首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Comparison of two stream gauging systems for measuring runoff and sediment yield for a semi-arid watershed
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Comparison of two stream gauging systems for measuring runoff and sediment yield for a semi-arid watershed

机译:两种测量半干旱流域径流和泥沙量的流量测量系统的比较

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摘要

Our ability to understand erosion processes in semi-arid ecosystems depends on establishing relationships between rainfall and runoff. This requires collection of extensive and accurate hydrologic and sediment data sets. A supercritical flume with a total load traversing slot sediment sampler used on several sites at the Walnut Gulch Experimental Watershed (WGEW) near Tombstone, AZ has proven to be a reliable way to measure flow and sediment discharge from small watersheds. However, it requires installation of a costly structure that is only suitable for relatively small flows. A more commonly used method based on ease of installation and expense is the pump sampler. One example of this is a set of instrumentation developed by the Australian Commonwealth Scientific and Industrial Research Organization (CSIRO), in which the pump sediment sampler is part of an in-channel, fully automated system for measuring water velocity, depth, turbidity and collecting runoff samples. A 3.7ha arid watershed at WGEW was instrumented with both systems and hydrologic and sediment data were collected and compared during a 2year period. Total sediment yield for the entire period measured by the CSIRO pump sampler (11.6tha~(-1)) was similar to that by traversing slot sampler (11.5tha~(-1)). The pump sampler accurately estimated the amount of fine (< 0.5mm) sediment fractions exported, but consistently underestimated the coarse (>0.5mm) sediment fractions. Median sediment diameter of samples collected by traversing slot and pump sampler were 0.32 and 0.22mm, respectively. This study outlines the benefits and limitations of the pump sampler based system for monitoring sediment concentration and yield in high-energy headwater catchments, and makes recommendations for improvement of its performance.
机译:我们了解半干旱生态系统侵蚀过程的能力取决于建立降雨与径流之间的关系。这就需要收集广泛而准确的水文和沉积物数据集。在亚利桑那州墓碑附近的胡桃谷实验流域(WGEW)的多个站点上使用了带有总负荷穿越槽沉积物采样器的超临界水槽,这已被证明是测量小流域流量和沉积物排放的可靠方法。但是,这需要安装仅适用于相对较小流量的昂贵结构。基于易于安装和费用的一种更常用的方法是泵采样器。一个例子就是澳大利亚联邦科学与工业研究组织(CSIRO)开发的一套仪器,其中的泵沉积物采样器是用于测量水速,深度,浊度和收集的全自动管道内系统的一部分。径流样本。 WGEW对一个3.7公顷的干旱流域进行了系统和仪器测量,并在2年期间收集并比较了水文和泥沙数据。 CSIRO泵采样器(11.6tha〜(-1))测得的整个时期的沉积物总产量与横移槽采样器(11.5tha〜(-1))的相似。泵采样器准确估算了出口的细小(<0.5毫米)沉积物部分的数量,但始终低估了粗略的(> 0.5毫米)沉积物部分。横移槽和泵进样器收集的样品中值沉积物直径分别为0.32和0.22mm。这项研究概述了基于泵采样器的系统的优点和局限性,该系统用于监控高能源水集水区的沉积物浓度和产量,并提出改善其性能的建议。

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