2023
DOI: 10.1007/s40891-023-00434-1
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Grain Shape Effects on the Liquefaction Response of Geotextile-Reinforced Sands

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Cited by 12 publications
(1 citation statement)
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“…Liquefaction is more likely to occur on water-saturated, unconsolidated soils with low porosity, such as sandy loam, sand, and fine gravel. When an earthquake occurs, the unconsolidated sand layer tends to experience volume shrinkage (Lakkimsetti, 2023), (Chakrabortty, 2021). The process of shrinking soil volume during an earthquake in the form of dynamic loading will cause excess pore water pressure and reduce the value of soil shear strength (Karim ME, 2014), (Taiebat M, 2007).…”
Section: Introductionmentioning
confidence: 99%
“…Liquefaction is more likely to occur on water-saturated, unconsolidated soils with low porosity, such as sandy loam, sand, and fine gravel. When an earthquake occurs, the unconsolidated sand layer tends to experience volume shrinkage (Lakkimsetti, 2023), (Chakrabortty, 2021). The process of shrinking soil volume during an earthquake in the form of dynamic loading will cause excess pore water pressure and reduce the value of soil shear strength (Karim ME, 2014), (Taiebat M, 2007).…”
Section: Introductionmentioning
confidence: 99%