Liquefaction is the name given to the process that converts a solid soil mass into a liquid.
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in the bedrock (soil/ground) with loose sediments.
liquefaction
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.
Another name for saturated soil could be soil liquefaction.
Soil liquefaction occurs when loosely packed, water-saturated soil temporarily loses strength during an earthquake, causing it to behave like a liquid. The purpose of studying soil liquefaction is to understand how it can impact the stability of structures and infrastructure built on these soils, and to develop strategies to mitigate its effects through proper engineering and construction techniques.
liquefaction. During liquefaction, the water-saturated soil behaves like a liquid due to increased pore water pressure, resulting in loss of strength and stability. This process can lead to ground failure, settlement, and potential structural damage during an earthquake.
Homes and other structures can be protected from liquefaction by being anchored to a rock below the soil. Liquefaction happens when structures are built on soft ground.
liquefaction
Water-saturated soil and rock become liquid
Albert T. F Chen has written: 'RELA' -- subject(s): Computer programs, Sandy soils, Soil liquefaction, Testing 'PETAL, Penetrating Testing And Liquefaction' -- subject(s): Soil liquefaction, Data processing
The process you are referring to is liquefaction. Liquefaction occurs when water-saturated soil is shaken by an earthquake, causing it to lose strength and behave like a liquid, often resulting in ground failure and structural damage.
Liquefaction turns soft soil into mud and then the building sinks. If it were raining, then it would make soil and mud more muddy and more buildings would collapse.