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contributor authorA. T. Kirkpatrick
contributor authorD. H. Johnson
contributor authorR. F. Gordon
date accessioned2017-05-08T23:23:22Z
date available2017-05-08T23:23:22Z
date copyrightAugust, 1986
date issued1986
identifier issn0199-6231
identifier otherJSEEDO-28191#214_1.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/101634
description abstractA solar pond can be used as a thermal energy source provided that convective instabilities do not occur. This paper experimentally examines the stability of a fluid layer with nonlinear salinity and temperature profiles. A nonlinear salt profile was set up in a fluid layer, and the water was heated by a solar radiation simulator. Three stability experiments were conducted. Instabilities occurred at the location of the weakest salinity gradient, and were confined to a thin region, as predicted by theory. A local length scale was used to produce a stability parameter, the ratio of thermal to solute Rayleigh numbers. It is shown that for nonconstant solute and temperature gradients, the appropriate length scale is based on the radius of curvature of the salinity distribution. With this chocie of a length scale, good agreement was found between theory and experiment for the onset of an instability.
publisherThe American Society of Mechanical Engineers (ASME)
titleDouble Diffusive Natural Convection in Solar Ponds With Nonlinear Temperature and Salinity Profiles
typeJournal Paper
journal volume108
journal issue3
journal titleJournal of Solar Energy Engineering
identifier doi10.1115/1.3268095
journal fristpage214
journal lastpage218
identifier eissn1528-8986
keywordsTemperature
keywordsNatural convection
keywordsSolar energy
keywordsStability
keywordsFluids
keywordsSolar radiation
keywordsThermal energy
keywordsRayleigh number
keywordsGradients
keywordsTemperature profiles
keywordsWater AND Temperature gradients
treeJournal of Solar Energy Engineering:;1986:;volume( 108 ):;issue: 003
contenttypeFulltext


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