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Applying ADCPs for Long-Term Monitoring of SSC in Rivers

机译:应用ADCPS在河流中的SSC长期监测

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摘要

The flow rate and the suspended sediment concentration (SSC) of two different rivers draining into the Adriatic Sea basin, the Secchia in Italy and the Devoll in Albania, were analyzed by processing the data collected in a 245-day period at monitoring stations equipped with side-looking acoustic Doppler current profilers (H-ADCPs). SSC was determined as a by-product of the echo profiles along the horizontal aligned acoustic beams emitted by H-ADCPs. For the first time, the effect of organic matter other than a change of inorganic particles size distribution was evaluated as a possible reason for backscatter and attenuation variations during hydrological events. This reduced average deviations between acoustically inferred and sampled concentrations from 1 order of magnitude to 20% of actual values. The improvement required the measuring of attenuation to backscatter ratio (ABR) in addition to sound attenuation. The validation interval covered 3 orders of magnitude from 10(-1) to 10 g L-1. In this paper the potential of the ABR method using H-ADCP to continuously monitor suspended sediment fluxes is tested in two different rivers, enabling single peak flood analysis and reliable assessment of sediment budget across a river cross section. The advantages and disadvantages of this method are presented and discussed.
机译:通过加工在配备的监测站245天期间收集的数据,分析了两种不同河流排放到亚得里亚海盆地中的两种不同河流的流量和悬浮在亚得里亚海盆地中的塞尔巴尼亚和阿尔巴尼亚的森林。侧视声学多普勒电流分析仪(H-ADCPS)。 SSC被确定为沿着H-ADCP发射的水平对准声光束的回波曲线的副产物。首次,除了无机颗粒尺寸分布的变化之外的有机质的影响被评价为后散射和水文事件期间的衰减变化的可能原因。这种从1级到20%的原声学推断和采样浓度之间的平均偏差降低到实际值的20%。除了声音衰减之外,改善需要测量衰减与反散射率(ABR)的衰减。验证间隔涵盖从10(-1)到10g l-1的3个级。本文在两种不同的河流中测试了使用H-ADCP以连续监测悬浮沉积物的ABR方法的潜力,从而实现了河流横截面上的单峰洪水分析和对沉积物预算的可靠评估。提出和讨论了该方法的优点和缺点。

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  • 来源
    《Water resources research》 |2020年第1期|e2019WR026087.1-e2019WR026087.23|共23页
  • 作者单位

    Univ Bologna Dept Civil Chem Environm & Mat Engn Bologna Italy;

    Univ Bologna Dept Civil Chem Environm & Mat Engn Bologna Italy;

    Polish Acad Sci Inst Geophys Hydrol & Hydrodynam Dept Warsaw Poland;

    NTNU Dept Civil & Environm Engn Trondheim Norway;

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