Difficulty: Easy
Correct Answer: liquid limit
Explanation:
Introduction / Context:
The consistency of fine-grained soils changes with water content. Atterberg limits define key transition points between the liquid, plastic, semi-solid, and solid states. The threshold at which a soil stops flowing like a viscous liquid and just begins to sustain a minute shear resistance is fundamental for classification and for predicting field behavior such as workability and settlement.
Given Data / Assumptions:
Concept / Approach:
The liquid limit (LL) is the water content at which soil changes from a liquid-like state to a plastic state. In the lab, LL is determined by standardized methods (e.g., Casagrande cup or cone penetrometer) that correspond to a very low shear strength. This boundary is used with the plastic limit to compute plasticity index PI = LL - PL, a key classifier in systems like USCS and BIS/IS codes.
Step-by-Step Solution:
Verification / Alternative check (if short method exists):
In practice, the cone penetrometer LL test targets a specific penetration at which the soil’s undrained shear strength is about 1.7–2.0 kPa, aligning with the “small shear strength” description.
Why Other Options Are Wrong:
Plastic limit — boundary between plastic and semi-solid, not liquid behavior.
Shrinkage limit — boundary below which further drying does not reduce volume.
Permeability limit/consistency limit — not standard Atterberg terms defining this transition.
Common Pitfalls (misconceptions, mistakes):
Confusing LL with PL; assuming LL is a fixed property independent of test method; ignoring sensitivity of LL to sample remolding and salts.
Final Answer:
liquid limit
Discussion & Comments