Experimental analysis of pore-scale flow and transport in porous media

被引:90
作者
Rashidi, M
Peurrung, L
Tompson, AFB
Kulp, TJ
机构
[1] Battelle, Pacific Northwest Laboratories, Richland
[2] Sandia National Laboratories, Livermore
[3] Environmental Programs Department, Lawrence Livermore Natl. Laboratory, University of California, Livermore
关键词
transport; porous media; pore-scale flow; microscopic measurement; refractive index-matching; 3D imaging; velocimetry;
D O I
10.1016/0309-1708(95)00048-8
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
A novel, non-intrusive fluorescence imaging technique has been used to quantitatively measure the pore geometry, fluid velocity, and solute concentration within a saturated, three-dimensional porous medium. Discrete numerical averages of these quantities have been made over a representative volume of the medium and used to estimate macroscopic quantities that appear in conventional continuum models of flow and transport. The approach is meant to illustrate how microscopic information can be measured, averaged, and used to characterize medium-scale processes that are typically approximated constitutively. The experimental system consisted of a clear, cylindrical column packed with clear spherical beads and a refractive index-matched fluid seeded with fluorescent tracer particles and solute dye. By illuminating the fluid within the column with a scanning planar laser beam, details of flow and concentration within the pore spaces can be quantitatively observed, allowing for three-dimensional, time dependent information to be obtained at good resolution. In the current experiment, volumetrically averaged velocities and void-to-volume ratios are first compared with bulk measurements of fluid flux and medium porosity. Microscopic measurements of concentration are then used to construct cross-sectionally averaged profiles, mean breakthrough curves, and direct measurements of the dispersive flux, velocity variance, and concentration variance. In turn, the dispersive flux measurements are compared with mean concentration gradients to provide a basis for confirming the Fickian dispersion model and estimating dispersion coefficients for the medium. Coefficients determined in this manner are compared with others based upon traditional length-scale arguments, mean breakthrough analyses, and curve fits with numerical simulations.
引用
收藏
页码:163 / 180
页数:18
相关论文
共 28 条
[1]  
[Anonymous], CONVECTIVE HEAT MASS
[2]  
Bear J., 1972, DYNAMICS FLUIDS PORO
[3]  
Bear J., 1979, HYDRAULICS GROUNDWAT
[4]   LATTICE GAS AUTOMATA FOR FLOW THROUGH POROUS-MEDIA [J].
CHEN, SY ;
DIEMER, K ;
DOOLEN, D ;
EGGERT, K ;
FU, C ;
GUTMAN, S ;
TRAVIS, BJ .
PHYSICA D, 1991, 47 (1-2) :72-84
[5]  
Gray W. G., 1993, MATH TOOLS CHANGING
[6]   DERIVATION OF EQUATIONS FOR MULTIPHASE TRANSPORT [J].
GRAY, WG .
CHEMICAL ENGINEERING SCIENCE, 1975, 30 (02) :229-233
[7]   LATTICE-BOLTZMANN STUDIES OF IMMISCIBLE 2-PHASE FLOW THROUGH POROUS-MEDIA [J].
GUNSTENSEN, AK ;
ROTHMAN, DH .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1993, 98 (B4) :6431-6441
[8]   LONGITUDINAL AND LATERAL DISPERSION IN PACKED-BEDS - EFFECT OF COLUMN LENGTH AND PARTICLE-SIZE DISTRIBUTION [J].
HAN, NW ;
BHAKTA, J ;
CARBONELL, RG .
AICHE JOURNAL, 1985, 31 (02) :277-288
[9]   LONGITUDINAL AND LATERAL DISPERSION IN AN ISOTROPIC POROUS MEDIUM [J].
HARLEMAN, DRF ;
RUMER, RR .
JOURNAL OF FLUID MECHANICS, 1963, 16 (03) :385-394
[10]   General conservation equations for multi-phase systems: 1. Averaging procedure [J].
Hassanizadeh, Majid ;
Gray, William G. .
ADVANCES IN WATER RESOURCES, 1979, 2 :131-144