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The effect of void distribution on the Hugoniot state of porous media

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dc.contributor.advisor Griffiths, David J.
dc.creator Creel, Emory Myron Willett
dc.date.accessioned 2012-11-07T19:57:28Z
dc.date.available 2012-11-07T19:57:28Z
dc.date.copyright 1995-12-06
dc.date.issued 1995-12-06
dc.identifier.uri http://hdl.handle.net/1957/34912
dc.description Graduation date: 1996 en_US
dc.description.abstract Shocked porous granular material experiences pressure dependent compaction. D. John Pastine introduced a model in which the degree of compaction is dependent on the pressure induced by the shock wave, the shear strength of the material, and the distribution of void sizes. In the past, the model could only be approximated. Using computational techniques and higher speed computers, the response of this model to void size distributions may be displayed to a high degree of precision. en_US
dc.language.iso en_US en_US
dc.subject.lcsh Shock waves -- Mathematical models en_US
dc.subject.lcsh Equations of state en_US
dc.subject.lcsh Porous materials -- Mathematical models en_US
dc.title The effect of void distribution on the Hugoniot state of porous media en_US
dc.type Thesis/Dissertation en_US
dc.degree.name Master of Arts (M.A.) in Physics en_US
dc.degree.level Master's en_US
dc.degree.discipline Science en_US
dc.degree.grantor Oregon State University en_US
dc.description.digitization File scanned at 300 ppi (Monochrome, 8-bit Grayscale) using ScandAll PRO 1.8.1 on a Fi-6670 in PDF format. CVista PdfCompressor 4.0 was used for pdf compression and textual OCR. en_US
dc.description.peerreview no en_us

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