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One of the measures of rock quality in terms of availability for flow:

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{ \rm FZI } = \frac{\rm RQI}{\phi_z}

where

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body\rm RQI

Rock Quality Index

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body\phi_z

normalised porosity


Unit = μm


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, although it's rarely met in practise.

The FZI depends on grains size distribution, shape and packing and can be modelled as follows:

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anchorFZI
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{\rm FZI} = \frac{1}{\sqrt{F_S} \, S_{gV} \, \tau }

where

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body--uriencoded--S_%7BgV%7D = \Sigma_e/V_\phi

surface pore area per unit pore volume

LaTeX Math Inline
body\Sigma_e

pore surface area

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bodyF_S

pore shape factor

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bodyV_\phi

pore volume

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body\tau

pore channel tortuosity


In some practical cases this can be further simplified to:

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anchorFZI_d
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{\rm FZI} \approx 0.0037 \cdot \frac{d}{\tau }

where

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bodyd

average grain size


One of the proposed qualification of reservoir quality based on FZI is given by the Table 1.


Table1. One of the qualification schedules of reservoir quality.

FZI ValueReservoir Quality
FZI > 8.0Very Good
3.5 < FZI ≤ 8.0Good
1.0 < FZI ≤ 3.5Medium
0.45 < FZI ≤ 1.0Poor
FZI ≤ 0.45Very Poor

See also


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

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