About This Item
- Full TextFull Text(subscription required)
- Pay-Per-View PurchasePay-Per-View
Purchase Options Explain
Share This Item
The Kozeny equation for fluid flow through isotropic unconsolidated porous media is developed. It is shown that the utility and application of this equation to consolidated and non-isotropic porous media hinge on the derivation of appropriate values for the Kozeny constant, k. It is postulated on the basis of a dichotomy originally suggested by Carman that the Kozeny constant for any porous system can be measured. Electrical methods to determine tortuosity in isotropic, non-isotropic, and partially saturated porous media are outlined and experimental data bearing on the validity of these methods are examined.
By combining the fundamental postulates of the Kozeny equation with the properties of the capillary pressure desaturation curve of a porous medium, a new expression for permeability is obtained:
Similarly, the wetting phase relative permeability is shown to be,
Here K is permeability, ^ggr interfacial tension, F formation factor, ^phgr porosity, Sw fractional wetting phase saturation, and Pc capillary pressure.
It is noted that the principal difference between unconsolidated and consolidated porous media lies in the higher tortuosities applicable to the latter. By the preparation of thin sections and the use of a statistical method for determining surface area, it is shown that the Kozeny equation appears to give valid surface areas for consolidated porous media. Such measurements make possible an estimate of the average grain sizes of many consolidated porous media.
Pay-Per-View Purchase Options
The article is available through a document delivery service. Explain these Purchase Options.
|Protected Document: $10|
|Internal PDF Document: $14|
|Open PDF Document: $24|
Members of AAPG receive access to the full AAPG Bulletin Archives as part of their membership. For more information, contact the AAPG Membership Department at [email protected].