Effect of pore-size distribution on unsaturated shear strength of residual soil from sedimentary Jurong formation
The residual soil from Sedimentary Jurong Formation is a weathering product of sedimentary rocks. Residual soils are often found in an unsaturated condition. The soil-water characteristic curve of the soil indicates how the mineral composition and weathering grade affect the pore-size distribution o...
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| Format: | Final Year Project (FYP) |
| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/10356/16055 |