Research Article
Estimating the Climate-Controlled Soil Parameters and the Distorted Mound Shape for Analysis of Stiffened Rafts on Expansive Soils
Table 1
Average properties for expansive soils at different locations in the KSA.
| No. | Location | Soil type | USCS group symbol | Consistency limits (%) | Suction parameters (bars) | Slope of SWRC (kPa or pF) units | In situ water content | % Clay | LL | PL | PI | A | B | B = (dh/dw) | (%) | (%) |
| 1 | Tayma | Silty shale | CL–ML | 38 | 27 | 13 | 1.85 | −0.057 | −5.70 | 2.3 | 23 | 2 | Tabuk | Clay shale | MH | 61 | 27 | 34 | 1.61 | −0.025 | −2.50 | 4.5 | 45 | 3 | Al-Ghat | Silty shale | CL | 46 | 21 | 25 | 1.67 | −0.017 | −1.70 | 12 | 45 | 4 | Al-Ghat | Clay shale | CH | 65 | 30 | 35 | 2.1 | −0.025 | −2.50 | 19 | 72 | 5 | Madina | Green clay | CH | 105 | 39 | 66 | 2.28 | −0.03 | −3.00 | 59.1 | 64 | 6 | Madina | White clay | CH | 82 | 37 | 45 | 2.34 | −0.045 | −4.50 | 33.1 | 68 | 7 | Hofuf | Calcareous clay | CH–MH | 60 | 24 | 36 | 2.16 | −0.033 | −3.30 | 14 | 37 |
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USCS, unified soil classification system; SWRC, soil–water retention curve.
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