What is excess pore water pressure?

Excess pore water pressure is a temporarily raised water pressure in the soil, caused when the ground is loaded or deformed faster than the water can escape. The gradual dissipation of that excess pressure is called consolidation.

How it arises

Saturated soil consists of grains with water in the pores between them. Load that soil and the load is initially carried by the pore water, not by the grain skeleton — water is barely compressible. In low-permeability soils such as clay and peat the water cannot escape quickly, so the water pressure rises.

As long as the water carries the load, the effective stress between the grains is low and the soil has little strength. Only once the water has drained does the grain skeleton take over the load, strength increases and settlement occurs.

Typical situations:

Why it concerns you

Related terms

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