Part 1 of 2
Consolidation of Soil
Last reviewed 16 Sept 2026 · 6 min read
What consolidation is
When load is applied to a saturated clay, water cannot escape quickly because permeability is very low. The load is first carried by excess pore water pressure; as water slowly drains, the load transfers to the soil skeleton, effective stress increases and the soil compresses. This time-dependent volume reduction due to expulsion of pore water is consolidation.
Total settlement of a foundation on clay:
- = immediate (elastic) settlement — distortion at constant volume.
- = primary consolidation settlement — expulsion of pore water (this chapter).
- = secondary compression — creep of the skeleton after excess pore pressure has dissipated.
Spring–piston analogy (Terzaghi)
A cylinder full of water with a spring (soil skeleton) and a piston with a small valve (low permeability):
- Instant of loading (): water carries the whole load; excess pore pressure ; spring stress unchanged.
- During drainage: water escapes through the valve; load gradually shifts to the spring; falls, rises.
- End of consolidation: ; the spring carries the full load; .
Oedometer (consolidation) test
An undisturbed specimen (typically 60–75 mm diameter, 20–25 mm thick) is confined laterally in a ring between porous stones (one-dimensional compression, drainage top and bottom). Loads are applied in stages (each usually doubled, held about 24 hours) and dial readings recorded with time. Results give void ratio at the end of each stage.
Compressibility parameters
- Coefficient of compressibility: (m²/kN)
- Coefficient of volume compressibility: (m²/kN)
- Compression index (slope of the virgin line on –log σ′):
- Swelling / recompression index (or ): slope of unloading–reloading line, typically to .
- Skempton's empirical relations: (undisturbed clays of low–medium sensitivity); (remoulded).
Normally consolidated and over-consolidated clays
- Preconsolidation pressure (or ) — the maximum effective stress the soil has experienced in its history. Found from the –log σ′ curve by Casagrande's graphical construction (point of maximum curvature, horizontal line, tangent, bisector, intersection with the extended virgin line).
- Normally consolidated (NC): present effective stress — soil is on the virgin line; highly compressible.
- Over-consolidated (OC): (past erosion, desiccation, lowered water table, glacial load); much less compressible for stresses below .
- Under-consolidated: still consolidating under its own recent weight ( less than the final value).
Consolidation settlement
Normally consolidated:
Over-consolidated, final stress ≤ :
Over-consolidated, final stress > :
Using : (for a small stress range).
and are taken at the middle of the layer (thick layers are divided into sub-layers).