405 / 2024-03-13 21:55:46
Unsteady suspended sediment transport flux measurement using ADCP
unsteady flow,suspended sediment,Yangtze River,ADCP
摘要录用
Lei Xu / The National Key Laboratory of Water Disaster Prevention;Key Laboratory of Hydrologic-Cycle and Hydrodynamic-System of Ministry of Water Resources
Saiyu Yuan / The National Key Laboratory of Water Disaster Prevention;Key Laboratory of Hydrologic-Cycle and Hydrodynamic-System of Ministry of Water Resources
Bart Vermeulen / Wageningen University and Research
Jiajian Qiu / The National Key Laboratory of Water Disaster Prevention;Key Laboratory of Hydrologic-Cycle and Hydrodynamic-System of Ministry of Water Resources
Hongwu Tang / The National Key Laboratory of Water Disaster Prevention;Key Laboratory of Hydrologic-Cycle and Hydrodynamic-System of Ministry of Water Resources
Suspended sediment transport flux is an important indicator for hydrological monitoring. While the estimation of suspended load transport from Acoustic Doppler Current Profilers (ADCPs) has been extensively investigated, the calibration of ADCP backscatter may face challenges, particularly due to variations in specific attenuation. The accurate prediction of specific attenuation success relies primarily on changes in suspended particle size, posing considerable challenges to monitoring unsteady suspended sediment transport. To investigate the characteristics and observation methods of unsteady suspended sediment transport, we conducted continuous monitoring of flow structure and suspended sediment using acoustic instruments and water sampling both upstream and downstream of the confluence between the Yangtze River and Poyang Lake within the Three Gorges Dam regulation period (June 30, 2023 - July 10, 2023). Our findings reveal a nuanced pattern in flow discharge at Jiujiang Station, decreasing from 27000m^3/s to 23800m^3/s initially and then increasing to 26100m^3/s over the observation period. Similarly, suspended sediment concentration and median particle size exhibited an initial increase followed by a subsequent decrease. Notably, the traditional method, which neglects specific attenuation, struggled to accurately estimate suspended sediment concentration. In contrast, the method incorporating the suspended sediment absorption coefficient successfully retrieved the concentration using ADCP backscatter, where the absorption coefficient displayed variations in tandem with particle size changes. This study contributes valuable insights to sediment regulation and management, offering crucial support for decision-making in water resource management.

 
重要日期
  • 会议日期

    10月14日

    2024

    10月17日

    2024

  • 09月30日 2024

    初稿截稿日期

  • 10月17日 2024

    注册截止日期

主办单位
国际水利与环境工程学会亚太地区分会
承办单位
长江水利委员会长江科学院
四川大学
联系方式
移动端
在手机上打开
小程序
打开微信小程序
客服
扫码或点此咨询