2006
DOI: 10.1061/(asce)1090-0241(2006)132:11(1413)
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Liquefaction Susceptibility Criteria for Silts and Clays

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Cited by 340 publications
(132 citation statements)
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“…It is essential to identify silts behaving as sand-like or clay-like. Boulanger and Idriss (2006) found that sand-like (behaving more fundamentally as sand) and clay-like soils (behaving more fundamentally as clay) have some fundamental differences in terms of stress-strain behaviour, compressibility and the slope of the critical-state line (CSL) in the e-ln p 0 space against the slope of the normally consolidated line (NCL). The major observations of Boulanger and Idriss (2004) include the following.…”
Section: Introductionmentioning
confidence: 99%
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“…It is essential to identify silts behaving as sand-like or clay-like. Boulanger and Idriss (2006) found that sand-like (behaving more fundamentally as sand) and clay-like soils (behaving more fundamentally as clay) have some fundamental differences in terms of stress-strain behaviour, compressibility and the slope of the critical-state line (CSL) in the e-ln p 0 space against the slope of the normally consolidated line (NCL). The major observations of Boulanger and Idriss (2004) include the following.…”
Section: Introductionmentioning
confidence: 99%
“…In a subsequent study, Boulanger and Idriss (2006) proposed that materials with P I less than 7% would have a sand-like behaviour, while materials with P I greater than or equal to 7% would exhibit a clay-like behaviour. In addition, it was also described that finegrained soils with P I values between 3 and 6% may exhibit a transitional behaviour.…”
Section: Introductionmentioning
confidence: 99%
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“…Liquefaction is mostly observed in sandy soils, but the results of comprehensive investigations carried out in the last decades have shown that sands containing some portion of a fine fraction may liquefy as well (Yamamuro andCovert 2001, Boulanger andIdriss 2006).…”
Section: Introductionmentioning
confidence: 99%