The total unit weight of the glacial outwash soil is 16 kN/m3. The specific gravity of soil particles of the soil is 2.67. The water content of the soil is 17%. Calculate:(a) Dry unit weight (b) Porosity(c) Void ratio (d) Degree of saturation

Soil Properties (GATE Exam 1998)

Problem Statement (GATE Exam 1998)

The total unit weight of the glacial outwash soil is 16 kN/m³. The specific gravity of soil particles is 2.67, and the water content of the soil is 17%. Calculate:

  1. Dry unit weight (\( \gamma_d \))
  2. Porosity (\( n \))
  3. Void ratio (\( e \))
  4. Degree of saturation (\( S \))

Solution

1. Given Data

  • Total unit weight (\( \gamma \)) = 16 kN/m³
  • Specific gravity (\( G \)) = 2.67
  • Water content (\( w \)) = 17% = 0.17
  • Unit weight of water (\( \gamma_w \)) = 9.81 kN/m³

2. Calculate Dry Unit Weight (\( \gamma_d \))

\( \gamma_d = \frac{\gamma}{1 + w} = \frac{16}{1 + 0.17} = \frac{16}{1.17} = 13.675 \, \text{kN/m³} \)

3. Calculate Void Ratio (\( e \))

\( e = \frac{G \cdot \gamma_w}{\gamma_d} – 1 \)
Substituting values: \( e = \frac{2.67 \cdot 9.81}{13.675} – 1 = \frac{26.2}{13.675} – 1 = 0.9153 \)

4. Calculate Porosity (\( n \))

\( n = \frac{e}{1 + e} = \frac{0.9153}{1 + 0.9153} = \frac{0.9153}{1.9153} = 0.4779 \times 100 = 47.79\% \)

5. Calculate Degree of Saturation (\( S \))

\( S = \frac{w \cdot G}{e} = \frac{0.17 \cdot 2.67}{0.9153} = \frac{0.4539}{0.9153} = 0.4959 \times 100 = 49.59\% \)
Results:
  • Dry unit weight (\( \gamma_d \)) = 13.675 kN/m³
  • Porosity (\( n \)) = 47.79%
  • Void ratio (\( e \)) = 0.9153
  • Degree of saturation (\( S \)) = 49.59%

Explanation

Key Steps:

  • Dry Unit Weight: Calculated to remove the influence of water content and represents the weight of solids per unit volume.
  • Void Ratio: Measures the volume of voids relative to the volume of solids, calculated using the dry unit weight, specific gravity, and unit weight of water.
  • Porosity: Indicates the proportion of the total volume occupied by voids, derived from the void ratio.
  • Degree of Saturation: Represents the fraction of voids filled with water, derived using water content, specific gravity, and void ratio.

Physical Meaning

1. Dry Unit Weight (13.675 kN/m³):

  • Represents the density of the soil in a completely dry state, essential for analyzing soil stability and compaction.

2. Void Ratio (0.9153):

  • A high void ratio indicates the soil is loosely packed, which could impact its strength and compressibility.

3. Porosity (47.79%):

  • Almost half of the soil volume consists of voids, which influences its permeability and storage capacity.

4. Degree of Saturation (49.59%):

  • Indicates that about half of the voids are filled with water, affecting the soil’s capillarity and suction potential.

Engineering Significance:

  • The dry unit weight helps in compaction tests to achieve desired soil strength.
  • The void ratio and porosity provide insights into the soil’s compactness and drainage properties.
  • The degree of saturation helps in analyzing the soil’s behavior under varying moisture conditions, crucial for foundation design.

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