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The relationship between the connected porosity and the total porosity is subparallel to the isoline (total porosity = connected porosity), whereas the vertical deviation from the isoline is given by the isolated porosity.
This study focuses only on connected porosity.
Porosity includes both connected porosity and unconnected porosity.
Bulk density decreases as connected porosity increases, as expected for samples of similar composition (Figure 8A).
Fracture occurred primarily between particles, and there is evidence of extensive intergranular connected porosity.
Low absorption indicates a reduction in the volume of the water-accessible surface connected porosity.
Techniques using inert gas measuring permeability and connected porosity simultaneously under mechanical loading have been presented.
Figure 11 indicates that for the rocks we tested, relatively low connected porosity generally correlates with samples with microfractures while relatively high connected porosity correlates with those containing pores or mixed microfractures and pores.
The bulk density decreases at high percentages of residue, however, indicating connected porosity and water-accessible porosity.
Connected porosity and dry bulk density were determined using the saturation and buoyancy method (Ulusay and Hudson 2007).
From this observation, we can infer that elastic closure of microfractures is important even in samples with high connected porosity.
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