A thermo-hydro-mechanical coupled model in local thermal non-equilibrium for fractured HDR reservoir with double porosity

The constitutive thermo‐hydro‐mechanical equations of fractured media are embodied in the theory of mixtures applied to three‐phase poroelastic media. The solid skeleton contains two distinct cavities filled with the same fluid. Each of the three phases is endowed with its own temperature. The const...

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Published inJournal of Geophysical Research Vol. 117; no. B7; pp. 1 - n/a
Main Authors Gelet, R., Loret, B., Khalili, N.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.07.2012
American Geophysical Union
Subjects
Civil Engineering
dual porosity
Earth sciences
Earth, ocean, space
Engineering Sciences
enhanced geothermal system
Exact sciences and technology
fluid loss
heat exchange
mass exchange
thermo-hydro-mechanical couplings
Sandoval County New Mexico
United States
New Mexico
Fenton Hill
stress
skeletons
porosity
finite element analysis
North America
mass transfer
fluid pressure
geothermal reservoirs
circulation
displacements
temperature
Chemical potential
equilibrium
Diffusion
fractures
theory
energy
hot dry rocks
constitutive modeling
Hot Dry Rock
geothermal energy
dual-porous media
local thermal non-equilibrium
Online AccessGet full text
ISSN0148-0227
2156-2202
DOI10.1029/2012JB009161

