A pore volume fraction of bulk rock volume
containing the hydrodynamically connected fluids (also called free fluids) within each pore element:
\phi_e = \frac{V_\phi}{V_r} |
The reason to introduce this concept is that a part of the actual inter-grain void is filled with shale thus reducing the actual volume available for fluids.
It splits into two components:
| with interconnected pores | with isolated pores |
subject to condition:
\phi_e = \phi_{\rm opn} + \phi_{\rm cls} |
Effective porosity is a function of reservoir pressure at a given location :
\phi_e(\mathbf{r}, \ p) = \phi_{ei}(\mathbf{r}) \exp \left[ \int_{p_i}^p c_\phi(p) \, dp \right] |
where
| pore compressibility (see also Pore compressibility @model ) | |
| initial formation pressure |
This leads to the effect of Porosity Shrinkage.
Since the pore compressibility is very low (~ cϕ = 0.5 ÷ 1.5 GPa-1) and has a weak dependence on reservoir pressure for subsurface rocks in petroleum reservoirs the can be written as:
\phi_e(\mathbf{r}, \ p) = \phi_{ei}(\mathbf{r}) \cdot \left[ 1 + c_\phi \, (p-p_i) + 0.5 \, c_\phi^2 \, (p-p_i)^2 \right] |
Most Subsurface E&P Disciplines (except Petrophysics) usually omit index "e" and denote Effective porosity as .
Petroleum Industry / Upstream / Subsurface E&P Disciplines / Petrophysics (PP) / Volumetric Rock Model
[ Basic reservoir properties ] [ Pore volume ] [ Connected pore volume ] [ Closed pore volume ] [ Porosity ] [ Open porosity ] [ Closed porosity ][ Initial Porosity ϕi ]
[ Pore compressibility @model ]