Rayleigh-Darcy convection with hydrodynamic dispersion

被引:33
作者
Wen, Baole [1 ,2 ]
Chang, Kyung Won [2 ,3 ]
Hesse, Marc A. [1 ,2 ]
机构
[1] Univ Texas Austin, Inst Computat Engn & Sci, Austin, TX 78712 USA
[2] Univ Texas Austin, Jackson Sch Geosci, Dept Geol Sci, Austin, TX 78712 USA
[3] Sandia Natl Labs, Geomech Dept, Albuquerque, NM 87123 USA
关键词
CARBON-DIOXIDE DISSOLUTION; POROUS-MEDIUM; COLUMNAR CONVECTION; SOLUTAL-CONVECTION; NUMBER CONVECTION; CO2; DISSOLUTION; TENSOR FORM; STORAGE; FLOW; FLUID;
D O I
10.1103/PhysRevFluids.3.123801
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
We investigate the effect of hydrodynamic dispersion on convection in porous media by performing direct numerical simulations (DNS) in a two-dimensional Rayleigh-Darcy domain. Scaling analysis of the governing equations shows that the dynamics of this system are not only controlled by the classical Rayleigh-Darcy number based on molecular diffusion, Ra-m, and the domain aspect ratio, but also controlled by two other dimensionless parameters: the dispersive Rayleigh number Ra-d = H/alpha(t) and the dispersivity ratio r = alpha(l)/alpha(t), where H is the domain height and alpha(t )and alpha(l) are the transverse and longitudinal dispersivities, respectively. For Delta = Ra-d/Ra-m > O(1), the influence from the mechanical dispersion is minor; for Delta less than or similar to 0.02, however, the flow pattern is determined by Ra-d while the convective flux is F similar to c(Ra-d)Ra-m for large Ra-m. Our DNS results also show that the increase of mechanical dispersion, i.e., decreasing Ra-d, will coarsen the convective pattern by increasing the plume spacing. Moreover, the inherent anisotropy of mechanical dispersion breaks the columnar structure of the megaplumes at large Ra-m, if Ra-d < 5000. This results in a fan-flow geometry that reduces the convective flux.
引用
收藏
页数:18
相关论文
共 64 条
[1]   Anisotropic dispersive Henry problem [J].
Abarca, Elena ;
Carrera, Jesus ;
Sanchez-Vila, Xavier ;
Dentz, Marco .
ADVANCES IN WATER RESOURCES, 2007, 30 (04) :913-926
[2]   Causes of underpressure in natural CO2 reservoirs and implications for geological storage [J].
Akhbari, Daria ;
Hesse, Marc A. .
GEOLOGY, 2017, 45 (01) :47-50
[3]   GENERAL EQUATIONS OF HYDRODYNAMIC DISPERSION IN HOMOGENEOUS ISOTROPIC POROUS MEDIUMS [J].
BACHMAT, Y .
JOURNAL OF GEOPHYSICAL RESEARCH, 1964, 69 (12) :2561-&
[4]   Convective Instability and Mass Transport of Diffusion Layers in a Hele-Shaw Geometry [J].
Backhaus, Scott ;
Turitsyn, Konstantin ;
Ecke, R. E. .
PHYSICAL REVIEW LETTERS, 2011, 106 (10)
[5]   ON TENSOR FORM OF DISPERSION IN POROUS MEDIA [J].
BEAR, J .
JOURNAL OF GEOPHYSICAL RESEARCH, 1961, 66 (04) :1185-+
[6]   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)
[7]   Pore-scale modeling of transverse dispersion in porous media [J].
Bijeljic, Branko ;
Blunt, Martin J. .
WATER RESOURCES RESEARCH, 2007, 43 (12)
[8]   Dissolution in anisotropic porous media: Modelling convection regimes from onset to shutdown [J].
De Paoli, Marco ;
Zonta, Francesco ;
Soldati, Alfredo .
PHYSICS OF FLUIDS, 2017, 29 (02) :1-9
[9]   Influence of anisotropic permeability on convection in porous media: Implications for geological CO2 sequestration [J].
De Paoli, Marco ;
Zonta, Francesco ;
Soldati, Alfredo .
PHYSICS OF FLUIDS, 2016, 28 (05)
[10]  
DEJONG GD, 1958, T AM GEOPHYS UNION, V39, P67, DOI DOI 10.1029/TR039I001P00067