2017
DOI: 10.5194/se-8-805-2017
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A new theoretical interpretation of Archie's saturation exponent

Abstract: Abstract. This paper describes the extension of the concepts of connectedness and conservation of connectedness that underlie the generalized Archie's law for n phases to the interpretation of the saturation exponent. It is shown that the saturation exponent as defined originally by Archie arises naturally from the generalized Archie's law. In the generalized Archie's law the saturation exponent of any given phase can be thought of as formally the same as the phase (i.e. cementation) exponent, but with respect… Show more

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Cited by 52 publications
(26 citation statements)
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“…Archie's second law was then developed in applications to unsaturated porous media. In addition, many improved models of Archie's model have been proposed (Ewing and Hunt, 2006;Ghanbarian et al, 2014;Glover, 2017).…”
Section: Soil Modelmentioning
confidence: 99%
“…Archie's second law was then developed in applications to unsaturated porous media. In addition, many improved models of Archie's model have been proposed (Ewing and Hunt, 2006;Ghanbarian et al, 2014;Glover, 2017).…”
Section: Soil Modelmentioning
confidence: 99%
“…Statistically, exponents in empirical models describing petrophysical properties of have been shown to account for the arrangement of specific properties in porous media. As an example, a generalized saturation exponent in Archie's law (Archie, 1942), an empirical model, is said to account for the distribution of water phase within the pore space (Glover, 2017). Also, exponent in the general empirical expression for relative permeability (Ashford, 1969) is a characteristic of the capillary pressure, permeability, and porosity of the porous media; a specific value of this exponent reflects the nature of pertinent rock parameters (Ashford, 1969).…”
Section: Water Resources Researchmentioning
confidence: 99%
“…In the generalised Archie’s law, phase exponent m < 1 represents a phase with a high degree of connectivity [ 19 , 26 ]. A value of m ≈ 1 can be observed for rocks with a low porosity but a well-developed fracture network, the network then has fairly direct flow paths.…”
Section: Introductionmentioning
confidence: 99%