Research Article
Analysis and Prediction of Stable Height of Capillary Water Rising under Unsaturated Subgrade Soil
Table 3
The physical indices of the fine-grained soils.
| Sample number | Particle size composition (%) | Dry density/g.cm−3 | WP (%) | WL (%) | IP (%) | Soil type | 2∼0.5 | 0.5∼0.25 | 0.25∼ 0.075 | 0.075∼ 0.05 | 0.05∼ 0.01 | 0.01∼ 0.005 | 0.005∼ 0.002 | <0.002 |
| 7# | 0.21 | 0.34 | 0.64 | 11.86 | 44.46 | 17.78 | 16.80 | 7.91 | 1.556 | 26.3 | 52.7 | 26.4 | High liquid limit clay | 8# | 0.28 | 0.41 | 0.62 | 18.75 | 47.38 | 13.82 | 13.82 | 4.92 | 1.683 | 22.2 | 40.3 | 18.1 | Low liquid limit clay | 9# | 1.85 | 9.04 | 14.41 | 18.75 | 42.38 | 9.00 | 4.57 | - | 1.719 | 20.7 | 33.5 | 12.8 | Low liquid limit clay | 10# | — | 9.05 | 24.50 | 27.24 | 34.82 | 3.06 | 1.33 | - | 1.755 | 18.8 | 28.1 | 9.3 | Low liquid limit silt |
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