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Using deionised water as working fluid, the measured average permeability value on scaffolds of 90 95% porosity was 1.96×10−9 m2.
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To measure average permeability, the amount of this parameter is calculated in each layer in Table 4.
However, results of this work correspond to those of Willens et al. [14], who measured the average permeability coefficient of dorsal skin of Rana catesbeiana exposed to malathion in vitro being lower (6.5 × 10−3cm/h) than that of ventral skin (8.95 × 10−3cm/h).
Note that in this paper, we use terms "observed permeability", "measured permeability" and "effective permeability" interchangeably and subscript "eff" refers to the effective permeability.
Additionally, the average permeability value is re-estimated.
To calculate average permeability, weighted-average permeability, harmonic-average permeability, and geometric-average permeability techniques are derived from experimental evaluations (McCain et al. 2011).
The average permeability was 350 mD.
The selected average permeability represents the average permeability of the candidate reservoir.
Few layers exhibit permeabilities that are high (higher than twice the average permeability).
Such local permeability models are herein suggested for predicting the average permeability of geothermal prospects.
Average permeability ranges from 53 to 567 mD.
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