Problem Statement (GATE Exam)
A sandy stratum has the following properties:
- Natural bulk unit weight (\( \gamma \)) = 18.54 kN/m³
- Water content (\( w \)) = 8%
- Specific gravity (\( G \)) = 2.66
- Mould volume = 300 cm³
- Loose dry mass = 480 g
- Dense dry mass = 570 g
Determine the density index (\( I_D \)) of the sand.
Solution
1. Convert Given Data
- \( \gamma_w = 9.81 \, \text{kN/m}^3 \)
- Mould volume = 0.0003 m³
- Loose dry density: \( \rho_{d\text{-loose}} = \frac{480}{300} = 1.6 \, \text{g/cm}^3 = 15.696 \, \text{kN/m}^3 \)
- Dense dry density: \( \rho_{d\text{-dense}} = \frac{570}{300} = 1.9 \, \text{g/cm}^3 = 18.639 \, \text{kN/m}^3 \)
2. Calculate Natural Dry Unit Weight
\( \gamma_d = \frac{\gamma}{1 + w} = \frac{18.54}{1.08} = 17.167 \, \text{kN/m}^3 \)
3. Determine Void Ratios
Natural void ratio: \( e = \frac{G\gamma_w}{\gamma_d} – 1 = \frac{2.66 \times 9.81}{17.167} – 1 = 0.519 \)
Max void ratio (loose): \( e_{\text{max}} = \frac{G\gamma_w}{\gamma_{d\text{-loose}}} – 1 = \frac{2.66 \times 9.81}{15.696} – 1 = 0.662 \)
Min void ratio (dense): \( e_{\text{min}} = \frac{G\gamma_w}{\gamma_{d\text{-dense}}} – 1 = \frac{2.66 \times 9.81}{18.639} – 1 = 0.400 \)
4. Calculate Density Index
\( I_D = \frac{e_{\text{max}} – e}{e_{\text{max}} – e_{\text{min}}} \times 100 = \frac{0.662 – 0.519}{0.662 – 0.400} \times 100 = 54.58\% \)
Final Result:
- Density Index (\( I_D \)) = 54.6%
Explanation
Critical Steps:
- Conversion between mass and unit weight considering mould volume
- Void ratio calculation using dry unit weight relationships
- Density index formula application with extreme void ratios
Physical Meaning
1. Density Index (54.6%):
Indicates medium-dense sand condition (40-70% range)
2. Engineering Significance:
- Affects bearing capacity and settlement characteristics
- Helps predict liquefaction potential during earthquakes
- Guides compaction requirements for construction
3. Void Ratio Analysis:
The natural void ratio (0.519) lies between loose (0.662) and dense (0.400) states, showing moderate compaction in situ.




