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The rock volume  \Omega_R is split into three major components: effective pore volume  \Omega_eshale 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}



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