4.7 Article

Critical pore radius and transport properties of disordered hard- and overlapping-sphere models

期刊

PHYSICAL REVIEW E
卷 104, 期 1, 页码 -

出版社

AMER PHYSICAL SOC
DOI: 10.1103/PhysRevE.104.014127

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资金

  1. Princeton University Innovation Fund for New Ideas in the Natural Sciences
  2. Air Force Office of Scientific Research Program on Mechanics of Multifunctional Materials and Microsystems [FA9550-18-1-0514]
  3. Volkswagenstiftung via the Experiment-Projekt Mecke

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Transport properties of porous media are closely related to their pore-space microstructures, with the critical pore radius 8c and the second moment of the pore size (82) serving as key length scales. The alternative estimate of fluid permeability based on (82) is promising for porous media with a well-connected pore space. Models with effectively hyperuniformity tend to exhibit lower fluid permeability values compared to nonhyperuniform counterparts.
Transport properties of porous media are intimately linked to their pore-space microstructures. We quantify geometrical and topological descriptors of the pore space of certain disordered and ordered distributions of spheres, including pore-size functions and the critical pore radius 8c. We focus on models of porous media derived from maximally random jammed sphere packings, overlapping spheres, equilibrium hard spheres, quantizer sphere packings, and crystalline sphere packings. For precise estimates of the percolation thresholds, we use a strict relation of the void percolation around sphere configurations to weighted bond percolation on the corresponding Voronoi networks. We use the Newman-Ziff algorithm to determine the percolation threshold using universal properties of the cluster size distribution. The critical pore radius 8c is often used as the key characteristic length scale that determines the fluid permeability k. A recent study [Torquato, Adv. Wat. Resour. 140, 103565 (2020)] suggested for porous media with a well-connected pore space an alternative estimate of k based on the second moment of the pore size (82), which is easier to determine than 8c. Here, we compare 8c to the second moment of the pore size (82), and indeed confirm that, for all porosities and all models considered, 8c2 is to a good approximation proportional to (82). However, unlike (82), the permeability estimate based on 8c2 does not predict the correct ranking of k for our models. Thus, we confirm (82) to be a promising candidate for convenient and reliable estimates of the fluid permeability for porous media with a well-connected pore space. Moreover, we compare the fluid permeability of our models with varying degrees of order, as measured by the v order metric. We find that (effectively) hyperuniform models tend to have lower values of k than their nonhyperuniform counterparts. Our findings could facilitate the design of porous media with desirable transport properties via targeted pore statistics.

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