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dc.contributor.authorXu, Guohui
dc.contributor.authorSun, Yongfu
dc.contributor.authorYu, Yueqian
dc.contributor.authorLin, Lin
dc.contributor.authorHu, Guanghai
dc.contributor.authorZhao, Qingpeng
dc.contributor.authorGuo, Xiujun
dc.date.accessioned2018-11-23T03:29:26Z
dc.date.available2018-11-23T03:29:26Z
dc.date.issued2012
dc.identifier.urihttp://hdl.handle.net/1834/14820
dc.description.abstractGeological disasters on the superficial seafloor were revealed in geological investigation on the Yellow River subaqueous delta. Combined with dynamic triaxial tests and wave flume experiments, occurring conditions and forming patterns of liquefaction as well as motion of the liquefied soil were explained in this paper. Based on the viewpoint that the geological disasters were formed due to silty soil liquefaction under storm waves, re-stratification issue of the superficial stratum was analyzed. Movement of the liquefied soil agreed with the wave, leading to differentiation of the soil particles. Research issues in respect of geological, environment and engineering of storm-induced liquefaction were also discussed.en_US
dc.language.isoenen_US
dc.subject.otherYellow River subaqueous deltaen_US
dc.subject.otherLiquefactionen_US
dc.subject.otherRe-stratificationen_US
dc.titleDiscussion on storm-induced liquefaction of the superficial stratum in the Yellow River subaqueous delta.en_US
dc.typeJournal Contributionen_US
dc.bibliographicCitation.issue1en_US
dc.bibliographicCitation.titleMarine Science Bulletinen_US
dc.bibliographicCitation.volume14en_US
dc.description.statusPublisheden_US
dc.format.pagerangepp.80-89en_US
dc.type.refereedNot Knownen_US
refterms.dateFOA2021-01-30T18:48:18Z


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