Thermal convection in three-dimensional fractured porous media

C. Mezon, V. V. Mourzenko, J.-F. Thovert, R. Antoine, F. Fontaine, A. Finizola, and P. M. Adler
Phys. Rev. E 97, 013106 – Published 11 January 2018

Abstract

Thermal convection is numerically computed in three-dimensional (3D) fluid saturated isotropically fractured porous media. Fractures are randomly inserted as two-dimensional (2D) convex polygons. Flow is governed by Darcy's 2D and 3D laws in the fractures and in the porous medium, respectively; exchanges take place between these two structures. Results for unfractured porous media are in agreement with known theoretical predictions. The influence of parameters such as the fracture aperture (or fracture transmissivity) and the fracture density on the heat released by the whole system is studied for Rayleigh numbers up to 150 in cubic boxes with closed-top conditions. Then, fractured media are compared to homogeneous porous media with the same macroscopic properties. Three major results could be derived from this study. The behavior of the system, in terms of heat release, is determined as a function of fracture density and fracture transmissivity. First, the increase in the output flux with fracture density is linear over the range of fracture density tested. Second, the increase in output flux as a function of fracture transmissivity shows the importance of percolation. Third, results show that the effective approach is not always valid, and that the mismatch between the full calculations and the effective medium approach depends on the fracture density in a crucial way.

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  • Received 4 May 2017

DOI:https://doi.org/10.1103/PhysRevE.97.013106

©2018 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

C. Mezon1,2,3,*, V. V. Mourzenko4, J.-F. Thovert4, R. Antoine2, F. Fontaine3, A. Finizola3, and P. M. Adler1

  • 1UPMC METIS, Boîte 105, 4 Place Jussieu, 75252 Paris Cedex 05, France
  • 2CEREMA, Direction territoriale Normandie Centre, Laboratoire de Rouen, Groupe Sciences de la Terre, Le Grand Quevilly, France
  • 3Laboratoire GéoSciences Réunion, Université de la Réunion, Institut de Physique du Globe de Paris, Sorbonne Paris Cité, CNRS UMR 7154, Saint Denis, La Réunion, France
  • 4Institut Pprime, CNRS, SP2MI, Boîte Postale 30179, 86962 Futuroscope Chasseneuil Cedex, France

  • *Corresponding author: cecile.mezon@upmc.fr

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Vol. 97, Iss. 1 — January 2018

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