2014
DOI: 10.1016/j.soildyn.2013.11.001
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Requirements for soil-specific correlation between shear wave velocity and liquefaction resistance of sands

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Cited by 42 publications
(30 citation statements)
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“…14. The more recent relationship established by Ahmadi & Paydar (2014) from two types of clean sands, namely the Firoozkooh and the Babolsar sands, are also shown in Fig. 14, and the one based on the Babolsar sand gives much less satisfactory evaluation than that of the Firoozkooh sand.…”
Section: Validation and Discussionmentioning
confidence: 94%
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“…14. The more recent relationship established by Ahmadi & Paydar (2014) from two types of clean sands, namely the Firoozkooh and the Babolsar sands, are also shown in Fig. 14, and the one based on the Babolsar sand gives much less satisfactory evaluation than that of the Firoozkooh sand.…”
Section: Validation and Discussionmentioning
confidence: 94%
“…This is especially true for sites underlain by soils that are difficult to penetrate or sample (Andrus & Stokoe, 2000;Kayen et al, 2013). The V s -based simplified method has attracted an increasing number of studies, and various 'boundary curves' have been relatively well established on the basis of either field data (Robertson et al, 1992;Andrus & Stokoe, 2000;Juang et al, 2001;Andrus et al, 2004;Juang et al, 2005;Kayen et al, 2013), or laboratory studies (Dobry et al, 1981;de Alba et al, 1984;Tokimatsu & Uchida, 1990;Chen et al, 2005;Wang et al, 2006;Zhou & Chen, 2007;Baxter et al, 2008;Zhou et al, 2010;Ahmadi & Paydar, 2014).…”
Section: Introductionmentioning
confidence: 99%
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“…Near-surface shear wave velocity is of great importance in the fields of geophysics and earthquake engineering, since it is closely correlated with the physical and mechanical properties of soil and rock in shallow crust. In engineering practice, it has a wide range of applications, such as classification of building sites (Borcherdt, 1994), evaluation of liquefaction potential (Ahmadi & Paydar, 2014), estimation of seismic response (Choi & Stewart, 2005), and assessment of earthquake loss (Bendito et al, 2014). In recent years, shear wave velocity has been used to detect minor material changes in the subsurface for seismic monitoring of faults (Hillers & Campillo, 2018;Wegler & Sens-Schönfelder, 2007), volcanoes (Brenguier et al, 2014;Wegler et al, 2006), landslides (Bièvre et al, 2018;Mainsant et al, 2012), and hydrocarbon reservoirs (Bakulin & Calvert, 2006;Miyazawa et al, 2008).…”
Section: Introductionmentioning
confidence: 99%