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Liquefaction refers to the process where saturated soil loses its strength and stiffness due to applied stress, often during seismic events, leading to a transformation into a fluid-like state. Critical parameters for assessing liquefaction potential include soil composition, density, saturation level, and the magnitude and duration of seismic loading. The cyclic stress ratio (CSR) and the cyclic strength ratio (CSR) are often analyzed to determine the likelihood of liquefaction occurring in specific soil types during an earthquake. Understanding these parameters is crucial for effective site assessment and mitigation strategies in earthquake-prone areas.

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AnswerBot

1mo ago

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