Sandstone reservoir permeability characteristics analysis based on White model
Chen Cheng1, Wen Xiaotao1,2, Hao Yaju1, Liu Jiale1, Zeng Yi3, Hu Junhui1
1. Geophysical Institute, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
2. Key Laboratory of Geodetection and Information Technology, Ministry of Education, Chengdu University of Technology, Chengdu, Sichuan 610059, China;
3. Shenzhen Branch, CNOOC, Shenzhen, Guangdong 510240, China
Abstract:This paper presents sandstone reservoir permeability characteristics analysis based on White model with patchy saturation. According Biot classical theory, we analyze permeability influence on seismic wave attenuation, velocity dispersion, normal-incident reflection coefficient, and phase for different consolidated sand reservoirs. It is found that permeability has strong influence on seismic wave attenuation and velocity dispersion for sand reservoirs, especially in medium consolidated sandstone reservoirs and unconsolidated sandstone reservoirs. Permeability has also strong influence on reflection coefficient and phase, especially in medium consolidated sandstone reservoirs, which might lead to phase polarity reversal.
Biot M. Theory of propagation of elastic waves in a fluid saturated porous solid,Ⅱ:Higher frequency range. Journal of the Acoustical Society of Americal,1956,28(2):179-191.
[2]
Biot M. Theory of propagation of elastic waves in a fluid saturated porous solid,Ⅰ:Low frequency range. Journal of the Acoustical Society of Americal,1956,28(2):168-178.
[3]
Mavko G M and Nur A. Wave attenuation in partially saturated rocks. Geophysics,1979,44(2):161-178.
[4]
Dvorkin J,Nolen-Hoeksema R and Nur A.The squirt-flow mechanism:macroscopic description. Geophy-sics,1994,59(3): 428-438.
Yang Dinghui,Chen Xiaohong. BISQ model for fluid-filled porous medium. OGP,2001,36(2):146-159.
[6]
杨德宽,杨顶辉,王书强. 基于BISQ高频极限方程的交错网格法数值模拟. 石油地球物理勘探,2002,37(5):463-468.Yang Dekuan,Yang Dinghui,Wang Shuqiang. Numerical simulation by staggered grid method for high frequency limited BISQ equation. OGP,2002,37(5):463-468.
[7]
Diallo M S,Prasad M and Appel E. comparison between experimental results and theoretical predictions of P-wave velocity and attenuation at ultrasonic frequency. Wave Motion,2003,37(1):1-16.
[8]
White J. computed seismic speeds and attenuation in rocks with partial gas saturation. Geophysics,1975,40(2):224-232.
[9]
Kozlov E. Seismic signatures of a permeable,dual-porosity layer. Geophysics,2007,72(5):SM281-SM291.
[10]
Ren H,Goloshubin G and Hilterman F. Poroelastic analysis of permeability effects in thinly layered porous media. Geophysics,2009,74(6):N49-N54.
[11]
Trapeznikova N A. Prognosis and Interpretation of Seismic Wave Dynamic [D]. Russian:Russian St Petersburg National University,1985.
[12]
Müller T M and Gurevich B. One-dimensional random patchy saturation model for velocity and attenuation in porous rocks. Geophysics, 2004,69(5):1166-1172.
[13]
Rubino J G. Permeability effects on the seismic response of gas reservoirs. Geophysical Journal International,2012,189(1):448-468.
[14]
Wood A. A Textbook of Sound. New York:MacMillan Publishing company,1995.
[15]
Hill R. Theory of mechanical properties of fiber-strengthened materials. Journal of the Mechanics and Physics of Solids,1964,12(1):357-372.
[16]
Johnson D L. Theory of frequency dependent acoustics in patchy saturated porous media. Journal of the Acoustical Society of Americal,2001,110(2):682-694.
[17]
Carcione J M. Wave Field in Real Media:Wave Propagation in Anisotropic,Anelastic and Porous Media. Pergamon Press,2001.
[18]
牟永光,陈小宏,刘洋等. 地震数据处理方法. 北京:石油工业出版社,2007,197-200.
[19]
Gazdag J. Wave equation migration with the phase shift method. Geophysics,1978,43(7):1342-1351.