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Stability of flow in a model of a hydrothermal system

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dc.contributor.authorSutton, Frances M
dc.date.accessioned2011-06-21T01:54:28Z
dc.date.accessioned2022-10-26T20:52:53Z
dc.date.available2011-06-21T01:54:28Z
dc.date.available2022-10-26T20:52:53Z
dc.date.copyright1969
dc.date.issued1969
dc.description.abstractA model of a geothermal system is described. The critical Rayleigh number for convective flow in this model is found for two cases: first when the system is closed, and secondly when there is a small net upward through flow. The equations for the isotherms and streamlines at marginal stability are found for the first case.en_NZ
dc.formatpdfen_NZ
dc.identifier.urihttps://ir.wgtn.ac.nz/handle/123456789/24890
dc.languageen_NZ
dc.language.isoen_NZ
dc.publisherTe Herenga Waka—Victoria University of Wellingtonen_NZ
dc.rights.holderAll rights, except those explicitly waived, are held by the Authoren_NZ
dc.rights.licenseAuthor Retains Copyrighten_NZ
dc.rights.urihttps://www.wgtn.ac.nz/library/about-us/policies-and-strategies/copyright-for-the-researcharchive
dc.subjectFluid mathematicsen_NZ
dc.subjectMathematicsen_NZ
dc.titleStability of flow in a model of a hydrothermal systemen_NZ
dc.typeTexten_NZ
thesis.degree.disciplineMathematicsen_NZ
thesis.degree.grantorTe Herenga Waka—Victoria University of Wellingtonen_NZ
thesis.degree.levelMastersen_NZ
thesis.degree.nameMaster of Scienceen_NZ
vuwschema.type.vuwAwarded Research Masters Thesisen_NZ

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