We start with (Single-phase pressure diffusion @model:1):
|
|
and neglect the non-linear term c \cdot ( {\bf u} \, \nabla p) for low compressibility fluid c \sim 0 which is equivalent to assumption of nearly constant fluid density: \rho(p) = \rho = \rm const.
Together with constant pore compressibility c_\phi = \rm const this will lead to constant total compressibility c_t = c_\phi + c \approx \rm const.
Assuming that permeability and fluid viscosity do not depend on pressure k(p) = k = \rm const and \mu(p) = \mu = \rm const one arrives to the differential equation with constant coefficients:
|
|
or
(5) | \phi \, c_t \cdot \partial_t p + = \nabla \left( \frac{k}{\mu} \cdot ( \nabla p - \rho \, {\bf g}) \right) + \sum_k q_k(t) \cdot \delta({\bf r}-{\bf r}_k) |
See also
Physics / Mechanics / Continuum mechanics / Fluid Mechanics / Fluid Dynamics / Pressure Diffusion / Pressure Diffusion @model / Single-phase pressure diffusion @model