Research Article
Shear Properties and Mechanism of Freeze-Thaw Interface in Unsaturated Coarse-Grained Soil from Qinghai-Tibet Plateau
Figure 6
Variation of vertical displacement (δv) with the increasing shear displacement (δh). (a) = 9.0%, ρd = 1.9 g/cm3. (b) = 9.0%, σ = 200 kPa. (c) ρd = 2.0 g/cm3, σ = 200 kPa.
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| (b) |
| (c) |