Thermal recovery from a fractured medium in local thermal non-equilibrium

Authors

  • Rachel Gelet,

    Corresponding author
    1. Laboratoire Sols, Solides, Structures, Grenoble Institute of Technology, Grenoble Cedex, France
    • School of Civil and Environmental Engineering, The University of New South Wales, Sydney, Australia
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  • Benjamin Loret,

    1. Laboratoire Sols, Solides, Structures, Grenoble Institute of Technology, Grenoble Cedex, France
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  • Nasser Khalili

    1. School of Civil and Environmental Engineering, The University of New South Wales, Sydney, Australia
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Correspondence to: Rachel Gelet, School of Civil and Environmental Engineering, The University of New South Wales, Sydney 2052, Australia.

E-mail: rachel.gelet@gmail.com

SUMMARY

Thermal recovery from a hot dry rock (HDR) reservoir viewed as a deformable fractured medium is investigated with a focus on the assumption of local thermal non-equilibrium (LTNE).

Hydraulic diffusion, thermal diffusion, forced convection and deformation are considered in a two-phase framework, the solid phase being made by impermeable solid blocks separated by saturated fractures. The finite element approximation of the constitutive and field equations is formulated and applied to obtain the response of a generic HDR reservoir to circulation tests. A change of time profile of the outlet fluid temperature is observed as the fracture spacing increases, switching from a single-step pattern to a double-step pattern, a feature which is viewed as characteristic of established LTNE. A dimensionless number is proposed to delineate between local thermal equilibrium (LTE) and non-equilibrium. This number embodies local physical properties of the mixture, elements of the geometry of the reservoir and the production flow rate. All the above properties being fixed, the resulting fracture spacing threshold between LTNE and LTE is found to decrease with increasing porosity or fluid velocity. The thermally induced effective stress is tensile near the injection well, illustrating the thermal contraction of the rock, while the pressure contribution of the fracture fluid is negligible during the late period. Copyright © 2012 John Wiley & Sons, Ltd.

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