Soil is a three-phase material consisting of:
The total volume: V = Vs + Vv = Vs + Vw + Va
In a fully saturated soil → Va = 0 (voids filled with water only) In a completely dry soil → Vw = 0
Ratio of volume of voids to volume of solids.
e = Vv / Vs
Ratio of volume of voids to total volume.
n = Vv / V = e / (1 + e)
e = n / (1 - n)
Range: 0 < n < 1 (expressed as % or fraction)
Ratio of volume of water to volume of voids.
S = Vw / Vv × 100 (%)
ac = Va / V = n(1 - S)
av = Va / Vs = e(1 - S)
Total weight: W = Ws + Ww (weight of air is negligible)
Ratio of weight of water to weight of solids.
w = Ww / Ws × 100 (%)
S × e = w × Gs
Where S = degree of saturation (decimal), e = void ratio, w = water content (decimal), Gs = specific gravity of solids.
This single formula connects all four key parameters. Memorise it without fail.
γw = unit weight of water = 9.81 kN/m³ ≈ 10 kN/m³ (for GATE approximations)
γt = W / V = Gs·γw·(1 + w) / (1 + e)
γd = Ws / V = Gs·γw / (1 + e) = γt / (1 + w)
γsat = (Gs + e)·γw / (1 + e)
γ' = γsat - γw = (Gs - 1)·γw / (1 + e)
| Type | Formula | Range (kN/m³) |
|---|---|---|
| γdry | Gs·γw / (1+e) | 14 - 18 |
| γbulk | Gs·γw·(1+w) / (1+e) | 16 - 22 |
| γsat | (Gs+e)·γw / (1+e) | 18 - 23 |
| γ' | γsat - γw | 8 - 13 |
Gs = γs / γw = Ws / (Vs × γw)
| Soil Type | Typical Gs |
|---|---|
| Sand | 2.63 - 2.67 |
| Gravel | 2.65 - 2.68 |
| Clay | 2.68 - 2.80 |
| Organic soil / Peat | 1.30 - 1.90 |
| Default assumed value | 2.65 or 2.67 |
| Parameter | Primary Formula | Secondary Formula |
|---|---|---|
| Void Ratio (e) | e = Vv/Vs | e = n/(1-n) |
| Porosity (n) | n = Vv/V | n = e/(1+e) |
| Saturation (S) | S = Vw/Vv | Se = wGs |
| Water Content (w) | w = Ww/Ws | w = Se/Gs |
| Air Content (ac) | ac = Va/V | ac = n(1-S) |
| Dry Unit Weight (γd) | γd = Ws/V | γd = γt/(1+w) |
| Bulk Unit Weight (γt) | γt = W/V | γt = Gs·γw·(1+w)/(1+e) |
| Saturated (γsat) | (Gs+e)·γw/(1+e) | γd + n·γw |
| Buoyant (γ') | γsat - γw | (Gs-1)·γw/(1+e) |
Used only for granular soils (sands and gravels). Also called Density Index (ID).
Dr = (emax - e) / (emax - emin) × 100 (%)
Also expressed in terms of dry unit weight:
Dr = [(γd - γd,min) / (γd,max - γd,min)] × (γd,max / γd) × 100 (%)
| Dr (%) | State |
|---|---|
| 0 - 15 | Very Loose |
| 15 - 35 | Loose |
| 35 - 65 | Medium Dense |
| 65 - 85 | Dense |
| 85 - 100 | Very Dense |
Note: emax → γd,min (loosest state); emin → γd,max (densest state)
| 1. What are volume relationships in soil mechanics? | ![]() |
| 2. How do weight and mass relationships affect soil mechanics? | ![]() |
| 3. What is the significance of the GATE Star Formula in soil mechanics? | ![]() |
| 4. How is specific gravity (Gs) defined in the context of soil? | ![]() |
| 5. What is relative density (Dr) and why is it important in soil mechanics? | ![]() |