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(see Compressibility @ Wikipedia)


A measure of formation porosity  \phi change due to pressure  p variation:

(1) c_r = \frac{1}{\phi} \frac{\partial \phi}{\partial p}

The above correlation assumes constant  which holds true in many practical applications.


It stays constant for small pressure variations ( c_r(p) = \rm const) but for a wide range pressure variations the dependence on ambient pressure  c_r(p) can not be neglected and can be estimated experimentally or via popular compressibility-porosity correlations on c_r(\phi)


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