By Faruk Civan

ISBN-10: 1118086430

ISBN-13: 9781118086438

ISBN-10: 1118086805

ISBN-13: 9781118086803

ISBN-10: 1118086813

ISBN-13: 9781118086810

ISBN-10: 1283176289

ISBN-13: 9781283176286

"This ebook covers the mass, momentum, and effort conservation equations, and their functions in engineered and traditional porous media for basic functions. This ebook is a vital textual content for graduate classes in a number of disciplines regarding fluids in porous fabrics and an invaluable reference publication. It offers a multi-disciplinary method of delivery in porous media. This booklet covers common porous media purposes together with chapters at the influence of temperature and particle migration and gives emphasis in strength assets improvement. the cloth is gifted in a uniform layout with constant SI units"--  Read more... Frontmatter -- evaluation -- shipping homes of Porous Media -- Macroscopic shipping Equations -- Scaling and Correlation of delivery in Porous Media -- Fluid movement in Porous Media -- gasoline delivery in Tight Porous Media -- Fluid shipping via Porous Media -- Parameters of Fluid move in Porous Media -- Mass, Momentum, and effort delivery in Porous Media -- Suspended Particulate shipping in Porous Media -- shipping in Heterogeneous Porous Media -- References -- Index

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2. Consequently, the pore body and pore-throat diameters are averaged as the mean hydraulic tube diameter. The coordination number and tortuosity are assumed to remain constant during dissolution and precipitation because the pore-throat plugging effect is negligible. The rate of variation of the pore volume is assumed as directly proportional to the instantaneous available pore volume and the participating pore surface, over which scale can be formed because of the affinity of the precipitating substance to the substrate present at the pore surface.

12 shows a data fit to a graphical depiction of Eq. 65). 1, column 4. 3 implies that the area open for flow belongs to a constricted fractal porous medium in contrast to the value of d = 3 for a theoretical nonfractal three-dimensional medium. 13 shows the variation of Γ and β with φ according to Eq. 59). 13 covers the range of 0 ≤ φ ≤ 1. In reality, the range utilized in the analysis is limited by the range of actual data. 2. 0 implied by the Kozeny–Carman equation, that is, Eq. 7). This confirms the claim by Couvreur et al.

The power-law correlation of these data indicates that the pore surface vanishes at zero porosity. 2 Example 2: Dolomite Mowers and Budd (1996) studied the dolomite reservoirs of Little Sand Draw Field, Wyoming, and Bindley Field, Kansas, both of which contain late-stage calcite cements. 5 Correlation of specific grain or pore surface area versus porosity for the data of Haughey and Beveridge (1969) and Mowers and Budd (1996) (Civan, 2002d; © 2002 SPWLA, reproduced by permission of the Society of Petrophysicists and Well Log Analysts).

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Porous media transport phenomena by Faruk Civan


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