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高频浊度作为河流总磷浓度替代指标的评估。

An evaluation of high frequency turbidity as a proxy for riverine total phosphorus concentrations.

机构信息

Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, P.O. Box 7050, 75007 Uppsala, Sweden.

Department of Aquatic Sciences and Assessment, Swedish University of Agricultural Sciences, P.O. Box 7050, 75007 Uppsala, Sweden.

出版信息

Sci Total Environ. 2019 Feb 15;651(Pt 1):103-113. doi: 10.1016/j.scitotenv.2018.09.127. Epub 2018 Sep 11.

Abstract

Surface water eutrophication resulting from excessive phosphorus (P) inputs is one of today's most challenging environmental issues. Riverine total phosphorus (TP) concentrations have high temporal variability, which complicates flux estimation. We evaluated the usefulness of high frequency in-situ turbidity measurements as a proxy for TP in Sävjaån, a river draining a mixed land use catchment (722 km) in central Sweden. Turbidity was monitored every 10th-15th minute during 6 consecutive years (2012-2017). Linear regression showed a good relationship between high frequency turbidity and TP (r = 0.64) and could hence be used for comparison of flux estimation methods. Predictive power of the turbidity-TP relationship was not improved by adding seasons, hydrograph rising/falling limb or high/low stream discharge to the model which argues for a single transfer function relating turbidity and TP. Both TP and turbidity were log-normally distributed. However, flux estimates were sensitive to data transformation; predicted TP concentrations and fluxes based on log-transformed data were biased towards lower concentrations and fluxes compared to non-transformed data. In five of six years grab sample and high frequency estimated TP fluxes were similar (grab sample estimates -10% to +13% P transport compared to high frequency flux estimates). The exception was in 2013, when a 50-year spring flood occurred, and the grab sample estimated flux was 56% larger than that estimated from high frequency data. Thus, the flux comparisons were mostly affected by stream discharge, which underlines the importance of capturing high discharge episodes with, e.g. in situ sensors. While uncertainties regarding the use of turbidity as a proxy for TP remain, it is clear that credible water chemistry data can be obtained with current high frequency sensors. We conclude that high frequency data can be used to better understand catchment response to external pressures and gain insights into water quality that will be missed with grab sampling.

摘要

由于过量磷(P)输入导致的地表水富营养化是当今最具挑战性的环境问题之一。河流总磷(TP)浓度具有很高的时间变异性,这使得通量估算变得复杂。我们评估了高频原位浊度测量作为瑞典中部一个混合土地利用流域(722km)的 Sävjaån 河流 TP 替代物的有用性。在 6 个连续年份(2012-2017 年)中,每 10-15 分钟监测一次浊度。线性回归显示高频浊度与 TP 之间存在良好的关系(r=0.64),因此可用于比较通量估算方法。该浊度-TP 关系的预测能力并未因向模型中添加季节、水文上升/下降支或高/低流量而得到改善,这表明存在一个将浊度和 TP 联系起来的单一传递函数。TP 和浊度均呈对数正态分布。然而,通量估计对数据转换敏感;基于对数转换数据预测的 TP 浓度和通量与未转换数据相比,浓度和通量较低。在六年中的五年中, grab 样本和高频估计的 TP 通量相似(grab 样本估计值比高频通量估计值低 10%到高 13%的 P 输送)。例外是在 2013 年,当时发生了一次 50 年一遇的春季洪水,grab 样本估计的通量比高频数据估计的通量大 56%。因此,通量比较主要受流量影响,这强调了使用原位传感器捕获高流量事件的重要性。虽然使用浊度作为 TP 替代物仍然存在不确定性,但很明显,可以使用当前的高频传感器获得可靠的水质数据。我们得出结论,高频数据可用于更好地了解集水区对外部压力的响应,并深入了解抓样采样会错过的水质信息。

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