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Determination of Pore Size Distribution in Grained and Cavernous Rocks

  • V. I. Selyakov
  • V. V. Kadet
Part of the Theory and Applications of Transport in Porous Media book series (TATP, volume 9)

Abstract

It follows from the results presented above that the quantities Σ, K, k i are determined primarily by the function f(r). Therefore the first thing to know for the calculation of permeabilties is the size probability density function (PDF) for the pore channels.

Keywords

Probability Density Function Pore Size Distribution Percolation Threshold Percolation Model Reverse Problem 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer Science+Business Media Dordrecht 1996

Authors and Affiliations

  • V. I. Selyakov
    • 1
  • V. V. Kadet
    • 2
  1. 1.Laboratory of Heterogeneous Media, Department of Theoretical ProblemsRussian Academy of ScienceMoscowRussia
  2. 2.Department of Oil & Gas HydromechanicsState Gubkin Oil & Gas AcademyMoscowRussia

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