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.