[口头报告]耦合泥沙连通性指数和MUSLE模型探究事件尺度的侵蚀与产沙关系

耦合泥沙连通性指数和MUSLE模型探究事件尺度的侵蚀与产沙关系
编号:655 稿件编号:1959 访问权限:仅限参会人 更新:2024-04-10 22:12:55 浏览:461次 口头报告

报告开始:2024年05月19日 15:31 (Asia/Shanghai)

报告时间:7min

所在会议:[S11] 主题11、地表过程与地貌 » [S11-5] 主题11、地表过程与地貌 专题11.5、专题11.6(19日下午,204)

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摘要
Sediment connectivity quantifies the intermediate processes between initial erosion and the corresponding sediment yield. However, fully capturing the variations in sediment connectivity at the event scale and revealing their impact on watershed sediment sources remains challenging. Herein, we established an event-based model to assess sediment connectivity by integrating runoff factors. The spatiotemporal variability of sediment connectivity was evaluated for 58 rainfall events in three heterogeneous watersheds. The degree of sediment connectivity served as an indicator to quantify the proportion of potential sediment transport from units to the watershed outlet, with 1 indicating that the eroded sediment can be fully connected and 0 indicating that it cannot be transported. Moreover, the controls of sediment connectivity on watershed sediment sources and yield were determined. Our results indicated that the watersheds with poor vegetation and dense gullies were characterized by high sediment connectivity during all the rainfall events. The connectivity degree was below 0.5 in approximately 80% of the watershed area, suggesting that most of the eroded sediment was deposited. Rainfall amount and duration dominated the degree of connectivity of the distal hillslopes, while rainfall intensity exerted a primary control on the transport of sediments from riverbanks to the outlet. In addition, the increase of mismatched area between sediment connectivity and erosion resulted in the decrease of sediment yield. The interaction between sediment connectivity and erosion effectively explained the spatial patterns of sediment sources (p < 0.05). Our work confirmed that the coupled erosion model and sediment connectivity predicted the sediment yield accurately. The predictions for different watersheds portrayed that the Nash-Sutcliffe efficiency and Willmott’s agreement index were greater than 0.70 and 0.89, respectively. These findings revealed the role of sediment connectivity and are the critical basis to identify watershed-specific sediment management practices.
 
关键字
sediment connectivity,rainfall events,spatio-temporal data model
报告人
郝芮
博士研究生 华中农业大学

稿件作者
郝芮 华中农业大学
史志华 华中农业大学
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