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Connected porosity is more easily measured through the volume of gas or liquid that can flow into the rock, whereas fluids cannot access unconnected pores. Porosity is the ratio of pore volume to its total volume. Porosity is controlled by: rock type, pore distribution, cementation, diagenetic history and composition. Porosity is not controlled ...
The porosity is a measure of the total pore space in the soil. This is defined as a fraction of volume often given in percent. The amount of porosity in a soil depends on the minerals that make up the soil and on the amount of sorting occurring within the soil structure.
In the vast majority of cases, this core analysis and Petroleum Engineering definition of effective porosity equates to total porosity. Effective porosity ϕ e 2 {\displaystyle \phi _{e2}} Effective porosity measured on core samples which are dried in a humidity oven so that clays retain one or two molecular layers of bound water—however ...
Φ T = Total porosity (PHIT), which includes the connected and not connected pore throats. Φ e = Effective porosity which includes only the inter-connected pore throats. V b = bulk volume of the rock. Key equations: V ma + V cl + V fw + V hyd = 1 Rock matrix volume + wet clay volume + water free volume + hydrocarbon volume = bulk rock volume [20]
where is void ratio, is porosity, V V is the volume of void-space (air and water), V S is the volume of solids, and V T is the total or bulk volume of medium. [1] The significance of the porosity is that it gives the idea of water storage capacity of the aquifer. Qualitatively, porosity less than 5% is considered to be small, between 5 and 20% ...
Porosimetry is an analytical technique used to determine various quantifiable aspects of a material's porous structure, such as pore diameter, total pore volume, surface area, and bulk and absolute densities. The technique involves the intrusion of a non-wetting liquid (often mercury) at high pressure into a material through the use of a ...
The Lagrangian porosity, (), which measures the porosity with respect to the initial or undeformed configuration. In a Lagrangian description of porosity, the pore volume is measured by ϕ ( x ) d V 0 {\displaystyle \phi (\mathbf {x} )\mathrm {d} V_{0}} , where d V 0 {\displaystyle \mathrm {d} V_{0}} represents an infinitesimal volume of the ...
NMR cryoporometry [1] [2] [3] is a recent technique for measuring total porosity and pore size distributions. NMRC is based on two equations: the Gibbs–Thomson equation, which maps the melting point depression to pore size, and the Strange–Rahman–Smith equation, [1] which maps the melted signal amplitude at a particular temperature to ...