Gravelly soil is generally recognized to have no liquefaction potential. However, liquefaction cases were reported in central Taiwan in the 1999 Chi-Chi Taiwan earthquake and in the 1988 Armenia earthquake. Thus, further studies on the liquefaction potential of gravelly soil are warranted. Because l
Correlation of shear wave velocity with liquefaction resistance based on laboratory tests
โ Scribed by Chen Yunmin; Ke Han; Chen Ren-peng
- Book ID
- 104093313
- Publisher
- Elsevier Science
- Year
- 2005
- Tongue
- English
- Weight
- 502 KB
- Volume
- 25
- Category
- Article
- ISSN
- 0267-7261
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โฆ Synopsis
According to the results of cyclic triaxial tests on Hangzhou sands, a correlation is presented between liquefaction resistance and elastic shear modulus. Material-dependent but independent of confining stress, shows the linear relation of (s d /2) 1/2 with G max . For its application to different soils, a method proposed by Tokimatsu [Tokimatsu K, Uchida A. Correlation between liquefaction resistance and shear wave velocity. Soils Found 1990:30(2):33-42] is utilized to normalize the shear modulus with respect to minimum void ratio. A simplified equation is established to evaluate the liquefaction potential by shear-wave velocity. The critical shear-wave velocity of liquefaction is in linear relation with 1/4 power of depth and the peak horizontal ground surface acceleration during earthquakes. The equation proposed in this paper is compared with previous methods especially the procedure proposed by Andrus [RD Andrus, KH Stokoe. Liquefaction resistance of soils from shear-wave velocity. J Geotech Geoenviron Eng 2000:126(11):1015-25]. The results show its simplicity and effectiveness when applied to sands, but more validation or modification is needed for its application to sand with higher fines content.
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This papers presents a new approach for developing a limit state for liquefaction evaluation based on "eld performance data. As an example to illustrate the new approach, a database that consists of, among many other features, in situ shear wave velocity measurements and "eld observations of liquefa