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. / Graduation date: 1996
| Identifer | oai:union.ndltd.org:ORGSU/oai:ir.library.oregonstate.edu:1957/34912 |
| Date | 06 December 1995 |
| Creators | Creel, Emory Myron Willett |
| Contributors | Griffiths, David J. |
| Source Sets | Oregon State University |
| Language | en_US |
| Detected Language | English |
| Type | Thesis/Dissertation |
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