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Exact(41)
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 ambient medium is assumed to have radial, axial and azimuthal component of fluid velocities.
The fractured medium is assumed to be a single fissure in a porous rock matrix.
The solid medium is assumed to be linear, isotropic, and dependent on the rate of temperature.
Similar(19)
The fluid velocities, the initial density and the initial magnetic field of the ambient medium are assumed to be varying and obey power laws.
Constant temperature and pH, as well as the homogeneity of the diffusion medium, are assumed.
Homogeneity and local thermal equilibrium in the porous medium are assumed.
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).
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