Research Article
The Uniaxial Creep Characteristics of Red Sandstone under Dry-Wet Cycles
Table 4
Axial strain changes of the red sandstone’s creep (unit: 10−2).
| Red sandstone’s state | s = 1 | s = 2 | s = 3 | s = 4 | s = 5 | εa | εb | εa | εb | εa | εb | εa | εb | εa | εb |
| Dry state | 0.389 | 0.403 | 0.504 | 0.517 | 0.562 | 0.574 | 0.625 | 0.644 | 0.703 | 0.737 | Wet state | 0.599 | 0.621 | 0.692 | 0.722 | 0.789 | 0.816 | 0.888 | 0.931 | 0.993 | 1.086 | 3 dry-wet cycles | 0.700 | 0.745 | 0.901 | 0.978 | 1.016 | 1.236 | 1.517 | 1.811 | Destruction | 6 dry-wet cycles | 0.801 | 0.853 | 1.048 | 1.127 | 1.248 | 1.490 | Destruction | 9 dry-wet cycles | 1.110 | 1.169 | 1.402 | 1.484 | 1.615 | 1.928 | Destruction |
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εa denotes the initial strain value of each stage; εb denotes the end strain value of each stage; s is the loading stage; s = 1, 2, 3, 4, 5.
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