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When Solid Ground Turns to Liquid: Effective Stress

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In some earthquakes, firm ground suddenly behaves like a liquid — buildings tilt and sink, and water erupts from the soil. This alarming phenomenon, liquefaction, is explained by one of the most important ideas in soil mechanics: effective stress, the insight that soil strength comes not from all the weight it bears, but only from the part carried grain to grain.

Two Ways to Carry a Load

When weight presses on saturated soil, the load is shared between two things: the solid grains pressing against one another, and the water filling the pore spaces. Karl Terzaghi's crucial insight was that these carry the load differently — and that the soil's strength depends only on the portion borne by grain-to-grain contact, not on the water pressure.

Effective Stress

Effective stress is the part of the total load actually transmitted through the touching grains — the total stress minus the pressure of the pore water. It is this effective stress, not the total, that gives soil its strength and stiffness, because it is the grains pressing together that let soil resist being sheared apart. The water, by contrast, holds the grains slightly apart.

Sharing the load
Carried byEffect
Grain contactProvides strength
Pore water pressureReduces effective stress

The Danger of Rising Water Pressure

The principle carries a warning. If the pressure of the pore water rises — from an earthquake shaking saturated soil, heavy rain, or rapid loading — it takes over more of the load, and the effective stress carried by the grains falls. As grain-to-grain contact weakens, so does the soil, even though nothing has been added to it. Water pressure quietly steals the ground's strength.

Liquefaction

Push this far enough and effective stress can drop toward zero: the grains lose contact, and the soil momentarily loses all ability to resist shear, flowing like a liquid. This is liquefaction, and it is why shaking can turn solid ground to slurry beneath buildings during an earthquake. Effective stress explains both why soil is strong and how, in an instant, it can fail.

Calculating Effective Stress

To compute effective stress, use the Effective Stress Calculator. Find the pore pressure it subtracts with the Pore Water Pressure Calculator, and relate it to bearing capacity with the Soil Bearing Capacity Calculator.

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