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Assessing stream restoration effectiveness at reducing nitrogen export to downstream waters

机译:评估河流恢复的有效性,以减少向下游水域的氮出口

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The degradation of headwater streams is common in urbanized coastal areas, and the role these streams play in contributing to downstream pollution is a concern among natural resource managers and policy makers. Thus, many urban stream restoration efforts are increasingly focused on reducing the downstream flux of pollutants. In regions that suffer from coastal eutrophication, it is unclear whether stream restoration does in fact reduce nitrogen (N) flux to downstream waters and, if so, by how much and at what cost. In this paper, we evaluate whether stream restoration implemented to improve water quality of urban and suburban streams in the Chesapeake Bay region, USA, is effective at reducing the export of N in stream flow to downstream waters. We assessed the effectiveness of restored streams positioned in the upland vs. lowland regions of Coastal Plain watershed during both average and stormflow conditions. We found that, during periods of low discharge, lowland streams that receive minor N inputs from groundwater or bank seepage reduced in-stream N fluxes. Furthermore, lowland streams with the highest N concentrations and lowest discharge were the most effective. During periods of high flow, only those restoration projects that converted lowland streams to stream-wetland complexes seemed to be effective at reducing N fluxes, presumably because the design promoted the spillover of stream flow onto adjacent floodplains and wetlands. The observed N-removal rates were relatively high for stream ecosystems, and on the order of 5% of the inputs to the watershed. The dominant forms of N entering restored reaches varied during low and high flows, indicating that N uptake and retention were controlled by distinctive processes during different hydrological conditions. Therefore, in order for stream restoration to effectively reduce N fluxes exported to downstream waters, restoration design should include features that enhance the processing and retention of different forms of N, and for a wide range of flow conditions. The use of strategic designs that match the dominant attributes of a stream such as position in the watershed, influence of groundwater, dominant flow conditions, and N concentrations is crucial to assure the success of restoration.
机译:在城市化的沿海地区,源头水流的退化很普遍,而这些水流在造成下游污染中所扮演的角色是自然资源管理者和决策者的关注点。因此,许多城市河流恢复工作越来越集中于减少下游污染物的排放量。在遭受沿海富营养化的地区,目前尚不清楚河流恢复是否确实会减少流向下游水域的氮(N)通量,如果减少的话,将减少多少,以及降低多少成本。在本文中,我们评估了为改善美国切萨皮克湾地区的城市和郊区溪流水质而实施的溪流恢复是否能有效减少溪流向下游水域中氮的出口。我们评估了在平均和暴雨条件下,位于沿海平原流域的高地与低地地区的恢复河流的有效性。我们发现,在低流量时期,接收来自地下水或堤岸渗漏的少量N输入的低地溪流减少了流入N流量。此外,氮浓度最高,排放量最低的低地溪流最为有效。在高流量时期,只有那些将低地溪流转变为溪流-湿地综合体的修复项目似乎对减少氮通量有效,这大概是因为该设计促进了溪流向邻近洪泛区和湿地的溢出。对于河流生态系统,观察到的氮去除率相对较高,约为流域投入的5%。进入恢复河段的氮的主要形式在低流量和高流量期间变化,这表明在不同的水文条件下,氮的吸收和保留受独特过程控制。因此,为了使河流恢复能有效减少出口到下游水域的氮通量,恢复设计应包括可在各种流动条件下增强对不同形式氮素的处理和保留的功能。使用与河流的主要属性相匹配的战略设计,例如流域中的位置,地下水的影响,主要水流条件和氮浓度,对于确保恢复成功至关重要。

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