Sedimentary Changes of a Sand Layer in Liquefied Silts  

作　　者：REN Yupeng ZENG Yu XU Xingbei XU Guohui 

机构地区：[1]Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering,Qingdao 266100,China [2]Laboratory for Marine Geology,Qingdao National Laboratory for Marine Science and Technology,Qingdao 266061,China [3]Zhejiang Huadong Construction Engineering Co.,Ltd.,Hangzhou 310000,China

出　　处：《Journal of Ocean University of China》2021年第5期1046-1054,共9页中国海洋大学学报（英文版）

基　　金：The funding for this project was provided by the National Natural Science Foundation of China(No.41976049);the Fundamental Research Funds for the Central Universities(No.202061028).

摘　　要：A flume experiment was conducted to investigate the restratification of liquefied sediment strata under a wave load with the focus on the interbedded strata of coarse and fine sediments formed in estuarine and coastal areas.The aim of this research was to study the characteristics and processes of liquefied sediment strata in terms of wave-induced liquefaction.In the experiment,the bottom bed liquefied under the wave action and the liquefied soil moved in the same period with the overlying waves,and the track of the soil particles in the liquefied soil was an ellipse.The sand layer consisting of coarse particles in the upper part,settled into the lower silt layer.The sinking of coarse particles and upward migration of the fine particles of the lower layer induced by liquefied sediment fluctuations are the likely reasons for sedimentation of the sand layer in liquefied silt.

关 键 词：storm-liquefied sediment strata LIQUEFACTION sand layer settlement silt interlayer particle sorting 

分 类 号：P736.21[天文地球—海洋地质]