FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2017603805> ?p ?o ?g. }

• W2017603805 endingPage "1544" @default.
• W2017603805 startingPage "1535" @default.
• W2017603805 abstract "In the present study we aim at investigating the instabilities in a plane bubble plume by means of two-way coupling simulations. The continuous phase motion is obtained by direct numerical solution of the Navier–Stokes equations forced by the presence of the bubbles. The collective effects induced by the presence of the bubbles are modeled by a spatiotemporal distribution of momentum. Time evolution of the dispersed phase is solved by Lagrangian tracking of all the bubbles. In the present study, the motion of the carrying fluid is initiated and driven by the induced buoyancy of bubbles released from a source located in an initially quiescent fluid layer. A quantitative analysis of the flow transition is thus investigated for several plume widths and for various fluid viscosities over a range of Grashof numbers based on the injection conditions. An analogy is drawn with buoyant single-phase flows for the steady laminar region. Following the similarity formulation of Fujii [Int. J. Heat Mass Transfer 6, 597 (1963)] under boundary layer approximations for free thermal plumes, the velocity profiles can be collapsed to a single self-similar plot. Nevertheless, this analogy with single-phase flow shows some discrepancies in the description of the transition. Numerical data emphasize that the key parameter controlling the height of transition is the Grashof number, which is based on injection conditions of the dispersed phase. Our results concur with the recent experiments of Alam and Arakeri [J. Fluid Mech. 254, 363 (1993)]. Although the Grashof number also determines the transition in thermal plumes [Wakitani and Yosinobu, Fluid Dyn. Res. 2, 363 (1988)], the two-phase configuration is more unstable. These new results underline the important role played by the slip velocity of the bubbles in plume stability. Indeed, it tends to delay the plume transition when the slip velocity increases and approaches the buoyancy-induced velocity. This feature should also be related to the lack of diffusion by the bubble cloud in the Lagrangian transport of the density gradient." @default.
• W2017603805 created "2016-06-24" @default.
• W2017603805 creator A5010466986 @default.
• W2017603805 creator A5042475469 @default.
• W2017603805 creator A5054664973 @default.
• W2017603805 date "2003-05-02" @default.
• W2017603805 modified "2023-09-23" @default.
• W2017603805 title "Two-way coupling simulations of instabilities in a plane bubble plume" @default.
• W2017603805 cites W1985613524 @default.
• W2017603805 cites W1995231460 @default.
• W2017603805 cites W1995566341 @default.
• W2017603805 cites W2004834212 @default.
• W2017603805 cites W2006430937 @default.
• W2017603805 cites W2007257200 @default.
• W2017603805 cites W2007543823 @default.
• W2017603805 cites W2011138124 @default.
• W2017603805 cites W2024490349 @default.
• W2017603805 cites W2025920130 @default.
• W2017603805 cites W2027268413 @default.
• W2017603805 cites W2027967353 @default.
• W2017603805 cites W2030490508 @default.
• W2017603805 cites W2046150917 @default.
• W2017603805 cites W2059402367 @default.
• W2017603805 cites W2070828334 @default.
• W2017603805 cites W2080900618 @default.
• W2017603805 cites W2083636270 @default.
• W2017603805 cites W2084969588 @default.
• W2017603805 cites W2091147009 @default.
• W2017603805 cites W2095488577 @default.
• W2017603805 cites W2104741465 @default.
• W2017603805 cites W2111432870 @default.
• W2017603805 cites W2113006754 @default.
• W2017603805 cites W2114038989 @default.
• W2017603805 cites W2117002426 @default.
• W2017603805 cites W2122430579 @default.
• W2017603805 cites W2137783180 @default.
• W2017603805 cites W2147104524 @default.
• W2017603805 cites W2164622024 @default.
• W2017603805 doi "https://doi.org/10.1063/1.1566754" @default.
• W2017603805 hasPublicationYear "2003" @default.
• W2017603805 type Work @default.
• W2017603805 sameAs 2017603805 @default.
• W2017603805 citedByCount "17" @default.
• W2017603805 countsByYear W20176038052012 @default.
• W2017603805 countsByYear W20176038052015 @default.
• W2017603805 countsByYear W20176038052016 @default.
• W2017603805 countsByYear W20176038052017 @default.
• W2017603805 countsByYear W20176038052019 @default.
• W2017603805 crossrefType "journal-article" @default.
• W2017603805 hasAuthorship W2017603805A5010466986 @default.
• W2017603805 hasAuthorship W2017603805A5042475469 @default.
• W2017603805 hasAuthorship W2017603805A5054664973 @default.
• W2017603805 hasConcept C111603439 @default.
• W2017603805 hasConcept C121332964 @default.
• W2017603805 hasConcept C130230704 @default.
• W2017603805 hasConcept C13027520 @default.
• W2017603805 hasConcept C182748727 @default.
• W2017603805 hasConcept C196558001 @default.
• W2017603805 hasConcept C2775840915 @default.
• W2017603805 hasConcept C538625479 @default.
• W2017603805 hasConcept C57879066 @default.
• W2017603805 hasConcept C74650414 @default.
• W2017603805 hasConcept C76563973 @default.
• W2017603805 hasConcept C90278072 @default.
• W2017603805 hasConcept C97355855 @default.
• W2017603805 hasConceptScore W2017603805C111603439 @default.
• W2017603805 hasConceptScore W2017603805C121332964 @default.
• W2017603805 hasConceptScore W2017603805C130230704 @default.
• W2017603805 hasConceptScore W2017603805C13027520 @default.
• W2017603805 hasConceptScore W2017603805C182748727 @default.
• W2017603805 hasConceptScore W2017603805C196558001 @default.
• W2017603805 hasConceptScore W2017603805C2775840915 @default.
• W2017603805 hasConceptScore W2017603805C538625479 @default.
• W2017603805 hasConceptScore W2017603805C57879066 @default.
• W2017603805 hasConceptScore W2017603805C74650414 @default.
• W2017603805 hasConceptScore W2017603805C76563973 @default.
• W2017603805 hasConceptScore W2017603805C90278072 @default.
• W2017603805 hasConceptScore W2017603805C97355855 @default.
• W2017603805 hasIssue "6" @default.
• W2017603805 hasLocation W20176038051 @default.
• W2017603805 hasOpenAccess W2017603805 @default.
• W2017603805 hasPrimaryLocation W20176038051 @default.
• W2017603805 hasRelatedWork W1996050661 @default.
• W2017603805 hasRelatedWork W1998930801 @default.
• W2017603805 hasRelatedWork W2025465266 @default.
• W2017603805 hasRelatedWork W2088093498 @default.
• W2017603805 hasRelatedWork W2089773471 @default.
• W2017603805 hasRelatedWork W2092925746 @default.
• W2017603805 hasRelatedWork W2103749632 @default.
• W2017603805 hasRelatedWork W2161624991 @default.
• W2017603805 hasRelatedWork W2284977116 @default.
• W2017603805 hasRelatedWork W37290958 @default.
• W2017603805 hasVolume "15" @default.
• W2017603805 isParatext "false" @default.
• W2017603805 isRetracted "false" @default.
• W2017603805 magId "2017603805" @default.
• W2017603805 workType "article" @default.