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英格兰南部邓河、肯尼特和埃文运河以及肯尼特河中的磷浓度。

Phosphorus concentrations in the River Dun, the Kennet and Avon Canal and the River Kennet, southern England.

作者信息

Neal Colin, House W Alan, Jarvie Helen P, Neal Margaret, Hill Linda, Wickham Heather

机构信息

Centre for Ecology and Hydrology, Maclean Building, Crowmarsh Gifford, Wallingford, OXON, OX10 8BB, UK.

出版信息

Sci Total Environ. 2005 May 15;344(1-3):107-28. doi: 10.1016/j.scitotenv.2005.02.009. Epub 2005 Mar 21.

Abstract

Variations in phosphorus (P) concentrations in an agriculturally impacted river draining a Chalk aquifer and an associated canal in the west of the Thames Basin, southern England are examined and linked to agricultural and sewage sources and within river/canal process controls. The study area comprises the River Dun, the adjacent River Kennet and the Kennet and Avon (K&A) Canal. Large seasonal variations are observed for soluble reactive phosphorus (SRP) and dissolved silicon (Si) with low concentrations in the spring and summer times when biological activity is high. The K&A Canal shows the largest SRP and Si concentration declines. This reflects high biological activity coupled with higher temperatures and higher water residence times. The extent of SRP removal is examined in relation to organic (uptake/release with phytoplankton growth/decay) and, to a lesser extent, inorganic (SRP coprecipitation with calcite) mechanisms. Boron (B) is used as a tracer of sewage sources. Agricultural inputs of both dissolved and particulate P (PP) can be important particularly under conditions where the catchment is wet and near surface/overland flow is important: sewage treatment works effluent and septic tank discharges to groundwater also probably provide a major component of the SRP occurring within the water column. The canal, and to a lesser extent the river, acts as sink for P in sewage effluent sources due to the high biological activity especially during the spring and summer. The aquifer probably acts as a major sink for agricultural and septic tank inputs of P.

摘要

对英格兰南部泰晤士河流域西部一条受农业影响的、流经白垩含水层的河流及其相关运河中的磷(P)浓度变化进行了研究,并将其与农业和污水来源以及河流/运河内部的过程控制联系起来。研究区域包括邓河、相邻的肯尼特河以及肯尼特和埃文(K&A)运河。可溶性活性磷(SRP)和溶解硅(Si)呈现出较大的季节性变化,在生物活性较高的春季和夏季浓度较低。K&A运河的SRP和Si浓度下降幅度最大。这反映了高生物活性以及较高的温度和较长的水体停留时间。研究了SRP去除程度与有机机制(随浮游植物生长/衰退的吸收/释放)以及在较小程度上与无机机制(SRP与方解石的共沉淀)之间的关系。硼(B)被用作污水来源的示踪剂。溶解态和颗粒态磷(PP)的农业输入可能很重要,特别是在集水区湿润且近地表/坡面流很重要的情况下:污水处理厂的废水和化粪池向地下水的排放也可能是水柱中SRP的主要组成部分。由于高生物活性,尤其是在春季和夏季,运河以及在较小程度上河流充当了污水排放源中磷的汇。含水层可能是农业和化粪池磷输入的主要汇。

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