The frequency dependence of harmonic fluid flow through networks of cracks and pores

被引:15
作者
Bernabe, Y
机构
[1] EOPG, CNRS URA 1358, Strasbourg, Université Louis Pasteur
关键词
permeability; electrical conductivity; porous rocks;
D O I
10.1007/s000240050037
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
The ''dynamic permeability k(omega) of heterogeneous networks of cracks, tubes and spheres, was determined by numerically simulating the harmonic Row of an interstitial fluid for a wide range of frequencies. For comparison with previous works, this procedure was applied to the 100 network realizations used in BERNABE (1995). In most cases, the calculated frequency dependence of the real and imaginary parts of k(omega) was consistent with the JKD model (JOHNSON et al., 1987), showing a transition from ''viscous'', macroscopic Row at low frequencies to ''inertial'' flow at high frequencies. The viscous skin depth delta(c) at the transition was found to be proportional to the critical capillary radius r(c) from a capillary invasion (KATZ and THOMPSON, 1986). A simple explanation is that these two length scales arise from the same percolation problem. On the other hand, delta(c) was not well correlated with the JKD parameter Lambda. The conclusion is that Lambda and delta(c) (or r(c)) are two independent parameters, derived from two unrelated approaches (i.e., weighted averaging and percolation theory). Finally, an attempt was made to relax the initial assumptions of a rigid solid matrix and an incompressible fluid. II was observed that the effect of the fluid compressibility could occasionally be very large, especially when networks with large amounts of storage pore space were considered.
引用
收藏
页码:489 / 506
页数:18
相关论文
共 23 条
[1]   INFLUENCE OF PORE ROUGHNESS AND PORE-SIZE DISPERSION IN ESTIMATING THE PERMEABILITY OF A POROUS-MEDIUM FROM ELECTRICAL MEASUREMENTS [J].
ACHDOU, Y ;
AVELLANEDA, M .
PHYSICS OF FLUIDS A-FLUID DYNAMICS, 1992, 4 (12) :2651-2673
[2]  
[Anonymous], 1981, CONTINUUM ELECTROMEC
[3]   DYNAMICS OF POROUS SATURATED MEDIA, CHECKING OF THE GENERALIZED LAW OF DARCY [J].
AURIAULT, JL ;
BORNE, L ;
CHAMBON, R .
JOURNAL OF THE ACOUSTICAL SOCIETY OF AMERICA, 1985, 77 (05) :1641-1650
[4]   PORE-SCALE HETEROGENEITY, ENERGY-DISSIPATION AND THE TRANSPORT-PROPERTIES OF ROCKS [J].
BERNABE, Y ;
REVIL, A .
GEOPHYSICAL RESEARCH LETTERS, 1995, 22 (12) :1529-1532
[5]   THE TRANSPORT-PROPERTIES OF NETWORKS OF CRACKS AND PORES [J].
BERNABE, Y .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1995, 100 (B3) :4231-4241
[6]   OSCILLATORY STOKES-FLOW IN PERIODIC POROUS-MEDIA [J].
CHAPMAN, AM ;
HIGDON, JJL .
PHYSICS OF FLUIDS A-FLUID DYNAMICS, 1992, 4 (10) :2099-2116
[7]   EXPERIMENTAL-STUDY OF DYNAMIC PERMEABILITY IN POROUS-MEDIA [J].
CHARLAIX, E ;
KUSHNICK, AP ;
STOKES, JP .
PHYSICAL REVIEW LETTERS, 1988, 61 (14) :1595-1598
[8]  
DULLIEN FAL, 1978, POROUS MEDIA
[9]   THE OSCILLATIONS OF A VISCOUS COMPRESSIBLE FLUID IN AN ARBITRARILY-SHAPED PORE [J].
Dvorkin, Jack ;
Mavko, Gary ;
Nur, Amos .
MECHANICS OF MATERIALS, 1990, 9 (02) :165-179
[10]   SCALING FUNCTION FOR DYNAMIC PERMEABILITY IN POROUS-MEDIA [J].
JOHNSON, DL .
PHYSICAL REVIEW LETTERS, 1989, 63 (05) :580-580