[1]Biot M A. Theory of elasticity and consolidation for a porous anisotropic solid
[J]. Applied Physics, 1955, 26: 182-185.
[2]Biot M A. Theory of propagation of elastic waves in a fluidsaturated porous solid:Ⅰ. lowfrequency range and Ⅱ. Higherfrequency range
[J]. Acoustical Society of America, 1956, 28: 168-191.
[3]Biot M A. Mechanics of deformation acoustic propagation in porous media
[J]. Applied Physics, 1962, 33: 1482-1498.
[4]Biot M A. Generalized theory of acoustic propagation in porous dissipative media
[J]. Acoustical Society of America, 1962, 34: 1254-1264.
[5]Mavko G, Mukerji T, Dvorkin J. The rock physics handbook
[M]. New York: Cambridge University Press, 1998: 221-224.
[6]Mavko G, Mukerji T, Dvorkin J. The rock physics handbook
[M]. 2nd Edition. New York: Cambridge University Press, 2009: 446-448.
[7]Yin H, Nur A, Mavko G. Critical porosityA physical boundary in poroelasticity
[J]. Rock Mechanics and Mining Sciences & Geomechanics, 1993, 30: 805-808.
[8]Nur A, Mavko G, Dvorkin J, and Galmudi D. Critical porosity: A key to relating physical properties to porosity in rocks
[J]. The Leading Edge, 1998, 17: 357-362.
[9]Chen Q, Nur A. Critical concentration models for porous materials
[M]// Yavuz Corapcioglu M. Advances in Porous Media. New York: Elsevier, 1994: 169-308.
[10]Niu B H, Sun C Y, Yan G Y,et al. Linear numerical calculation method for obtaining critical point, pore fluid, and framework parameters of gasbearing media
[J]. Applied Geophysics, 2009,6: 319-326.
[11]牛滨华, 孙晟, 孙春岩, 等. Biot介质密度参数的容差密度表达
[J]. 现代地质, 2007, 21(3): 551-555.
[12]Berge P A, Bonner B P, Berryman J G. Ultrasonic velocityporosity relationships for sandstone analogs made from fused glass beads
[J]. Geophysics, 1995, 60: 108-119. |