中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Wave & current-induced progressive liquefaction in loosely deposited seabed

文献类型:期刊论文

作者Yang, Guoxiang2; Ye, Jianhong1,2
刊名OCEAN ENGINEERING
出版日期2017
卷号142页码:303-314
关键词Pore pressure build up Progressive residual liquefaction Loosely deposited seabed floor Wave & current Pastor-Zienkiewicz Mark III FSSI-CAS 2D
ISSN号0029-8018
DOI10.1016/j.oceaneng.2017.07.027
英文摘要Quaternary newly deposited loose seabed soil widely distributes in offshore area in the world. Wave-induced residual liquefaction in loose seabed floor brings great risk to the stability of offshore structures in extreme climate. Understanding of the characteristics of wave-induced residual liquefaction in loose seabed is meaningful for engineers involved in design of offshore structures. In this study, wave & current-induced residual liquefaction in loose seabed floor is investigated deeply and comprehensively adopting a validated integrated numerical model. The time history of wave & current-induced pore pressure, effective stress, shear stress, lateral pressure coefficient K-0, stress angle, displacement of seabed soil are all quantitatively demonstrated. The variation process of progressive liquefaction, stress path, as well as stress-strain relation also are illustrated in detail. The classic effective stress principle has been modified to describe the nonlinear phenomenon that the reduction rate of vertical effective stress sigma'(Z) is faster than that of horizontal effective stress sigma'(x) and sigma'(y) accompanying residual pore pressure build up. It is shown that the integrated numerical model FSSI-CAS 2D incorporating PZIII soil model can effectively and precisely capture a series of nonlinear dynamic response characteristics of loose seabed floor under wave & current loading. The computational results further confirm the wave & current-induced liquefaction in loose seabed soil is progressively downward, initiating at seabed surface. Besides, it is found that three physical processes, including vertical distribution of oscillatory pore pressure, time history of stress angle as well as lateral pressure coefficient K-0 could be taken as indirect indicator to judge the occurrence of wave-induced residual liquefaction, and predict the residual liquefaction depth in loose seabed. It is also found that the progressive liquefaction process is significantly affected by wave height, permeability and saturation of seabed soil.
WOS研究方向Engineering ; Oceanography
语种英语
WOS记录号WOS:000410010700028
出版者PERGAMON-ELSEVIER SCIENCE LTD
源URL[http://119.78.100.198/handle/2S6PX9GI/4143]  
专题岩土力学所知识全产出_期刊论文
国家重点实验室知识产出_期刊论文
作者单位1.Chinese Acad Sci, Inst Rock & Soil Mech, State Key Lab Geomech & Geotech Engn
2.China Univ Geosci, Sch Engn & Technol, Dept Civil Engn ;
推荐引用方式
GB/T 7714
Yang, Guoxiang,Ye, Jianhong. Wave & current-induced progressive liquefaction in loosely deposited seabed[J]. OCEAN ENGINEERING,2017,142:303-314.
APA Yang, Guoxiang,&Ye, Jianhong.(2017).Wave & current-induced progressive liquefaction in loosely deposited seabed.OCEAN ENGINEERING,142,303-314.
MLA Yang, Guoxiang,et al."Wave & current-induced progressive liquefaction in loosely deposited seabed".OCEAN ENGINEERING 142(2017):303-314.

入库方式: OAI收割

来源:武汉岩土力学研究所

浏览0
下载0
收藏0
其他版本

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。