1389- 1398 ,(2003) , 10.1190/1.1598132
Steven R. Pride, James G. Berryman, Linear dynamics of double-porosity dual-permeability materials. II. Fluid transport equations. Physical Review E. ,vol. 68, pp. 036604- ,(2003) , 10.1103/PHYSREVE.68.036604
M. A. Biot, Theory of Propagation of Elastic Waves in a Fluid‐Saturated Porous Solid. I. Low‐Frequency Range The Journal of the Acoustical Society of America. ,vol. 28, pp. 168- 178 ,(1956) , 10.1121/1.1908239
David Linton Johnson, Theory of frequency dependent acoustics in patchy-saturated porous media Journal of the Acoustical Society of America. ,vol. 110, pp. 682- 694 ,(2001) , 10.1121/1.1381021
Mamadou Sanou Diallo, Erwin Appel, Acoustic wave propagation in saturated porous media: reformulation of the Biot/Squirt flow theory Journal of Applied Geophysics. ,vol. 44, pp. 313- 325 ,(2000) , 10.1016/S0926-9851(00)00009-4
JOSÉ M. CARCIONE, GERARDO QUIROGA-GOODE, SOME ASPECTS OF THE PHYSICS AND NUMERICAL MODELING OF BIOT COMPRESSIONAL WAVES Journal of Computational Acoustics. ,vol. 03, pp. 261- 280 ,(1995) , 10.1142/S0218396X95000136