FZI = \frac{RQI}{\phi_r}

where

Rock Quality Index

normalised porosity




It has much weaker dependence on effective porosity and shaliness and can be often considered constant within a given lithofacies which makes it a very efficient tool for lithofacies analysis


The constant FZI means that permeability strictly follows Cozeny-Karman permeability @model.


The FZI depends on grains size distribution, shape and packing.

The most popular correlation with a mean grain size  is given as:

FZI = a \cdot D_g

where coefficient  is a function of grain shape, packing, inter-grain clay and, as a consequence, of inter-grain effective porosity .

See also


Petroleum Industry / Upstream / Subsurface E&P Disciplines / Petrophysics

[ Rock Quality Index (RQI) ] [ Absolute permeability @model ]