粉质土在波浪作用下形成浮泥层的过程及流动特征  

Flow Characteristics and Process of Forming Fluid Mud Layer under Wave in Silty Soil

作　　者：吕楚岫 谭海东 李猛 LV Chuxiu;TAN Haidong;LI Meng(State Key Laboratory of Land and Sea Eco-Improvement and Systematic Regulation,Shandong Academy for Environmental Planning,Jinan,Shandong 250101,China;College of Environmental Science and Engineering,Ocean University of China,Qingdao,Shandong 266100,China)

机构地区：[1]国家环境保护陆海统筹生态治理与系统调控重点实验室,山东省生态环境规划研究院,山东济南250101 [2]中国海洋大学环境科学与工程学院,山东青岛266100

出　　处：《山东水利》2024年第11期51-54,共4页Shandong Water Resources

摘　　要：波浪作用所形成的浮泥层,其形成和流动是研究海底沉积物输运及地形地貌演变的重要内容。本文利用波浪水槽研究了浮泥层形成及流动的过程,并给出了浮泥层在静水环境下可以发生流动的临界含沙量。The formation and flow of fluid mud layer formed by wave action is an important content in the study of sediment transport and landform evolution.In this paper,the formation and flow process of fluid mud layer is studied by using wave flume,and the critical sediment content can flow in still water environment is put forward.

关 键 词：浮泥层 临界含沙量 波浪作用 

分 类 号：U416.1[交通运输工程—道路与铁道工程]