Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/112246
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dc.contributorDepartment of Civil and Environmental Engineering-
dc.creatorZhai, H-
dc.creatorTorres, JF-
dc.creatorZhao, Y-
dc.creatorXu, F-
dc.date.accessioned2025-04-08T00:43:39Z-
dc.date.available2025-04-08T00:43:39Z-
dc.identifier.issn0022-1120-
dc.identifier.urihttp://hdl.handle.net/10397/112246-
dc.language.isoenen_US
dc.publisherCambridge University Pressen_US
dc.rightsThis is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0), which permits unrestricted re-use, distribution and reproduction, provided the original article is properly cited.en_US
dc.rights© The Author(s), 2024. Published by Cambridge University Press.en_US
dc.rightsThe following publication is available at https://dx.doi.org/10.1109/JSTARS.2024.3502461.en_US
dc.subjectBoundary layer stabilityen_US
dc.subjectBuoyancy-driven instabilityen_US
dc.subjectPlumes/thermalsen_US
dc.titleTransition of the thermal boundary layer and plume over an isothermal section-triangular roof : an experimental studyen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume998-
dc.identifier.doi10.1017/jfm.2024.789-
dcterms.abstractThe development of thermal boundary layers and plume near a section-Triangular roof under different isothermal heating conditions has been the focus of numerous numerical studies. However, flow transition in this type of flow has never been observed experimentally. Here, phase-shifting interferometry and thermistor measurements are employed to experimentally observe and quantify the flow transitions in a buoyancy-driven flow over an isothermal section-Triangular roof. Visualisation of temperature contours is conducted across a wide range of Rayleigh numbers from laminar at 103 to chaotic state at 4 × 106. Power spectral density of the temperature measurements reveals the type of bifurcations developing as the Rayleigh number is increased. This flow transition is characterised as a complex bifurcation route with the presence of two fundamental frequencies, a low and a high frequency. We found that the thermal stratification in the environment plays a significant role in the flow transition. The spatial development of flow is also quantitatively and qualitatively described. In addition to clarifying flow transition in experiments, the work demonstrates the implementation of phase-shifting interferometry and punctual temperature measurements for characterisation of near-field flow over a heated surface.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationJournal of fluid mechanics, 10 Nov. 2024, v. 998, A7-
dcterms.isPartOfJournal of fluid mechanics-
dcterms.issued2024-11-
dc.identifier.scopus2-s2.0-85209361264-
dc.identifier.eissn1469-7645-
dc.identifier.artnA7-
dc.description.validate202504 bcrc-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.fundingSourceOthersen_US
dc.description.fundingTextNational Natural Science Foundation of China; 2019 ANU Global Research Partnership Scheme for the project ‘Exchange on multiscale convective heat transfer’en_US
dc.description.pubStatusPublisheden_US
dc.description.oaCategoryCCen_US
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