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首页> 外文期刊>River research and applications >Considerations for using turbidity as a surrogate for suspended sediment in small, ungaged streams: Time-series selection, streamflow estimation, and regional transferability
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Considerations for using turbidity as a surrogate for suspended sediment in small, ungaged streams: Time-series selection, streamflow estimation, and regional transferability

机译:使用浊度替代未成年的小溪中悬浮泥沙的注意事项:时间序列选择,溪流估算和区域可迁移性

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Suspended sediment (SS) transport is an important and natural process in aquatic ecosystems. However, accelerated erosion due to anthropogenic land uses causes excessive sedimentation, which makes SS pollution one of the most prevalent stressors causing biological impairments of freshwater. Despite the ubiquitous nature of sedimentation and the ways in which it negatively impacts streams, inherent obstacles exist to effective measurement and characterization of fluvial SS loading. SS concentrations (SSCs) can vary widely during similar hydrologic conditions, making discharge an unreliable predictor variable. Alternatively, turbidity has been shown to be an effective surrogate for SSC, and methods using in situ optical turbidity sensors to indirectly measure SSCs have been developed. We present data and results from research using turbidity as a surrogate for SSC in five small, ungaged streams in the Chesapeake Bay watershed. Objectives of this study include presenting practical considerations and strategies for applying the turbidity-SSC surrogate method in small headwater streams. Empirical evidence is presented illustrating the potential correlation between land use and sediment loading. Additionally, accurate estimates of sediment loading require utilization of high frequency time-series data and on-site monitoring to capture timing and magnitude of streamflow, especially during intense, short-duration runoff events. Similar turbidity-SSC relationships across watersheds suggest that regional regression curves could be established to allow more efficient and cost-effective estimation of sediment loading. The broad application of this method would also benefit water resource management, by enabling prioritization of sites for stream restoration, standardizing techniques for monitoring stream recovery, or documenting impacts of discrete land-use changes.
机译:悬浮沉积物(SS)的运输是水生生态系统中重要的自然过程。但是,由于人为土地利用而造成的加速侵蚀会导致过多的沉积,这使SS污染成为引起淡水生物损伤的最普遍的压力源之一。尽管沉积物无处不在,并且对河流产生负面影响,但仍然存在有效测量和表征河流SS负荷的固有障碍。在相似的水文条件下,SS浓度(SSCs)可能会有很大变化,从而使流量成为不可靠的预测变量。另外,浊度已被证明是SSC的有效替代物,并且已经开发出了使用原位光学浊度传感器间接测量SSC的方法。我们提供了切萨皮克湾流域中五个浊软的小溪中使用浊度作为SSC替代物的研究数据和结果。这项研究的目的包括提出在小型源头水流中应用浊度-SSC替代方法的实际考虑因素和策略。经验证据表明,土地利用与沉积物负荷之间可能存在相关性。此外,对泥沙负荷的准确估算需要利用高频时间序列数据和现场监测来捕获水流的时间和大小,特别是在剧烈的,短期的径流事件中。流域内相似的浊度-SSC关系表明,可以建立区域回归曲线,以更有效和成本效益地估算沉积物的负荷。该方法的广泛应用还可以通过优先考虑溪流恢复的地点,标准化监测溪流恢复的技术或记录离散的土地用途变化的影响,从而有益于水资源管理。

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