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  1. J-1. 環日本海域環境研究センター
  2. j-1 10. 学術雑誌掲載論文
  3. 1. 査読済論文

Numerical analysis of re-oscillation and non-centrosymmetric convection in a porous enclosure due to opposing heat and mass fluxes on the vertical walls

http://hdl.handle.net/2297/20360
http://hdl.handle.net/2297/20360
d44d83bb-b730-4af9-986c-dc2b14e10e9b
名前 / ファイル ライセンス アクション
NA-PR-KIMURA-S-250.pdf NA-PR-KIMURA-S-250.pdf (558.5 kB)
Item type 学術雑誌論文 / Journal Article(1)
公開日 2017-10-05
タイトル
タイトル Numerical analysis of re-oscillation and non-centrosymmetric convection in a porous enclosure due to opposing heat and mass fluxes on the vertical walls
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
著者 Matsuda, Yoshio

× Matsuda, Yoshio

WEKO 10707
金沢大学研究者情報 20401896
研究者番号 20401896

Matsuda, Yoshio

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Yoneya, Michio

× Yoneya, Michio

WEKO 50780

Yoneya, Michio

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Suzuki, Akira

× Suzuki, Akira

WEKO 50781

Suzuki, Akira

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Kimura, Shigeo

× Kimura, Shigeo

WEKO 10640
e-Rad 70272953
研究者番号 70272953

Kimura, Shigeo

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Alavyoon, Farid

× Alavyoon, Farid

WEKO 50782

Alavyoon, Farid

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提供者所属
内容記述タイプ Other
内容記述 金沢大学環日本海域環境研究センターエコテクノロジー研究部門
書誌情報 International Communications in Heat and Mass Transfer

巻 37, 号 3, p. 250-255, 発行日 2010-03-01
ISSN
収録物識別子タイプ ISSN
収録物識別子 0735-1933
NCID
収録物識別子タイプ NCID
収録物識別子 AA10520556
DOI
関連タイプ isVersionOf
識別子タイプ DOI
関連識別子 10.1016/j.icheatmasstransfer.2009.11.008
出版者
出版者 Elsevier
抄録
内容記述タイプ Abstract
内容記述 Two peculiar convection patterns-re-oscillation and stable non-centrosymmetric convection-are observed when two-dimensional double-diffusive convection in a porous enclosure (aspect ratio = 1.5) is analysed numerically. The top and bottom walls of the enclosure are insulated; constant and opposing heat and mass fluxes are prescribed on the vertical walls. Re-oscillation occurs when the convection pattern changes from centrosymmetric to non-centrosymmetric. When the buoyancy ratio, which generates re-oscillation convection, is marginally lower, the convection pattern changes to stable non-centrosymmetric. These two convection patterns can be observed only for limited values of the Rayleigh number, Lewis number, and buoyancy ratio. © 2009 Elsevier Ltd. All rights reserved.
著者版フラグ
出版タイプ AM
出版タイプResource http://purl.org/coar/version/c_ab4af688f83e57aa