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(1) \phi \, c_t \, \mu \cdot \partial_t \Psi - \nabla \cdot \left( k \cdot \vec \nabla \Psi \right) = 0

where

p(t, {\bf r})

reservoir pressure

t

time

\rho({\bf r},p)

fluid density 

{\bf r }

position vector

\phi({\bf r}, p)

effective porosity 

{\bf r }_k

position vector of the k-th source

c_t({\bf r},p)

total compressibility 

\nabla

gradient operator

q_k(t)

sandface flowrates of the k-th source



k

formation permeability to a given fluid



\mu(p)

dynamic viscosity of a given  fluid



Z(p)

fluid compressibility factor

\displaystyle \Psi(p) =2 \, \int_0^p \frac{p \, dp}{\mu(p) \, Z(p)}

Pseudo-Pressure




See also


Physics / Mechanics / Continuum mechanics / Fluid Mechanics / Fluid Dynamics / Pressure Diffusion / Pressure Diffusion @model



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