Abstract
Journal of the American Ceramic SocietyVolume 51, Issue 8 p. 465-467 Porosity Dependence of Sound Velocity and Poisson's Ratio for Polycrystalline MgO Determined by Resonant Sphere Method NAOHIRO SOGA, NAOHIRO SOGASearch for more papers by this authorEDWARD SCHREIBER, EDWARD SCHREIBERSearch for more papers by this author NAOHIRO SOGA, NAOHIRO SOGASearch for more papers by this authorEDWARD SCHREIBER, EDWARD SCHREIBERSearch for more papers by this author First published: August 1968 https://doi.org/10.1111/j.1151-2916.1968.tb11922.xCitations: 23 Contribution No. 1224 from Lamont Geoogical Observatory. Supported by the Air Force Materials Laboratory, Research Technology Division, Air Force Systems Command, United States Air Force, under Contract AF 33(615)-1700. At the time this work was done, the writers were research associates, Lamont Geological Observatory, Columbia University, Palisades, New York 10964. N. Soga is now assistant professor, Space Science and Mechanical Engineering, Rice University, Houston, Texas 77001. E. Schreiber is now visiting associate in geophysics, California Institute of Technology, Pasadena. California 91106. Obtained from the Avco Corporation through the Air Force Materials Laboratory. AboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinkedInRedditWechat No abstract is available for this article.Citing Literature Volume51, Issue8August 1968Pages 465-467 RelatedInformation
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