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That is to say, porosity is the ratio of void volume to the bulk volume (grains plus void space).
Density measurements for a given specimen involve the determination of any two of the following quantities: pore volume, bulk volume, or grain volume, along with the weight.
The term rock refers to the bulk volume of the material, including the grains or crystals as well as the contained void space.
Thus the total porosity (ϕT) is where VolG is the volume of grains (and cement, if any) and VolB is the total bulk volume.
As a result, some properties that are anisotropic (i.e., differ with direction) on a submicroscopic or crystalline scale are fairly isotropic for a large bulk volume of the rock.
● Bulk volume (range).
Reservoir bulk volume, ft3.
Bulk volume (ml).
Gridblock bulk volume (ft3).
Circle area represents the bulk volume.
The amount of quartz cement is generally below 10% bulk volume, but can exceed 10% bulk volume in single samples.
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