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首页> 外文期刊>Journal of Hydrology >Evaluating diffuse and point phosphorus contributions to river transfers at different scales in the Taw catchment, Devon, UK
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Evaluating diffuse and point phosphorus contributions to river transfers at different scales in the Taw catchment, Devon, UK

机译:在英国德文郡的Taw流域评估扩散磷和点磷对河流转移的不同规模贡献

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This paper describes an empirical study carried out to improve understanding of how small scale transfers of mobilised phosphorus (P) recorded at plot to field scale are mirrored by P fluxes measured at the river catchment scale. Phosphorus transfers were studied in partially nested sites that range in area from 30 m(2) to 834 km(2). The work was carried out within the grassland dominated catchment of the River Taw, south west England. The research sought to determine the characteristics of the link between plot and river scale P fluxes for different P forms. The highest point source inputs of P were generally recorded in the largest sub-catchments of the river. However, diffuse sources of P were estimated to constitute at least 60% of the annual P flux at all sites. The magnitude of the diffuse P input varied with catchment land use. Detailed studies focused on the lowland catchments showed that diffuse fluxes can be well represented by plot and field scale P transfers. The research produced no evidence for significant inputs of P from river channel banks. However, at the hillslope scale, additional transfers of P from 'incidental' sources such as re-seeded fields, open access ditches, and farmyard point sources were recorded. These inputs did not appear to significantly affect river P fluxes, suggesting that they are either of low frequency, or that there is a corresponding decrease in overall P transfer as the research scale is increased from field through to sub-catchment. Additional evidence of scaling was observed where riverine P fluxes were diluted by upland or groundwater flows. (c) 2005 Elsevier B.V. All rights reserved.
机译:本文描述了一项实证研究,以增进对在流域尺度上测得的P通量如何反映在样地向田间尺度上记录的动员磷(P)小规模转移的理解。在范围从30 m(2)到834 km(2)的部分嵌套站点中研究了磷的迁移。这项工作是在英格兰西南部的托河(River Taw)的草场为主的流域内进行的。该研究试图确定不同P形态的地块与河流尺度P通量之间的联系特征。 P的最高点源输入通常记录在河流的最大子汇水区。但是,据估计,所有地点的P扩散源至少占年度P通量的60%。扩散P输入量随集水区土地利用而变化。针对低地流域的详细研究表明,散点通量可以通过地块和田间尺度的P转移很好地表示。该研究没有证据表明河道岸边有大量的磷投入。但是,在山坡规模上,还记录了来自“偶然”源(例如重新播种的田地,开放式沟渠和农家点源)的额外P转移。这些投入似乎并未显着影响河流的磷通量,表明它们要么频率较低,要么随着研究规模从田间到子汇水面积的增加,总体磷的输送量相应减少。在高地或地下水流稀释了河流磷通量的地方,还观察到了结垢的证据。 (c)2005 Elsevier B.V.保留所有权利。

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