Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/5814
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dc.contributor.authorYen, Yin-Chao.-
dc.contributor.authorTien, Chi, 1930--
dc.date.accessioned2016-03-21T21:08:40Z-
dc.date.available2016-03-21T21:08:40Z-
dc.date.issued1966-03-
dc.identifier.urihttp://hdl.handle.net/11681/5814-
dc.descriptionResearch Report-
dc.descriptionAbstract: Approximate solutions of temperature distribution and melting rate of ice have been obtained for the case where the mode of heat transfer is natural convection due to the thermal instability caused by the heated lower surface. Extensive numerical solutions were obtained for the ice-water system corresponding to various thermal conditions in terms of parameters defined as š–± āˆ†š–³= (š–³š—Œ - Tš—†) / (Tš—† -Tš—ˆ) and Ī¦ = š–«/š–¢š—‰ (Tš—† - Tš—ˆ), where š–³š—Œ is the temperature fo the heat source, Tš—† is the melting point of ice, Tš—ˆ is the initial temperature of ice, š–« is the latent heat of fusion, and š–¢š—‰ is the heat capacity of ice.-
dc.publisherCold Regions Research and Engineering Laboratory (U.S.)-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1013126-
dc.relation.ispartofseriesResearch report (Cold Regions Research and Engineering Laboratory (U.S.)) ; 185.-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectIce-
dc.subjectThermal properties-
dc.subjectIce melting-
dc.subjectThermal conductivity-
dc.subjectThermal conduction-
dc.subjectHeat conduction-
dc.subjectHeat transfer-
dc.subjectHeat transmission-
dc.subjectThawing-
dc.subjectThermal diffusivity-
dc.titleAn analytical investigation of a modified Stefan problem-
dc.typeReporten_US
Appears in Collections:Research Report

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