Table 1 Basic experimental conditions for high-temperature rock specimens.
Serial number | High-temperature rock specimen number | Experimental boundary condition | Serial number | High-temperature rock specimen number | Experimental boundary condition/MPa |
---|---|---|---|---|---|
1 | A1 | T = 20 °C, uniaxial | 9 | B4 | T = 400 °C, triaxial, confining pressure σ3 = 25 |
2 | A2 | T = 150 °C, uniaxial | 10 | B5 | T = 500 °C, triaxial, confining pressure σ3 = 25 |
3 | A3 | T = 300, uniaxial | 11 | C1 | T = 20 °C, as the loading path shown in Fig. 3 |
4 | A4 | T = 400 °C, uniaxial | 12 | C2 | T = 150 °C, as the loading path shown in Fig. 3 |
5 | A5 | T = 500, uniaxial | 13 | C3 | T = 300 °C, as the loading path shown in Fig. 3 |
6 | B1 | T = 20 °C, triaxial, confining pressure σ3 = 25 | 14 | C4 | T = 400 °C, as the loading path shown in Fig. 3 |
7 | B2 | T = 150 °C, triaxial, confining pressure σ3 = 25 | 15 | C5 | T = 500 °C, as the loading path shown in Fig. 3 |
8 | B3 | T = 300, triaxial, confining pressure σ3 = 25 |