Three-dimensional vortices in single pores and their effects on transport

被引:49
作者
Cardenas, M. Bayani [1 ]
机构
[1] Univ Texas Austin, Dept Geol Sci, Austin, TX 78712 USA
关键词
D O I
10.1029/2008GL035343
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Three-dimensional Navier-Stokes flow and transport simulations are conducted for a single pore throat between cubic- packed grains 1-2 mm in diameter to advance our basic understanding of porous media processes. The grains are considered either spherical or ellipsoidal, and flow between the grains at different Reynolds Number is oriented along or across their long axis. Discharge through the pore varied linearly with imposed pressure gradients. Vortices are present near the pore throats, with narrower and deeper pore throats displaying a series of vortices. The vortices drive tailing of solutes resulting in power-law residence time distributions. Different tailing behavior is observed since the vortices are sensitive to grain shape and flow orientation. Tailing becomes more pronounced at higher Reynolds Number although the shape of the vortices remains unchanged.
引用
收藏
页数:6
相关论文
共 12 条
[1]   Modeling non-Fickian transport in geological formations as a continuous time random walk [J].
Berkowitz, Brian ;
Cortis, Andrea ;
Dentz, Marco ;
Scher, Harvey .
REVIEWS OF GEOPHYSICS, 2006, 44 (02)
[2]   Pore-scale modeling and continuous time random walk analysis of dispersion in porous media [J].
Bijeljic, B ;
Blunt, MJ .
WATER RESOURCES RESEARCH, 2006, 42 (01)
[3]   Trapping zones: The effect of fracture roughness on the directional anisotropy of fluid flow and colloid transport in a single fracture [J].
Boutt, David F. ;
Grasselli, Giovanni ;
Fredrich, Joanne T. ;
Cook, Benjamin K. ;
Williams, John R. .
GEOPHYSICAL RESEARCH LETTERS, 2006, 33 (21)
[4]   Navier-Stokes flow and transport simulations using real fractures shows heavy tailing due to eddies [J].
Cardenas, M. Bayani ;
Slottke, Donald T. ;
Ketcham, Richard A. ;
Sharp, John M., Jr. .
GEOPHYSICAL RESEARCH LETTERS, 2007, 34 (14)
[5]   Quantitative characterization of pore-scale disorder effects on transport in homogeneous granular media [J].
Cortis, Andrea ;
Chen, Youjian ;
Scher, Harvey ;
Berkowitz, Brian .
Physical Review E - Statistical, Nonlinear, and Soft Matter Physics, 2004, 70 (4 1) :041108-1
[6]   Anomalous transport in "classical" soil and sand columns [J].
Cortis, A ;
Berkowitz, B .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 2004, 68 (05) :1539-1548
[7]   A review of visualization techniques of biocolloid transport processes at the pore scale under saturated and unsaturated conditions [J].
Keller, Arturo A. ;
Auset, Maria .
ADVANCES IN WATER RESOURCES, 2007, 30 (6-7) :1392-1407
[8]   Do hydrodynamic dispersion coefficients exist? [J].
Lowe, CP ;
Frenkel, D .
PHYSICAL REVIEW LETTERS, 1996, 77 (22) :4552-4555
[9]   Pore-scale simulation of dispersion [J].
Maier, RS ;
Kroll, DM ;
Bernard, RS ;
Howington, SE ;
Peters, JF ;
Davis, HT .
PHYSICS OF FLUIDS, 2000, 12 (08) :2065-2079
[10]   TAYLOR DISPERSION IN POROUS-MEDIA - DETERMINATION OF THE DISPERSION TENSOR [J].
SALLES, J ;
THOVERT, JF ;
DELANNAY, R ;
PREVORS, L ;
AURIAULT, JL ;
ADLER, PM .
PHYSICS OF FLUIDS A-FLUID DYNAMICS, 1993, 5 (10) :2348-2376