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The pore structure ultimately affects the fluid flow property.
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They control the mechanics and fluid flow properties of the crust, and the architecture of sedimentary deposits in basins.
Such a correlation would be useful in dimensionally scaled storage vaults for experimental investigations of thermal and fluid flow properties.
Volume averaging of the pore-scale fluid flow properties allows calculation of the apparent permeability matrix of trabecular bone specimens.
Mesh convergence studies show that accurate fluid flow properties are obtained for a mesh size above 125,000 elements.
Pore network modeling gives a reasonable prediction of fluid flow properties at pore scale, and offers the flexibility of studying macroscopic properties relationship with pore structure and geometries.
Damage zones also influence fluid flow properties and the frictional strength of faults through their effects on pore pressure (Caine et al. 1996).
To explore the influence of various parameters on fluid flow properties, quantitative analysis is exhibited graphically and shown in the tabular form.
A hydraulic flow unit (HFU) is a region in a reservoir that presents similar petrophysical and fluid flow properties.
A non-isothermal flow of polymer melt with the temperature-dependent Carreau model for the fluid flow properties has been studied.
Engineers and hydrologists are commonly concerned with quantifying fluid flow properties, whereas sedimentogists are particularly interested in the sedimentary products that result from a variety of flow conditions.
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