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首页> 外文期刊>Hydrology and Earth System Sciences >High-frequency monitoring of nitrogen and phosphorus response in three rural catchments to the end of the 2011–2012 drought in England
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High-frequency monitoring of nitrogen and phosphorus response in three rural catchments to the end of the 2011–2012 drought in England

机译:高频监测三个农村流域氮和磷的响应,直至英格兰2011-2012年干旱结束

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This paper uses high-frequency bankside measurements from three catchmentsselected as part of the UK government-funded Demonstration Test Catchments(DTC) project. We compare the hydrological and hydrochemical patterns duringthe water year 2011–2012 from the Wylye tributary of the River Avon with mixedland use, the Blackwater tributary of the River Wensum with arable land useand the Newby Beck tributary of the River Eden with grassland land use. Thebeginning of the hydrological year was unusually dry and all threecatchments were in states of drought. A sudden change to a wet summeroccurred in April 2012 when a heavy rainfall event affected all threecatchments. The year-long time series and the individual storm responsescaptured by in situ nutrient measurements of nitrate and phosphorus (totalphosphorus and total reactive phosphorus) concentrations at each site revealdifferent pollutant sources and pathways operating in each catchment. Largestorm-induced nutrient transfers of nitrogen and or phosphorus to each streamwere recorded at all three sites during the late April rainfall event.Hysteresis loops suggested transport-limited delivery of nitrate in theBlackwater and of total phosphorus in the Wylye and Newby Beck, which wasthought to be exacerbated by the dry antecedent conditions prior to thestorm. The high rate of nutrient transport in each system highlights thescale of the challenges faced by environmental managers when designingmitigation measures to reduce the flux of nutrients to rivers from diffuseagricultural sources. It also highlights the scale of the challenge inadapting to future extreme weather events under a changing climate.
机译:本文使用从英国政府资助的示范测试集水区(DTC)项目中选出的三个集水区进行高频岸边测量。我们比较了2011-2012年水年期间埃文河的Wylye支流与混合土地利用,温苏姆河的黑水支流与可耕地利用以及伊甸河的纽比贝克支流与草地土地利用的水文和水化学模式。水文年开始时异常干旱,所有三个流域都处于干旱状态。 2012年4月,突然发生了一个潮湿的夏天,当时一场强降雨影响了所有三个集水区。为期一年的时间序列和通过对每个地点的硝酸盐和磷(总磷和总活性磷)浓度进行原位养分测量而捕获的单个风暴响应揭示了每个集水区的不同污染物来源和途径。在四月下旬的降雨事件中,在所有三个地点都记录到大暴风引起的氮和磷向各流的养分转移。磁滞回线表明黑水中硝酸盐的运移受限,而Wylye和Newby Beck中的总磷运移受限,据认为暴风雨来临前的干旱条件使情况更加恶化。每个系统中养分的高迁移率突显了环境管理者在设计缓解措施以减少养分从分散农业源流到河流时的挑战规模。它还强调了应对气候变化带来的未来极端天气事件的挑战的规模。

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