Please use this identifier to cite or link to this item: https://hdl.handle.net/11681/2747
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dc.contributor.authorButkovich, Theodore R.-
dc.date.accessioned2016-03-14T19:23:27Z-
dc.date.available2016-03-14T19:23:27Z-
dc.date.issued1957-12-
dc.identifier.urihttp://hdl.handle.net/11681/2747-
dc.descriptionResearch Report-
dc.descriptionSummary: Experiments were conducted on natural and artificial single ice crystals, commercial ice, snow-ice, and a glacial single crystal at temperatures from 0°C to -30°C to determine the effect of orientation on the linear thermal expansion coefficients. The orientation of the c-axis, the type of ice (whether single or polycrystalline), and the grain size did not appreciably affect the values of the coefficient; ice was practically isotropic with respect to thermal expansion at the temperatures tested. There was a steady decrease of the expansion coefficient with succeeding measurement on the same specimen, a phenomenon attributable to slow annealing. The ratio of the specific heat at constant pressure to that at constant volume 1.030 from 0°C to -30°C. Gruneisen’s constant was found to be about 0.78 and independent of temperature. An equation expressing the average coefficient of linear thermal expansion of ice of any type or orientation is presented.-
dc.publisherU.S. Army Snow, Ice, and Permafrost Research Establishment.-
dc.publisherEngineer Research and Development Center (U.S.)-
dc.relationhttp://acwc.sdp.sirsi.net/client/en_US/search/asset/1020580-
dc.relation.ispartofseriesResearch report (U.S. Army Snow-
dc.rightsApproved for public release; distribution is unlimited.-
dc.sourceThis Digital Resource was created from scans of the Print Resource-
dc.subjectIce-
dc.subjectIce crystals-
dc.subjectIce thermal properties-
dc.subjectSnow ice-
dc.subjectThermal expansion-
dc.subjectCoefficients-
dc.titleLinear thermal expansion of ice-
dc.typeReporten_US
Appears in Collections:Research Report

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