2018
DOI: 10.30632/pjv59n1-2018a3
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Microstructural Investigation of Stress-Dependent Permeability in Tight-Oil Rocks

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Cited by 9 publications
(11 citation statements)
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“…The difference in the bead sizes results in a large difference in the absolute permeabilities of the strata; we estimate these using the Kozeny-Carman equation previously validated for bead packings, 57], where i ∈ {c, f } denotes the stratum, yielding k c ≈ 120 µm 2 and k f = 1.9 µm 2 . The permeability ratio is then k c /k f ≈ 60, comparable to the permeability ratio characterizing many naturally-occurring strata [40].…”
Section: Experimental Methodsmentioning
confidence: 90%
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“…The difference in the bead sizes results in a large difference in the absolute permeabilities of the strata; we estimate these using the Kozeny-Carman equation previously validated for bead packings, 57], where i ∈ {c, f } denotes the stratum, yielding k c ≈ 120 µm 2 and k f = 1.9 µm 2 . The permeability ratio is then k c /k f ≈ 60, comparable to the permeability ratio characterizing many naturally-occurring strata [40].…”
Section: Experimental Methodsmentioning
confidence: 90%
“…For example, these results could provide insight into the pathways taken by fluids during oil/gas recovery from a stratified reservoir or from microporous media [37,38,40,81,82]-an increasingly important application given society's rising energy demands. Another operationally similar application of our work will be to inform strategies for injecting fluid to recover nonaqueous contaminants from a stratified porous groundwater aquifer [37,83]-another critical application due to the increasing need for water security.…”
Section: Discussionmentioning
confidence: 99%
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“…Thus, we anticipate that this work will help guide imbibition processes in energy, environmental, and industrial applications that seek to control both t b and S O . Two prominent examples include pump-andtreat remediation of contaminated groundwater aquifers [40,82] and enhanced oil/gas recovery [40,41,43,83,84]; in both cases, injected wetting fluids are used to displace nonwetting fluid from heterogeneous subsurface media as quickly and effectively as possible. Other examples include controlling moisture wicking in building materials [21][22][23], layered microporous fabrics [85][86][87], and paper microfluidics [20,[88][89][90],…”
Section: E Comparison To An Averaged Modelmentioning
confidence: 99%
“…However, in many cases, porous media are not homogeneous. Instead, they can have parallel strata, characterized by different mean pore sizes, oriented along the direction of macroscopic fluid flow [40][41][42][43]; these can further impact the interfacial dynamics in complex ways [40][41][42][43][44][45][46][47]. Being able to predict and control imbibition in stratified porous media is therefore both fundamentally interesting and of critical practical importance.…”
Section: Introductionmentioning
confidence: 99%