Correlation between surface area and Atterberg limits of fine-grained soils
As the water content is increased, the consistency of a fine-grained soil changes from a semi-solid state to a plastic state and finally to a liquid state. The plastic limit (PL) is the point at which the consistency, caused by the soil water content, is transformed from a semi-solid state to a plas...
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Veröffentlicht in: | Clays and clay minerals 2007-10, Vol.55 (5), p.519-523 |
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