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@wikipedia
Part of the bulk rock volume 


Pore volume 

LaTeX Math Inline
body\Omega_\phi
  fraction of  bulk rock volume 
LaTeX Math Inline
body
V
\Omega_r
 containing the the hydrodynamically connected fluids (also called called free fluids) within each pore element with total volume 
LaTeX Math Inline
bodyV_f
:

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\phi_e = V_\phi = \frac{V\Omega_f\phi}{V\Omega_r}

Although the fluid inside the pore is movable but some pores maybe isolated from each other and do not contribute to rock permeability.


This splits the effective pore volume It splits into two components: open pore volume and closed pore volumeporosity and closed porosity:

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V_\phi_e = V_{\rm open} + V_{\rm closed}

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