Numerical Monte Carlo analysis of the influence of pore-scale dispersion on macrodispersion in 2-D heterogeneous porous media
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作者:
Beaudoin, Anthony
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Univ Havre, LOMC, Le Havre, France
Univ Poitiers, CNRS, ENSMA, SP2MI,Inst P,UPR 3346, F-86962 Chasseneuil, FranceUniv Havre, LOMC, Le Havre, France
Beaudoin, Anthony
[1
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de Dreuzy, Jean-Raynald
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Univ Rennes 1, CNRS, UMR 6118, F-35042 Rennes, France
CSIC, Inst Environm Assessment & Water Res, Barcelona, SpainUniv Havre, LOMC, Le Havre, France
de Dreuzy, Jean-Raynald
[3
,4
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Erhel, Jocelyne
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INRIA Rennes, F-35042 Rennes, FranceUniv Havre, LOMC, Le Havre, France
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.
机构:
State Univ Campinas UNICAMP, Dept Mech Engn FEM, BR-13083855 Campinas, SP, BrazilTexas State Univ, Ingram Sch Engn, San Marcos, TX 78666 USA
Iraji, Shohreh
de Almeida, Tales Rodrigues
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State Univ Campinas UNICAMP, Geosci Inst IG, Dept Geol & Nat Resources, BR-13083855 Campinas, SP, BrazilTexas State Univ, Ingram Sch Engn, San Marcos, TX 78666 USA
de Almeida, Tales Rodrigues
Basso, Mateus
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State Univ Campinas UNICAMP, Ctr Energy & Petr Study CEPETRO, BR-13083855 Campinas, SP, BrazilTexas State Univ, Ingram Sch Engn, San Marcos, TX 78666 USA
Basso, Mateus
Munoz, Eddy Ruidiaz
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State Univ Campinas UNICAMP, Ctr Energy & Petr Study CEPETRO, BR-13083855 Campinas, SP, BrazilTexas State Univ, Ingram Sch Engn, San Marcos, TX 78666 USA
Munoz, Eddy Ruidiaz
Vidal, Alexandre Campane
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State Univ Campinas UNICAMP, Geosci Inst IG, Dept Geol & Nat Resources, BR-13083855 Campinas, SP, BrazilTexas State Univ, Ingram Sch Engn, San Marcos, TX 78666 USA