The phenomenon of soil liquefaction occurs when saturated soil substantially loses strength and stiffness due to an applied stress such as shaking from an earthquake. Let's analyze the conditions for liquefaction:
- High Ground Water Table: Liquefaction is more likely when the water table is high, as this increases pore water pressure, reducing soil strength.
- Dynamic Load: Dynamic or cyclic loading, like seismic activity, agitates soil particles, contributing to liquefaction.
- Soil Type: Loose fine sands are particularly susceptible to liquefaction. The soil particles are less densely packed, making it easier for pore pressures to disrupt the structure.
The correct combination of these factors is: High ground water table, dynamic load and loose fine sand