首页> 外文期刊>Journal of Hydrology >Role of river bed sediments as sources and sinks of phosphorus across two major eutrophic UK river basins: the Hampshire Avon and Herefordshire Wye
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Role of river bed sediments as sources and sinks of phosphorus across two major eutrophic UK river basins: the Hampshire Avon and Herefordshire Wye

机译:河床沉积物在整个两个主要富营养化英国流域(汉普郡雅芳和赫里福德郡怀氏)中作为磷源和汇的作用

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The Equilibrium Phosphorus Concentration (EPC0) of river bed sediments has been measured for a wide range of agricultural subcatchments and main river sites across two major eutrophic river basins: the Hampshire Avon and Herefordshire Wye catchments, to examine whether bed sediments are acting as sources or sinks of soluble reactive phosphorus (SRP) under low flows and times of greatest eutrophication risk. A conceptual reach-based model of interactions between bed sediment and river water has been used to estimate relative differences in bed-sediment SRP flux transfers. In this model, processes of SRP uptake and release are assumed to occur within an operationally defined 0.1 m river water 'boundary layer' and the uptake and release of SRP is assumed to be driven by a differential between the EPC0 of the sediment and SRP concentration in the boundary layer. Most of the river monitoring sites in the Wye and Avon catchments had elevated SRP and boron (B) concentrations in the water column at low flows, linked to sewage effluent discharges. At these sites, bed sediments consistently acted as net sinks for SRP, demonstrating the role of bed sediments in riverine 'self-cleansing' mechanisms. In contrast, bed sediments were found to act as net sources of SRP under three circumstances: (i) where there was minimal sewage influence (in headwater streams of the Avon), (ii) where sewage inputs were subject to large hydrological dilution by water of low SRP concentration (in the main River Wye), (iii) where EPC0 values were relatively high, as a result of deposition of particulates with high exchangeable P concentrations from diffuse sources or from effluents (immediately downstream of sewage treatment works (STWs)). Under baseflow conditions, high SRP concentrations from sewage effluent in the tributaries appear to 'swamp out' any potential release of SRP from the bed sediments. For rivers that are subject to effluent P-stripping, reductions in SRP in the overlying water could potentially result in changes to the in-stream P-cycling mechanisms, with bed sediments possibly switching from net sinks to net sources of SRP. This feature is of potential importance in relation to environmental management and phosphorus mitigation operations. (c) 2004 Elsevier B.V. All rights reserved.
机译:已测量了汉普郡雅芳和赫里福德郡怀河两个主要富营养化流域的各种农业子汇水区和主要河床的河床沉积物的平衡磷浓度(EPC0),以检查河床沉积物是作为源还是作为低流量和最大富营养化时间下的可溶性反应性磷(SRP)汇。基于概念范围的河床沉积物与河水之间相互作用的模型已用于估算河床沉积物SRP通量传递的相对差异。在该模型中,假定SRP的吸收和释放过程发生在可操作定义的0.1 m河流水“边界层”内,并且假设SRP的吸收和释放是由沉积物的EPC0和SRP浓度之间的差异驱动的在边界层。在怀河和雅芳河集水区的大多数河流监测点,水流中的SRP和硼(B)浓度低,流量低,与污水排放有关。在这些地点,河床沉积物始终充当SRP的净汇,表明河床沉积物在河流“自我清洁”机制中的作用。相反,在以下三种情况下,发现床层沉积物是SRP的净来源:(i)污水影响最小(在雅芳的源头水流中),(ii)污水输入受到水的大水文稀释SRP浓度较低(在怀河中),(iii)EPC0值相对较高,这是由于来自分散源或废水(紧接在污水处理厂(STWs)的下游)沉积了具有高交换性P浓度的颗粒)。在基流条件下,支流中污水中的高SRP浓度似乎“淹没”了床层沉积物中SRP的任何潜在释放。对于易受污水P排污的河流,上层水中SRP的降低可能会导致河流P循环机制的改变,河床沉积物可能会从SRP的净汇变为净SRP的来源。此功能对于环境管理和减磷操作具有潜在的重要性。 (c)2004 Elsevier B.V.保留所有权利。

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