海滩冲流带水沙运动综述  

Review on Water-sediment Movement in Swash Zone

作　　者：潘毅[1] 陈自怡 刘烨 朱芳芳 匡翠萍[3] PAN Yi;CHEN Ziyi;LIU Ye;ZHU Fangfang;KUANG Cuiping(College of Harbor,Coastal and Offshore Engineering,Hohai University,Nanjing 210024,China;Faculty of Science and Engineering,University of Nottingham Ningbo China,Ningbo 315100,China;College of Civil Engineering,Tongji University,Shanghai 200092,China)

机构地区：[1]河海大学港口海岸与近海工程学院,南京210024 [2]宁波诺丁汉大学理工学院,浙江宁波315100 [3]同济大学土木工程学院,上海200092

出　　处：《同济大学学报（自然科学版）》2024年第6期920-927,共8页Journal of Tongji University:Natural Science

基　　金：国家自然科学基金(51979098);江苏省自然科学基金(BK20181309)。

摘　　要：简述了冲流带水沙运动的基本特征,综述了入渗或出渗、段波紊动、泥沙平流、沉降或冲刷延后以及沿岸流、波浪-冲流相互作用和波群作用对冲流带水沙运动影响的最新研究进展;介绍了冲流带水沙运动物理实验的实现方式以及物理实验中冲流带泥沙运动观测技术的最新进展,论述了用于冲流带水沙运动研究的2类数学模型,并讨论了各自的优缺点。最后,探讨了现有研究成果和研究方法的局限性,并给出了未来的研究展望。In this paper,the basic characteristics of water-sediment movement in swash zone are described,and the latest research progress on the influence of infiltration or exfiltration,bore turbulence,sediment advection,settling or scour lag,longshore current,waveswash interaction and wave group on the water-sediment movement in the swash zone is summerized.The basic facilities of physical experiments on the water-sediment movement in the swash zone are introduced,and the latest progress of the observation technology of the sediment movement in the swash zone is reviewed.Two types of numerical models used to study the watersediment movement in the swash zone are presented,and their advantages and disadvantages are investigated.The limitations of existing research methods and results arediscussed, and the future research prospects areproposed.

关 键 词：冲流带 水沙运动 海岸泥沙 

分 类 号：P737.1[天文地球—海洋地质]