Submerged (Buoyant) Unit Weight
Worked example: 19.5 kN/m³ saturated → γ′ = 9.69 kN/m³ — press Try an example to run it live, then adjust anything.
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Submerged (Buoyant) Unit Weight explained
Below the water table every grain is buoyed by the water it displaces, so the stress it hands down to the grain beneath is reduced by exactly per unit volume. A saturated soil at 19.5 kN/m³ therefore contributes only 19.5 − 9.81 = 9.69 kN/m³ to effective stress — barely half. Multiply γ′ by depth and you get effective stress directly, without the σ − u round trip, which is why field engineers carry γ′ in their heads (a handy 62.4 pcf subtraction: 128.8 − 62.4 = 66.4 pcf).
The trap is using γ′ for total stress, or for effective stress. Total stress needs the full saturated weight, because the water is physically there and pressing; effective stress needs the buoyant weight. Get them backwards and a 10 m submerged profile is off by a factor of two. The second trap is that buoyancy applies to structures too: a below-grade parking garage with a high water table can float, and the Chicago and Boston waterfront basements that had to be tied down with tension piles are monuments to somebody forgetting that a box full of air weighs less than the water it displaces.
Submerged (Buoyant) Unit Weight formula
- = Submerged unit weight (kN/m³)
- = Saturated unit weight (kN/m³)
- = Unit weight of water (kN/m³)
Missing one of these? Work it out first, then come back
- Submerged unit weight — Infinite Slope Factor of Safety with Slope-Parallel Seepage, Pore Water Pressure (u = γw zw)
- Saturated unit weight — Infinite Slope Factor of Safety with Slope-Parallel Seepage, Saturated Unit Weight
- Unit weight of water — Pore Water Pressure (u = γw zw), Saturated Unit Weight
Soil phase relations
8 formulasVoid ratio, porosity, saturation, water content and the dry, saturated and submerged unit weights of a three-phase soil.
The effective stress principle
4 formulasTotal vertical stress, pore water pressure and Terzaghi's σ′ = σ − u — the single idea the whole of soil mechanics rests on.