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@wikipedia


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

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

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)


The typical values are in  0.5 \div 1.5 \cdot 10^{-6} \, {\rm kPa}^{-1} but may go higher for poorly consolidated rocks.



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