Centre for Ecology and Hydrology, Maclean Building, Crowmarsh Gifford, Wallingford, OXON, OX10 8BB, UK.
Sci Total Environ. 2010 Oct 15;408(22):5306-16. doi: 10.1016/j.scitotenv.2010.08.010.
Information is provided on phosphorus in the River Kennet and the adjacent Kennet and Avon Canal in southern England to assess their interactions and the changes following phosphorus reductions in sewage treatment work (STW) effluent inputs. A step reduction in soluble reactive phosphorus (SRP) concentration within the effluent (5 to 13 fold) was observed from several STWs discharging to the river in the mid-2000s. This translated to over halving of SRP concentrations within the lower Kennet. Lower Kennet SRP concentrations change from being highest under base-flow to highest under storm-flow conditions. This represented a major shift from direct effluent inputs to a within-catchment source dominated system characteristic of the upper part to the catchment. Average SRP concentrations in the lower Kennet reduced over time towards the target for good water quality. Critically, there was no corresponding reduction in chlorophyll-a concentration, the waters remaining eutrophic when set against standards for lakes. Following the up gradient input of the main water and SRP source (Wilton Water), SRP concentrations in the canal reduced down gradient to below detection limits at times near its junction with the Kennet downstream. However, chlorophyll concentrations in the canal were in an order of magnitude higher than in the river. This probably resulted from long water residence times and higher temperatures promoting progressive algal and suspended sediment generations that consumed SRP. The canal acted as a point source for sediment, algae and total phosphorus to the river especially during the summer months when boat traffic disturbed the canal's bottom sediments and the locks were being regularly opened. The short-term dynamics of this transfer was complex. For the canal and the supply source at Wilton Water, conditions remained hypertrophic when set against standards for lakes even when SRP concentrations were extremely low.
提供了英格兰南部肯尼特河及其附近的肯尼特和埃文运河的磷信息,以评估它们的相互作用以及污水处理厂(STW)出水输入磷减少后的变化。从 21 世纪中期开始,从几个向河流排放的 STW 中观察到废水中可溶解性反应磷(SRP)浓度的显著降低(5 到 13 倍)。这导致下游肯尼特河的 SRP 浓度降低了一半以上。下游肯尼特河的 SRP 浓度从基流条件下最高变为暴雨条件下最高。这代表了一个从直接废水输入到以流域内源为主的系统的重大转变,这种系统是流域上游的特征。随着时间的推移,下游肯尼特河的平均 SRP 浓度朝着良好水质的目标减少。至关重要的是,叶绿素-a 浓度没有相应降低,与湖泊标准相比,水质仍然处于富营养化状态。在主要水源和 SRP 源(威尔顿水)的上游输入之后,运河中的 SRP 浓度在下游与肯尼特河的交汇处附近有时会降低到检测限以下。然而,运河中的叶绿素浓度比河流中的高一个数量级。这可能是由于长时间的停留时间和较高的温度促进了藻类和悬浮沉积物的不断产生,从而消耗了 SRP。运河特别是在夏季,当船只交通干扰运河底部沉积物和经常打开船闸时,成为向河流输送沉积物、藻类和总磷的点源。这种转移的短期动态很复杂。对于运河和威尔顿水的供应源来说,即使 SRP 浓度极低,与湖泊标准相比,它们仍然处于富营养状态。