Numerical Monte Carlo analysis of the influence of pore-scale dispersion on macrodispersion in 2-D heterogeneous porous media

被引:27
作者
Beaudoin, Anthony [1 ,2 ]
de Dreuzy, Jean-Raynald [3 ,4 ]
Erhel, Jocelyne [5 ]
机构
[1] Univ Havre, LOMC, Le Havre, France
[2] Univ Poitiers, CNRS, ENSMA, SP2MI,Inst P,UPR 3346, F-86962 Chasseneuil, France
[3] Univ Rennes 1, CNRS, UMR 6118, F-35042 Rennes, France
[4] CSIC, Inst Environm Assessment & Water Res, Barcelona, Spain
[5] INRIA Rennes, F-35042 Rennes, France
关键词
HYBRID FINITE-ELEMENTS; WALK PARTICLE TRACKING; SOLUTE TRANSPORT; TEMPORAL BEHAVIOR; FLOW; SIMULATIONS; AQUIFERS; IMPLEMENTATION; FIELDS; CLOUD;
D O I
10.1029/2010WR009576
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
We investigate the influences of pore-scale dispersion and of larger-scale permeability heterogeneities on the macrodispersion without the molecular diffusion. Permeability follows a lognormal exponentially correlated distribution characterized by its correlation length l and its lognormal variance sigma(2). Macrodispersion is evaluated numerically by using parallel simulations on grids of characteristic size ranging from 200 lambda to 1600 lambda. We note alpha(L) and alpha(T) the pore-scale longitudinal and transversal dispersivities. For alpha(L)/lambda < 10(-2) and alpha(T)/lambda < 10(-3), the influence of pore-scale dispersion on the macrodispersion is smaller than 5% of the macrodispersion due only to permeability heterogeneities. Larger dispersivities (alpha(L)/lambda >= 10(-2) or alpha(T)/lambda >= 10(-3)) induce larger effects than those obtained by the semianalytical expression of Salandin and Fiorotto (1998) for sigma(2) > 1. The effects of local dispersion on the longitudinal macrodispersion remain limited to 25% at most of the macrodispersion due only to permeability heterogeneities. For sigma(2) > 1, isotropic local dispersion induces a reduction of the longitudinal macrodispersion, whereas anisotropic local dispersion lets it increase. The longitudinal and transverse local dispersions induce opposite effects on the longitudinal macrodispersion, which are respectively an increase and a reduction. The transverse macrodispersion null without local dispersion or molecular diffusion becomes strictly positive with local dispersion. Because of the velocity field heterogeneities, it is amplified by a factor of 2 to 50 from the grid scale to the macro scale. The transverse dispersion is triggered by both longitudinal and transverse local dispersions. A reduction of a factor of 2 of the transverse local dispersion at fixed longitudinal local dispersion yields only a reduction of a factor of 4 at most of the transverse macrodispersion for sigma(2) >= 2.25.
引用
收藏
页数:9
相关论文
共 42 条
[1]  
[Anonymous], 1973, DYNAMICS FLUIDS PORO
[2]   Exact transverse macro dispersion coefficients for transport in heterogeneous porous media [J].
Attinger, S ;
Dentz, M ;
Kinzelbach, W .
STOCHASTIC ENVIRONMENTAL RESEARCH AND RISK ASSESSMENT, 2004, 18 (01) :9-15
[3]  
BEAUDOIN A, 2007, EUR PAR RENN FRANC
[4]   Analytical solutions for macrodispersion in a 3D heterogeneous porous medium with random hydraulic conductivity and dispersivity [J].
Chaudhuri, A ;
Sekhar, M .
TRANSPORT IN POROUS MEDIA, 2005, 58 (03) :217-241
[5]   A UNIFIED PHYSICAL PRESENTATION OF MIXED, MIXED-HYBRID FINITE-ELEMENTS AND STANDARD FINITE-DIFFERENCE APPROXIMATIONS FOR THE DETERMINATION OF VELOCITIES IN WATERFLOW PROBLEMS [J].
CHAVENT, G ;
ROBERTS, JE .
ADVANCES IN WATER RESOURCES, 1991, 14 (06) :329-348
[6]   Reply to comment by A. Fiori et al. on "Asymptotic dispersion in 2D heterogeneous porous media determined by parallel numerical simulations'' [J].
de Dreuzy, Jean Raynald ;
Beaudoin, Anthony ;
Erhel, Jocelyne .
WATER RESOURCES RESEARCH, 2008, 44 (06)
[7]   Relation between fractional flow models and fractal or long-range 2-D permeability fields [J].
de Dreuzy, Jean-Raynald ;
Davy, Philippe .
WATER RESOURCES RESEARCH, 2007, 43 (04)
[8]   Simulating solute transport in porous or fractured formations using random walk particle tracking: A review [J].
Delay, F ;
Ackerer, P ;
Danquigny, C .
VADOSE ZONE JOURNAL, 2005, 4 (02) :360-379
[9]   Temporal behavior of a solute cloud in a heterogeneous porous medium - 3. Numerical simulations [J].
Dentz, M ;
Kinzelbach, H ;
Attinger, S ;
Kinzelbach, W .
WATER RESOURCES RESEARCH, 2002, 38 (07) :23-1
[10]   Temporal behavior of a solute cloud in a heterogeneous porous medium 1. Point-like injection [J].
Dentz, M ;
Kinzelbach, H ;
Attinger, S ;
Kinzelbach, W .
WATER RESOURCES RESEARCH, 2000, 36 (12) :3591-3604