Table 1.

Properties of soils whose behaviour is shown on Figs 3 and 6 

SoilGeologicalMechanics
D50: μm<60 μm<2 μmCUPI*λ10MtcNX
Sand: Brasted240<2%2·30·0501·290·352·8
Sand: Changi3200·4%2·00·1061·330·333·7
Sand: Erksak3300·7%1·80·0401·260·374·4
Sand: Fraser River300∼1%1·70·0901·470·455·0
Sand: Nerlerk2701·7%1·90·0531·260·384·2
Sand: Ticino5300%1·80·0571·270·353·5
 
Silt: Endako899%0%1823%0·5411·350·350·8
Silt: Guin35f11534%0%60·1021·390·306·8
Silt: TC16055%15%905%0·1051·520·358·2
Silt: NCS1097%10%60·2251·340·352·6
 
Clay: London100%50%52%0·3400·860·001·5
Clay: Weald100%40%25%0·1980·860·152·5
*

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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