Transport in Porous Media

, Volume 125, Issue 1, pp 23–39 | Cite as

An Object-Based Shale Permeability Model: Non-Darcy Gas Flow, Sorption, and Surface Diffusion Effects

  • Morteza E. Naraghi
  • Farzam JavadpourEmail author
  • Lucy T. Ko


Shale samples consist of two major components: organic matter (OM) and inorganic mineral component (iOM). Each component has its distinct pore network topology and morphology, which necessitates generating a model capable of distinguishing the two media. We constructed an object-based model using the OM and iOM composition of shale samples. In the model, we integrated information such as OM population and size distribution, as well as its associated pore-size distribution. For the iOM part, we used mineralogy and pore-size information derived from X-ray diffraction, scanning electron microscopy, and nitrogen sorption measurements. Our proposed model results in millimeter-scale 2D realizations of shale samples by honoring OM and mineral types, their compositions, shapes, and size distributions. The model can capture heterogeneities smaller than 1 mm. We studied the effects of different gas flow processes and found that Knudsen diffusion and gas slippage dominate the flow, but surface diffusion has little impact on total gas flow.


Gas flow in shale Nanopore Stochastic Reconstruction of porous media 



This work was supported partly by the NanoGeosciences laboratory and by the Mudrock Systems Research Laboratory (MSRL) consortium at the Bureau of Economic Geology, The University of Texas at Austin. MSRL member companies are Anadarko, BP, Cenovus, Centrica, Chesapeake, Cima, Cimarex, Chevron, Concho, ConocoPhillips, Cypress, Devon, Encana, Eni, EOG, EXCO, ExxonMobil, Hess, Husky, Kerogen, Marathon, Murphy, Newfield, Penn Virginia, Penn West, Pioneer, Samson, Shell, Statoil, Talisman, Texas American Resources, The Unconventionals, U.S. Enercorp, Valence, and YPF. We appreciate Drs S. Ruppel and R. Reed’s instructive comments. Susie Doenges edited the manuscript. Publication was authorized by the Director, Bureau of Economic Geology.


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© Springer Science+Business Media B.V., part of Springer Nature 2018

Authors and Affiliations

  1. 1.Bureau of Economic Geology, Jackson School of GeosciencesThe University of Texas at AustinAustinUSA

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