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宋艳暾

硕士生导师
教师姓名:宋艳暾
教师拼音名称:Song YanTun
职称:副教授
学历:博士研究生毕业
学位:理学博士学位
办公地点:资环楼203
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毕业院校:中山大学
所属院系:资源与环境学院
所在单位:资源与环境学院
学科:水土保持与荒漠化防治    
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论文成果
Evolution and deposition patterns of turbidity currents under complex vegetation canopies
发布时间:2025-03-24    点击次数:

DOI码:10.1016/j.jhydrol.2024.131698

发表刊物:Journal of Hydrology

关键字:Turbidity current Vegetation resistance Leaf morphology Suspended sediment flux Sediment size distribution

摘要:Understanding the flow-vegetation-sediment feedback mechanism is critical for ecological restoration of gently sloped landscapes. Numerous simulation or laboratory experiments on turbidity currents over vegetation have revealed the important roles of vegetation canopy morphology and structure in this feedback mechanism. However, there is still a lack of analysis on the related physical processes. This study investigated the evolutionary characteristics and sediment transport and deposition patterns of turbidity currents with different sediment size distribution in vegetation patches of different canopy morphologies through lock-exchange experiments. The roles of vegetation leaf morphology and canopy structure were explored by varying the leaf morphology and vegetation density with turbidity currents prepared using sediment samples configured with different particle sizes, which are more compatible with natural conditions. The kinetic characteristics and sediment distribution of the turbidity currents over vegetation were simultaneously analyzed, providing a new perspective for updating the methodology in laboratory experiments. The major findings of this study can be summarized as follows: 1) the general spatiotemporal evolution law of turbidity currents is applicable to complex vegetation canopy morphology; 2) canopy structure dominated by leaf morphology is an important influencing factor that needs to be taken into account in the research on vegetation resistance; and 3) the correlation between turbidity current momentum and suspended sediment transport decreases under complex conditions, and coarse-grained suspended sediment tend to limit the movement of turbidity currents and major deposition distance of the sediment. These findings can provide theoretical support for conservation of floodplain soil and water and restoration of watershed ecology.

论文类型:期刊论文

文献类型:J

卷号:640

页面范围:13169

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发表时间:2024-03-01

收录刊物:SCI