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An illustration of SPT spoon sample and cone penetration test data points with corresponding depths of shear-wave velocity.

An illustration of SPT spoon sample and cone penetration test data points with corresponding depths of shear-wave velocity.

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Direct measurement of shear-wave velocity, Vs, in the field to evaluate the liquefaction resistance of soils is an alternative or complement approach to penetration-based methods. However, the existing liquefaction assessment methods established on the Vs have uncertainties about how the fines content and soil-type change the relationship between V...

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... this study, for the soils that have the same geological age (Holocene-age) and geological depositional environments (uncemented deposits), overburden stress corrected V s values with normalized cone penetration resistance for three distinct ranges of non-/low plastic FC by mass of FC ≤ 5 %, 5% < FC ≤ 20%, and 20% < FC ≤ 35%, are shown in Fig. 6a-c. Figure 7 presents how the FC, cone penetration resistance, and V s were selected at the same depths. FC obtained from a 30 cm long soil sample from the SPT spoon. ...

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Citations

... The relationship between cyclic resistance ratio (CRR) and normalized velocity with respect to effective stress (V s1 ) was first suggested by Seed et al., 1 depending on the relationship between penetration blow count number (SPT-N) and V s . In the early 1990s, numerous V s1based liquefaction resistance correlations were proposed by directly measuring V s at sites where liquefaction was observed (e.g., 2,[3][4][5]. In the 2000s, probabilistic and deterministic methods were used to develop CRR-V s1 correlations (e.g., 6,7 ). ...
... Hegazy and Mayne, 52 Andrus et al., 53 Robertson, 40 and Ecemis 5 proposed V s versus q c correlations that interpret the soil-type from I c . At I c values from 1.3 to 2.9, the above-given researchers' curves are plotted in Figure 10 with the proposed trend lines (Figure 9) in this study for comparison. ...
... It should be reminded that some of the CRR-V s1 relationships shown in the figures are based primarily on tests performed on soil samples in the laboratory, [9][10][11][12][13][14][16][17][18][19][20] while the others are based primarily on field case histories. [2][3][4][5]7,8,64 At each figure, the existing (CRR) 7.5 -V s1 curves may reflect dissimilarities due to the differences in sedimentation history, mineralogy, grading characteristics of the soils, and testing conditions. The wide area (possible liquefaction zone) in each subplot representing all the triggering curves proposed in the literature were highlighted in gray. ...
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