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The rock volume
\Omega_R is split into three major components: effective pore volume
\Omega_e, shale volume
\Omega_{sh} and rock martix
\Omega_m:
(1) |
\Omega_R = \Omega_e +\Omega_{sh} + \Omega_m |
The usual practice is to use relative volumes:
(2) |
\phi_e = \frac{\Omega_e}{\Omega_R}, \quad V_{sh} = \frac{\Omega_{sh}}{\Omega_R}, \quad V_m = \frac{\Omega_m}{\Omega_R} |
which are measured in V/V units (or fracs) and honor the following constraint:
(3) |
\phi_e +V_{sh} + V_m = 1 |
The relative effective pore volume
\phi_e contains free or connate fluids (water, oil , gas) and called effective porosity.
It corresponds to air porosity of the dried laboratory cores:
\phi_e = V_{\rm air \, core}.