Interaction between internal solitary waves and the seafloor in the deep sea  

作　　者：Zhuangcai Tian Jinjian Huang Jiaming Xiang Shaotong Zhang Jinran Wu Xiaolei Liu Tingting Luo Jianhua Yue 

机构地区：[1]State Key Laboratory of Intelligent Construction and Healthy Operation and Maintenance of Deep Underground Engineering,China University of Mining and Technology,Xuzhou,China [2]Research Center for Deep Ocean Science and Underwater Engineering,China University of Mining and Technology,Xuzhou,China [3]Frontiers Science Center for Deep Ocean Multispheres and Earth System,Key Lab of Submarine Geosciences and Prospecting Techniques,MOE,College of Marine Geosciences,Ocean University of China,Qingdao,China [4]Institute for Learning Sciences&Teacher Education,Australian Catholic University,Brisbane,Queensland,Australia [5]Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering,Ocean University of China,Qingdao,China [6]Department of Chemical and Biomolecular Engineering,National University of Singapore,Singapore,Singapore [7]School of Resources and Geosciences,China University of Mining and Technology,Xuzhou,China

出　　处：《Deep Underground Science and Engineering》2024年第2期149-162,共14页深地科学（英文）

基　　金：National Natural Science Foundation of China,Grant/Award Number:42107158;Natural Science Foundation of Jiangsu Province,Grant/Award Number:BK20210527。

摘　　要：Internal solitary wave(ISW),as a typical marine dynamic process in the deep sea,widely exists in oceans and marginal seas worldwide.The interaction between ISW and the seafloor mainly occurs in the bottom boundary layer.For the seabed boundary layer of the deep sea,ISW is the most important dynamic process.This study analyzed the current status,hotspots,and frontiers of research on the interaction between ISW and the seafloor by CiteSpace.Focusing on the action of ISW on the seabed,such as transformation and reaction,a large amount of research work and results were systematically analyzed and summarized.On this basis,this study analyzed the wave–wave interaction and interaction between ISW and the bedform or slope of the seabed,which provided a new perspective for an in‐depth understanding of the interaction between ISW and the seafloor.Finally,the latest research results of the bottom boundary layer and marine engineering stability by ISW were introduced,and the unresolved problems in the current research work were summarized.This study provides a valuable reference for further research on the hazards of ISW to marine engineering geology.

关 键 词：bottom boundary layer INTERACTION internal solitary wave SEAFLOOR SEDIMENT 

分 类 号：P731.2[天文地球—海洋科学]