Saturated Unit Weight

γsat=(Gs+e) γw1+e\gamma_{sat} = \frac{(G_s + e)\,\gamma_w}{1 + e}

Worked example: Gs = 2.68, e = 0.70 → γsat = 19.50 kN/m³ — press Try an example to run it live, then adjust anything.

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Saturated Unit Weight explained

γwGseγsat

Take a unit volume of solids: it weighs GsγwG_s \gamma_w and occupies 1, while the voids occupy e and — if saturated — hold eγwe\gamma_w of water. Total weight (Gs+e)γw(G_s + e)\gamma_w over total volume (1 + e) gives the saturated unit weight directly. For GsG_s = 2.68, e = 0.70 and γw\gamma_w = 9.81 kN/m³ that is (3.38 × 9.81) ÷ 1.70 = 19.50 kN/m³. In imperial units GsG_s = 2.65 with e = 0.55 and γw\gamma_w = 62.4 pcf gives (3.20 × 62.4) ÷ 1.55 = 128.8 pcf.

The trap is applying γsat\gamma_{\text{sat}} above the water table. Soil there is moist, not saturated, and its unit weight is lower — using γsat\gamma_{\text{sat}} for a whole profile overstates total stress and, worse, understates the effective stress ratio the strength depends on. The second trap is arithmetic laziness: γsat\gamma_{\text{sat}} is not γd+γw\gamma_d + \gamma_w. A denser soil holds less water, so as e falls γsat\gamma_{\text{sat}} rises while the water carried per unit volume falls. Run the numbers at e = 0.4 and e = 1.0 and watch the two effects part company.

Saturated Unit Weight formula

γsat=(Gs+e) γw1+e\gamma_{sat} = \frac{(G_s + e)\,\gamma_w}{1 + e}
Where
  • γsat\gamma_{sat}= Saturated unit weight (kN/m³)
  • GsG_s= Specific gravity of solids
  • ee= Void ratio
  • γw\gamma_w= Unit weight of water (kN/m³)