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Abstract The constitutive thermo‐hydro‐mechanical equations of fractured media are embodied in the theory of mixtures applied to three‐phase poroelastic media. The solid skeleton contains two distinct cavities filled with the same fluid. Each of the three phases is endowed with its own temperature. The constitutive relations governing the thermomechanical behavior, generalized diffusion and transfer are structured by, and satisfy, the dissipation inequality. The cavities exchange both mass and energy. Mass exchanges are driven by the jump in scaled chemical potential, and energy exchanges by the jump in coldness. The finite element approximation uses the displacement vector, the two fluid pressures and the three temperatures as primary variables. It is used to analyze a generic hot dry rock geothermal reservoir. Three parameters of the model are calibrated from the thermal outputs of Fenton Hill and Rosemanowes HDR reservoirs. The calibrated model is next applied to simulate circulation tests at the Fenton Hill HDR reservoir. The finer thermo‐hydro‐mechanical response provided by the dual porosity model with respect to a single porosity model is highlighted in a parameter analysis. Emphasis is put on the influence of the fracture spacing, on the effective stress response and on the permeation of the fluid into the porous blocks. The dual porosity model yields a thermally induced effective stress that is less tensile compared with the single porosity response. This effect becomes significant for large fracture spacings. In agreement with field data, fluid loss is observed to be high initially and to decrease with time. Key Points Thermo‐hydro‐mechanical equations of fractured media The model is calibrated from the thermal outputs of two HDR reservoirs Simulation of circulation tests at Fenton Hill HDR reservoir
AbstractList The constitutive thermo‐hydro‐mechanical equations of fractured media are embodied in the theory of mixtures applied to three‐phase poroelastic media. The solid skeleton contains two distinct cavities filled with the same fluid. Each of the three phases is endowed with its own temperature. The constitutive relations governing the thermomechanical behavior, generalized diffusion and transfer are structured by, and satisfy, the dissipation inequality. The cavities exchange both mass and energy. Mass exchanges are driven by the jump in scaled chemical potential, and energy exchanges by the jump in coldness. The finite element approximation uses the displacement vector, the two fluid pressures and the three temperatures as primary variables. It is used to analyze a generic hot dry rock geothermal reservoir. Three parameters of the model are calibrated from the thermal outputs of Fenton Hill and Rosemanowes HDR reservoirs. The calibrated model is next applied to simulate circulation tests at the Fenton Hill HDR reservoir. The finer thermo‐hydro‐mechanical response provided by the dual porosity model with respect to a single porosity model is highlighted in a parameter analysis. Emphasis is put on the influence of the fracture spacing, on the effective stress response and on the permeation of the fluid into the porous blocks. The dual porosity model yields a thermally induced effective stress that is less tensile compared with the single porosity response. This effect becomes significant for large fracture spacings. In agreement with field data, fluid loss is observed to be high initially and to decrease with time. Thermo‐hydro‐mechanical equations of fractured media The model is calibrated from the thermal outputs of two HDR reservoirs Simulation of circulation tests at Fenton Hill HDR reservoir
The constitutive thermo-hydro-mechanical equations of fractured media are embodied in the theory of mixtures applied to three-phase poroelastic media. The solid skeleton contains two distinct cavities filled with the same fluid. Each of the three phases is endowed with its own temperature. The constitutive relations governing the thermomechanical behavior, generalized diffusion and transfer are structured by, and satisfy, the dissipation inequality. The cavities exchange both mass and energy. Mass exchanges are driven by the jump in scaled chemical potential, and energy exchanges by the jump in coldness. The finite element approximation uses the displacement vector, the two fluid pressures and the three temperatures as primary variables. It is used to analyze a generic hot dry rock geothermal reservoir. Three parameters of the model are calibrated from the thermal outputs of Fenton Hill and Rosemanowes HDR reservoirs. The calibrated model is next applied to simulate circulation tests at the Fenton Hill HDR reservoir. The finer thermo-hydro-mechanical response provided by the dual porosity model with respect to a single porosity model is highlighted in a parameter analysis. Emphasis is put on the influence of the fracture spacing, on the effective stress response and on the permeation of the fluid into the porous blocks. The dual porosity model yields a thermally induced effective stress that is less tensile compared with the single porosity response. This effect becomes significant for large fracture spacings. In agreement with field data, fluid loss is observed to be high initially and to decrease with time.
The constitutive thermo‐hydro‐mechanical equations of fractured media are embodied in the theory of mixtures applied to three‐phase poroelastic media. The solid skeleton contains two distinct cavities filled with the same fluid. Each of the three phases is endowed with its own temperature. The constitutive relations governing the thermomechanical behavior, generalized diffusion and transfer are structured by, and satisfy, the dissipation inequality. The cavities exchange both mass and energy. Mass exchanges are driven by the jump in scaled chemical potential, and energy exchanges by the jump in coldness. The finite element approximation uses the displacement vector, the two fluid pressures and the three temperatures as primary variables. It is used to analyze a generic hot dry rock geothermal reservoir. Three parameters of the model are calibrated from the thermal outputs of Fenton Hill and Rosemanowes HDR reservoirs. The calibrated model is next applied to simulate circulation tests at the Fenton Hill HDR reservoir. The finer thermo‐hydro‐mechanical response provided by the dual porosity model with respect to a single porosity model is highlighted in a parameter analysis. Emphasis is put on the influence of the fracture spacing, on the effective stress response and on the permeation of the fluid into the porous blocks. The dual porosity model yields a thermally induced effective stress that is less tensile compared with the single porosity response. This effect becomes significant for large fracture spacings. In agreement with field data, fluid loss is observed to be high initially and to decrease with time. Key Points Thermo‐hydro‐mechanical equations of fractured media The model is calibrated from the thermal outputs of two HDR reservoirs Simulation of circulation tests at Fenton Hill HDR reservoir
Author Loret, B.
Gelet, R.
Khalili, N.
Author_xml – sequence: 1
  givenname: R.
  surname: Gelet
  fullname: Gelet, R.
  email: rachel.gelet@gmail.com, rachel.gelet@gmail.com
  organization: Laboratoire Sols, Solides, Structures, Institut National Polytechnique de Grenoble, Grenoble, France
– sequence: 2
  givenname: B.
  surname: Loret
  fullname: Loret, B.
  organization: Laboratoire Sols, Solides, Structures, Institut National Polytechnique de Grenoble, Grenoble, France
– sequence: 3
  givenname: N.
  surname: Khalili
  fullname: Khalili, N.
  organization: School of Civil and Environmental Engineering, University of New South Wales, Sydney, New South Wales, Australia
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ContentType Journal Article
Copyright 2012. American Geophysical Union. All Rights Reserved.
2015 INIST-CNRS
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Issue B7
Keywords stress
skeletons
porosity
finite element analysis
North America
mass transfer
fluid pressure
geothermal reservoirs
circulation
displacements
temperature
Chemical potential
equilibrium
Diffusion
fractures
theory
energy
hot dry rocks
constitutive modeling
Hot Dry Rock
geothermal energy
dual-porous media
local thermal non-equilibrium
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1970; 8
2000; 49
2006; 35
2004; 28
2002; 57
1973; 16
1994; 23
2008; 37
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1996; 33
1965; 3
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2006; 61
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1992; 118
1983
1982
1981
2005; 38
1994; 32
1998; 27
2011
2000; 24
1999; 28
2002; 34
1996
1993
2011; 38
1966; I
2003; 30
1996; 15
1989; 94
1977; 17
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1984; 39
1997; 34
2011; 50
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2001; 32
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Snippet The constitutive thermo‐hydro‐mechanical equations of fractured media are embodied in the theory of mixtures applied to three‐phase poroelastic media. The...
The constitutive thermo-hydro-mechanical equations of fractured media are embodied in the theory of mixtures applied to three-phase poroelastic media. The...
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SubjectTerms Civil Engineering
dual porosity
Earth sciences
Earth, ocean, space
Engineering Sciences
enhanced geothermal system
Exact sciences and technology
fluid loss
heat exchange
mass exchange
thermo-hydro-mechanical couplings
Title A thermo-hydro-mechanical coupled model in local thermal non-equilibrium for fractured HDR reservoir with double porosity
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https://onlinelibrary.wiley.com/doi/abs/10.1029%2F2012JB009161
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Volume 117
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