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Small deviations of ambient pressure  p from initial pressure formation  p_0 lead to the exponential changes in porosity:

(1) \phi=\phi_0 \, e^{c_r (p-p_0)}

where  c_r is formation compressibility\phi_0 is porosity at reference pressure  p_0 (usually picked up at initial reservoir pressure  p_0 = p_i ).


The above correlation assumes constant formation compressibility which in most practical applications holds true in a wide range of pressure variations all the way down to porosity cut-off and all the way up to the fracture point.


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