Difficulty: Easy
Correct Answer: natural water content minus plastic limit, divided by plasticity index
Explanation:
Introduction / Context:
Liquidity index LI situates a cohesive soil’s in-situ water content within its Atterberg limits. It is widely used for qualitative assessment of consistency, workability, and expected undrained strength. Values below zero indicate stiff to hard soils; values near one indicate very soft behavior approaching liquid limit.
Given Data / Assumptions:
Concept / Approach:
The standard definition is LI (%) = (w - PL) / PI * 100. This normalizes the natural water content relative to the plastic range. If LI = 0, w equals PL; if LI = 1, w equals LL. Practitioners correlate LI with field behavior (e.g., hand vane shear) and with settlement potential under loading.
Step-by-Step Solution:
Verification / Alternative check:
The consistency index Ic is complementary: Ic = (LL - w) / PI. Note that LI + Ic = 1 when expressed as fractions, providing a cross-check between reported values.
Why Other Options Are Wrong:
Options reversing signs or adding PL do not reflect the definition. Using LL - w corresponds to Ic, not LI.
Common Pitfalls:
Mixing percentage and decimal forms; using disturbed samples with moisture loss before testing; misreporting PI due to inconsistent LL/PL determinations.
Final Answer:
natural water content minus plastic limit, divided by plasticity index
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