Properties of soils whose behaviour is shown on Figs 3 and 6
| Soil | Geological | Mechanics | |||||||
|---|---|---|---|---|---|---|---|---|---|
| D50: μm | <60 μm | <2 μm | CU | PI* | λ10† | Mtc | N | X | |
| Sand: Brasted | 240 | <2% | — | 2·3 | — | 0·050 | 1·29 | 0·35 | 2·8 |
| Sand: Changi | 320 | 0·4% | — | 2·0 | — | 0·106 | 1·33 | 0·33 | 3·7 |
| Sand: Erksak | 330 | 0·7% | — | 1·8 | — | 0·040 | 1·26 | 0·37 | 4·4 |
| Sand: Fraser River | 300 | ∼1% | — | 1·7 | — | 0·090 | 1·47 | 0·45 | 5·0 |
| Sand: Nerlerk | 270 | 1·7% | — | 1·9 | — | 0·053 | 1·26 | 0·38 | 4·2 |
| Sand: Ticino | 530 | 0% | — | 1·8 | — | 0·057 | 1·27 | 0·35 | 3·5 |
| Silt: Endako | 8 | 99% | 0% | 18 | 23% | 0·541 | 1·35 | 0·35 | 0·8 |
| Silt: Guin35f | 115 | 34% | 0% | 6 | — | 0·102 | 1·39 | 0·30 | 6·8 |
| Silt: TC1 | 60 | 55% | 15% | 90 | 5% | 0·105 | 1·52 | 0·35 | 8·2 |
| Silt: NCS | 10 | 97% | 10% | 6 | — | 0·225 | 1·34 | 0·35 | 2·6 |
| Clay: London | — | 100% | 50% | — | 52% | 0·340 | 0·86 | 0·00 | 1·5 |
| Clay: Weald | — | 100% | 40% | — | 25% | 0·198 | 0·86 | 0·15 | 2·5 |
| Soil | Geological | Mechanics | |||||||
|---|---|---|---|---|---|---|---|---|---|
| <60 μm | <2 μm | PI* | |||||||
| Sand: Brasted | 240 | <2% | — | 2·3 | — | 0·050 | 1·29 | 0·35 | 2·8 |
| Sand: Changi | 320 | 0·4% | — | 2·0 | — | 0·106 | 1·33 | 0·33 | 3·7 |
| Sand: Erksak | 330 | 0·7% | — | 1·8 | — | 0·040 | 1·26 | 0·37 | 4·4 |
| Sand: Fraser River | 300 | ∼1% | — | 1·7 | — | 0·090 | 1·47 | 0·45 | 5·0 |
| Sand: Nerlerk | 270 | 1·7% | — | 1·9 | — | 0·053 | 1·26 | 0·38 | 4·2 |
| Sand: Ticino | 530 | 0% | — | 1·8 | — | 0·057 | 1·27 | 0·35 | 3·5 |
| Silt: Endako | 8 | 99% | 0% | 18 | 23% | 0·541 | 1·35 | 0·35 | 0·8 |
| Silt: Guin35f | 115 | 34% | 0% | 6 | — | 0·102 | 1·39 | 0·30 | 6·8 |
| Silt: TC1 | 60 | 55% | 15% | 90 | 5% | 0·105 | 1·52 | 0·35 | 8·2 |
| Silt: NCS | 10 | 97% | 10% | 6 | — | 0·225 | 1·34 | 0·35 | 2·6 |
| Clay: London | — | 100% | 50% | — | 52% | 0·340 | 0·86 | 0·00 | 1·5 |
| Clay: Weald | — | 100% | 40% | — | 25% | 0·198 | 0·86 | 0·15 | 2·5 |
Plasticity index (PI), which has nothing to do with the Theory of Plasticity
The property λ10 ( = 2·3λ) is the best fit over the stress range 40–400 kPa and is only given as an index of soil compressibility.
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