2022
DOI: 10.1016/j.compgeo.2022.105019
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A 2D FDEM-based THM coupling scheme for modeling deformation and fracturing of the rock mass under THM effects

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Cited by 14 publications
(5 citation statements)
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“…𝑹 𝑎 is the lumped viscous drag acting on the fluid phase 𝑎 (𝑎 = 𝑤, 𝑔, 𝑛) which is defined by the Darcy seepage law as ẇ𝒂 = 𝒌 𝑎 𝑹 𝑎 (9) where 𝒌 𝑎 is the permeability tensor of the porous medium to the pore fluid 𝑎 defined as…”
Section: Governing Equations Of Multi-phase Porous Media With Thermo-...mentioning
confidence: 99%
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“…𝑹 𝑎 is the lumped viscous drag acting on the fluid phase 𝑎 (𝑎 = 𝑤, 𝑔, 𝑛) which is defined by the Darcy seepage law as ẇ𝒂 = 𝒌 𝑎 𝑹 𝑎 (9) where 𝒌 𝑎 is the permeability tensor of the porous medium to the pore fluid 𝑎 defined as…”
Section: Governing Equations Of Multi-phase Porous Media With Thermo-...mentioning
confidence: 99%
“…The second term in Equation ( 28) indicates the effect of the fluid mass transfer (manifested by the fluid flow velocity, ẇ𝑖 in the form of advection) through the boundaries of the control volume in the heat balance equation as a convection term. 40,46 The relative velocities of the fluid phases with respect to the mixture can be eliminated from the thermal energy conservation equations (28) considering the Darcy's seepage law (9), resulting in the following version of the mixture enthalpy balance equation represented in terms of displacement, temperature and fluid pressures variables.…”
Section: Governing Equations Of Multi-phase Porous Media With Thermo-...mentioning
confidence: 99%
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