Stability of flow in a model of a hydrothermal system

dc.contributor.author	Sutton, Frances M
dc.date.accessioned	2011-06-21T01:54:28Z
dc.date.accessioned	2022-10-26T20:52:53Z
dc.date.available	2011-06-21T01:54:28Z
dc.date.available	2022-10-26T20:52:53Z
dc.date.copyright	1969
dc.date.issued	1969
dc.identifier.uri	https://ir.wgtn.ac.nz/handle/123456789/24890
dc.description.abstract	A 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.format	pdf	en_NZ
dc.language	en_NZ
dc.language.iso	en_NZ
dc.publisher	Te Herenga Waka—Victoria University of Wellington	en_NZ
dc.title	Stability of flow in a model of a hydrothermal system	en_NZ
dc.type	Text	en_NZ
vuwschema.type.vuw	Awarded Research Masters Thesis	en_NZ
thesis.degree.discipline	Mathematics	en_NZ
thesis.degree.grantor	Te Herenga Waka—Victoria University of Wellington	en_NZ
thesis.degree.level	Masters	en_NZ
thesis.degree.name	Master of Science	en_NZ

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