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The Oberbeck-Boussinesq approximation was employed and homogeneity and local thermal equilibrium in the porous medium was assumed.
The electric field E in each uniform domain of the heterogeneous medium was assumed to be a solution of the vector Helmholtz equation (VHE): Delta ,mathbf{E}+ k^{2}, mathbf{E}=0, (1).
Since the composition of this medium is unknown, the medium was assumed to be similar to yeast extract [ 76], the composition used for simulations is indicated in the table in the Additional file 5: medium composition.
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The medium is assumed initially quiescent.
The pressurizing medium is assumed to be vacuum.
In the exterior domain, the unbounded elastic medium is assumed to be isotropic and homogeneous.
The fractured medium is assumed to be a single fissure in a porous rock matrix.
The ambient medium is assumed to have radial, axial and azimuthal component of fluid velocities.
The solid medium is assumed to be linear, isotropic, and dependent on the rate of temperature.
The elastic medium is assumed as two-parameter elastic foundation model proposed by Pasternak.
The medium is assumed to have a linear elastic constitutive behavior subjected to vertically propagating incident SV waves.
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