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Comparison of Klinkenberg-corrected gas permeability and water permeability in sedimentary rocks

https://hiroshima.repo.nii.ac.jp/records/2007135
https://hiroshima.repo.nii.ac.jp/records/2007135
e3458374-1f3f-48c3-af7a-2097c597fade
名前 / ファイル ライセンス アクション
IntJRockMechMinSci_46_229.pdf IntJRockMechMinSci_46_229.pdf (757.7 KB)
Item type デフォルトアイテムタイプ_(フル)(1)
公開日 2023-03-18
タイトル
タイトル Comparison of Klinkenberg-corrected gas permeability and water permeability in sedimentary rocks
言語 en
作成者 Tanikawa, Wataru

× Tanikawa, Wataru

en Tanikawa, Wataru

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Shimamoto, Toshihiko

× Shimamoto, Toshihiko

en Shimamoto, Toshihiko

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アクセス権
アクセス権 open access
アクセス権URI http://purl.org/coar/access_right/c_abf2
権利情報
権利情報 Copyright (c) 2008 Elsevier Ltd
主題
主題Scheme Other
主題 Gas permeability
主題
主題Scheme Other
主題 Water permeability
主題
主題Scheme Other
主題 Klinkenberg effect
主題
主題Scheme Other
主題 Sedimentary rock
主題
主題Scheme NDC
主題 450
内容記述
内容記述 Quick measurements of permeability can be made by using gas as the pore fluid. To apply gas permeability data to the evaluation of water permeability, the difference between gas and water permeabilities needs to be assessed. We measured intrinsic permeability of sedimentary rocks from the western foothills of Taiwan by using nitrogen gas and distilled water as pore fluids in effective-pressure cycling tests at room temperature. The observed difference in gas and water permeabilities was analyzed in view of the Klinkenberg effect. This effect is due to the slip flow of gases at pore walls, which enhances gas flow when pore sizes are very small. Our experimental results showed that (1) gas permeability was larger than water permeability by several times to one order of magnitude, (2) gas permeability increased with increasing pore pressure, and (3) water permeability increased slightly as the pore-pressure gradient across the specimen increased. Results (1) and (2) can be explained quantitatively by an empirical power law in relation to the Klinkenberg constant b that is applicable in low permeable range. This correlation enables us to estimate water permeability from gas permeability. The Klinkenberg effect is important when permeability is lower than 10-18 m2 and at low pore-pressure differentials, and correction for the effect is essential to estimate water permeability from gas permeability measurement data. A simplified Bingham flow model for water can partially explain the trend of result (3), though non-Darcy flow behavior or inertial forces of water-rock interaction are needed to account for the observed deviation from Darcy's law.
言語 en
出版者
出版者 Elsevier Science Ltd.
言語
言語 eng
資源タイプ
資源タイプ識別子 http://purl.org/coar/resource_type/c_6501
資源タイプ journal article
出版タイプ
出版タイプ AO
出版タイプResource http://purl.org/coar/version/c_b1a7d7d4d402bcce
関連情報
識別子タイプ DOI
関連識別子 10.1016/j.ijrmms.2008.03.004
関連情報
識別子タイプ DOI
関連識別子 http://dx.doi.org/10.1016/j.ijrmms.2008.03.004
収録物識別子
収録物識別子タイプ ISSN
収録物識別子 1365-1609
収録物識別子
収録物識別子タイプ NCID
収録物識別子 AA1116472X
開始ページ
開始ページ 229
書誌情報 International Journal of Rock Mechanics and Mining Sciences
International Journal of Rock Mechanics and Mining Sciences

巻 46, 号 2, p. 229-238, 発行日 2009-02
旧ID 25979
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