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dc.contributorDepartment of Metallurgical Engineering, Ohio State Universityen_US
dc.contributorDepartment of Materials Science and Engineering, University of Florida
dc.contributor.authorShewmon, P. G.
dc.contributor.authorRhines, F. N.
dc.date.accessioned2013-08-09T13:56:09Z
dc.date.accessioned2015-06-10T20:13:06Z
dc.date.available2013-08-09T13:56:09Z
dc.date.available2015-06-10T20:13:06Z
dc.date.issued2013-08-09
dc.identifier.citationP. G. Shewmon, F. N. Rhines, "Rate of Self-Diffusion in Polycrystalline Magnesium", Transactions of the Metallurgical Society of AIME, 1954, Vol. 6, pp. 1021-1025en_US
dc.identifier.urihttp://hdl.handle.net/11115/140
dc.description.abstractThe determination of the self-diffusion coefficient of magnesium has been made possible recently by discovery of a radioactive isotope, Mg-28 having a half-life of 21.3 hr, and subject to manufacture in useful quantity.en_US
dc.rightsAttribution 3.0 United States*
dc.rights.urihttp://creativecommons.org/licenses/by/3.0/us/*
dc.subjectMgen_US
dc.subjectself-diffusion
dc.titleMg Self-Diffusionen_US
dc.typeDataseten_US
dc.typeDiffusion Mobilities


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Attribution 3.0 United States
Except where otherwise noted, this item's license is described as Attribution 3.0 United States