Jarvi Helen P, Neal Colin, Williams Richard J, Neal Margaret, Wickham Heather D, Hill Linda K, Wade Andrew J, Warwick Alan, White John
Centre for Ecology and Hydrology, Wallingford, Oxfordshire, UK.
Sci Total Environ. 2002 Jan 23;282-283:175-203. doi: 10.1016/s0048-9697(01)00951-2.
This paper examines the behaviour of phosphorus (P) in a lowland chalk (Cretaceous-age) stream, the upper River Kennet in southern England, which has been subject to P remediation by tertiary treatment at the major sewage treatment works in the area. The effects of treatment are examined in relation to boron, a conservative tracer of sewage effluent and in terms of the relative contributions of soluble reactive phosphorus (SRP) loads from point and diffuse sources, and in-stream SRP loads. These results indicate a baseline reduction in in-stream SRP concentrations immediately following P-treatment of approximately 72%. Subsequent high flows result in a greater contribution of diffuse inputs and increases in SRP levels relative to the initial post-treatment period. The dynamics of SRP and particulate phosphorus (PP) are examined under a wide range of river flow conditions. Given the flashy nature of near-surface runoff in the River Kennet, sub-weekly (daily automated) sampling was used to examine the dynamics in SRP and PP concentrations in response to storm events. Simple empirical models linking weekly SRP concentrations with flow were developed. The empirical models were successfully applied to the daily data, to partition TP measurements and provide an estimate of daily SRP and PP concentrations. Mass balance studies were used to examine net gains and losses along the experimental river reach and indicate large net losses (up to 60%) during the extreme low flows and high SRP concentrations prior to P-treatment, which may be linked to extensive epiphytic growth. Phosphorus dynamics and response to P-treatment are discussed in relation to hydrological controls in permeable chalk catchments and wider implications for eutrophication management are examined.
本文研究了英格兰南部白垩纪低地河流肯尼特河上游磷(P)的行为,该河流域主要污水处理厂已通过三级处理进行磷修复。研究了处理效果与硼(污水排放的保守示踪剂)的关系,以及点源和非点源可溶性活性磷(SRP)负荷及河流中SRP负荷的相对贡献。这些结果表明,磷处理后,河流中SRP浓度立即出现基线下降,降幅约为72%。随后的高流量导致非点源输入的贡献更大,与初始处理后时期相比,SRP水平有所增加。在广泛的河流流量条件下,研究了SRP和颗粒态磷(PP)的动态变化。鉴于肯尼特河近地表径流的快速变化特性,采用每周次(每日自动)采样来研究SRP和PP浓度对暴雨事件的动态响应。建立了将每周SRP浓度与流量联系起来的简单经验模型。该经验模型成功应用于每日数据,用于划分总磷测量值,并估算每日SRP和PP浓度。采用质量平衡研究来考察实验河段的净增益和损失情况,结果表明,在磷处理前的极端低流量和高SRP浓度期间,存在大量净损失(高达60%),这可能与大量附生植物生长有关。本文结合渗透性白垩流域的水文控制,讨论了磷的动态变化及对磷处理的响应,并探讨了对富营养化管理的更广泛影响。