Abstract
Two problems, a borehole subject to a non-hydrostatic far-field stress and a pressurized crack, are examined within the framework of Biot's theory of poroelasticity. The significance of the coupled diffusion-deformation theory is demonstrated, and the implications of these effects in rock mechanics applications are discussed.
| Original language | English (US) |
|---|---|
| Pages | 575-584 |
| Number of pages | 10 |
| State | Published - 1987 |
| Externally published | Yes |
| Event | 28th U.S. Symposium on Rock Mechanics, USRMS 1987 - Tucson, United States Duration: Jun 29 1987 → Jul 1 1987 |
Other
| Other | 28th U.S. Symposium on Rock Mechanics, USRMS 1987 |
|---|---|
| Country/Territory | United States |
| City | Tucson |
| Period | 6/29/87 → 7/1/87 |
Bibliographical note
Publisher Copyright:© 28th U.S. Symposium on Rock Mechanics, USRMS 1987. All rights reserved.
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