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Soil Liquifaction

Soil liquefaction can be defined as the phenomenon by which the strength of the soil is lost either due to dynamic or static loading. Most of the earthquake forces are the major causes of soil liquefaction. The vibrations of earthquake shockwaves in water-saturated soils trigger the phenomenon. |                                                        saturate soil                Liquefaction occurs in saturated soils, that is, soils in which the space between individual particles is completely filled with water. This water exerts pressure on the soil particles that influence how tightly the particles themselves are pressed together. Prior to an earthquake, the water pressure is relatively low. However, earthquake shaking can cause the water pressure to increase to the point where the soil particle...