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

Graduate Thesis Or Dissertation

Public Deposited

Citeable URL: https://ir.library.oregonstate.edu/concern/graduate_thesis_or_dissertations/jm214r09v

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Attribute Name	Values
Creator	Creel, Emory Myron Willett
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.
Resource Type	Masters Thesis
Date Available	2012-11-07T19:57:28+00:00
Date Issued	1995-12-06
Degree Level	Master's
Degree Name	Master of Arts (M.A.)
Degree Field	Physics
Degree Grantor	Oregon State University
Commencement Year	1996
Advisor	Griffiths, David J.
Academic Affiliation	Physics
Non-Academic Affiliation	Oregon State University. Graduate School
Subject	Porous materials -- Mathematical models Equations of state Shock waves -- Mathematical models
Rights Statement	Copyright Not Evaluated
Publisher	Oregon State University
Peer Reviewed	No
Language	English [eng]
Digitization Specifications	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.
Replaces	http://hdl.handle.net/1957/34912

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