Abstract
The paper describes an effort to match the measured pore pressure response induced by a heater located inside a borehole, in an intact saturated granitic rock mass. The effect of the heater is modelled by a combination of heat and fluid sources, which are singular solutions of the linear theory of thermoporoelasticity. It is shown that a single parameter, γ, which lumps several thermoporoelastic constants, controls the magnitude of the pore pressure induced by thermal loading.
| Original language | English (US) |
|---|---|
| Title of host publication | Proceedings of Engineering Mechanics |
| Publisher | ASCE |
| Pages | 44-47 |
| Number of pages | 4 |
| Volume | 1 |
| State | Published - Jan 1 1996 |
| Event | Proceedings of the 1996 11th Conference on Engineering Mechanics. Part 1 (of 2) - Fort Lauderdale, FL, USA Duration: May 19 1996 → May 22 1996 |
Other
| Other | Proceedings of the 1996 11th Conference on Engineering Mechanics. Part 1 (of 2) |
|---|---|
| City | Fort Lauderdale, FL, USA |
| Period | 5/19/96 → 5/22/96 |