中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Erosion on irregular slope surface: A full N-S equation based numerical study

文献类型:会议论文

作者An Y(安翼); Liu QQ(刘青泉)
出版日期2017
会议日期September 19, 2016 - September 22, 2016
会议地点Stuttgart, Germany
关键词Erosion Landforms Rivers Sedimentation Characteristic length Depth averaged modeling Non uniform velocities Overland flow modeling Saint Venant equation Sediment yields Sheet erosions Slope surfaces
页码21
英文摘要Soil erosion by overland flowon hillslopes is one of the most crucial fundamental sediment yield processes. Generally, Saint-Venant equation based overland flow model is widely used to model this special flow, and in turn, the sheet erosion. However, it becomes more and more clear that the overland flow, which generally involves irregular micro landform, could behave different characteristics from river flow in which classical depth-averaged model suits well. The key issue is that the characteristic length of the irregular micro landform is considerable large comparing with the overland flow depth, which leads to nonuniform velocity profile in the depth direction. Thus, this paper employed full Navier-Stokes equation to study the overland flow on partially inundated irregular micro-relief and discuss the self-enhanced sheet erosion processes. © 2017 Taylor & Francis Group, London.
会议录River Sedimentation - Proceedings of the 13th International Symposium on River Sedimentation, ISRS 2016
语种英语
ISBN号9781138029453
源URL[http://dspace.imech.ac.cn/handle/311007/78018]  
专题力学研究所_流固耦合系统力学重点实验室(2012-)
作者单位Institute of Mechanics, Chinese Academy of Sciences, Beijing, China
推荐引用方式
GB/T 7714
An Y,Liu QQ. Erosion on irregular slope surface: A full N-S equation based numerical study[C]. 见:. Stuttgart, Germany. September 19, 2016 - September 22, 2016.

入库方式: OAI收割

来源: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。