Table of Contents
ToggleThe Liquid Limit (LL) of soil is the water content at which soil changes from a plastic state to a liquid state. The cone penetration method as per IS 2720 (Part 5): 1985 is a reliable and repeatable laboratory method used mainly for fine-grained soils.
Liquid Limit is determined by plotting a graph between moisture content (%) and penetration (mm). The moisture content corresponding to 20 mm penetration is reported as Liquid Limit.
| Soil Use | Liquid Limit (%) | Suitability |
|---|---|---|
| Subgrade (Granular) | < 35 | Suitable |
| Subgrade (Clayey) | 35 – 50 | Conditional |
| Highly Plastic Clay | > 50 | Unsuitable |