Rayleigh-Darcy convection with hydrodynamic dispersion

Baole Wen, Kyung Won Chang, and Marc A. Hesse
Phys. Rev. Fluids 3, 123801 – Published 7 December 2018

Abstract

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, Ram, and the domain aspect ratio, but also controlled by two other dimensionless parameters: the dispersive Rayleigh number Rad=H/αt and the dispersivity ratio r=αl/αt, where H is the domain height and αt and αl are the transverse and longitudinal dispersivities, respectively. For Δ=Rad/Ram>O(1), the influence from the mechanical dispersion is minor; for Δ0.02, however, the flow pattern is determined by Rad while the convective flux is Fc(Rad)Ram for large Ram. Our DNS results also show that the increase of mechanical dispersion, i.e., decreasing Rad, 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 Ram, if Rad<5000. This results in a fan-flow geometry that reduces the convective flux.

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  • Received 27 February 2018

DOI:https://doi.org/10.1103/PhysRevFluids.3.123801

©2018 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

Baole Wen1,2,*, Kyung Won Chang2,†, and Marc A. Hesse1,2,‡

  • 1Institute of Computational Engineering and Sciences, The University of Texas at Austin, Austin, Texas 78712, USA
  • 2Department of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, Texas 78712, USA

  • *wenbaole@gmail.com
  • Present address: Geomechanics Department, Sandia National Laboratories, Albuquerque, NM 87123, USA.
  • mhesse@jsg.utexas.edu

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Vol. 3, Iss. 12 — December 2018

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