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对比控制英格兰北部退化泥炭地集水区的砷和铅预算。

Contrasting controls on arsenic and lead budgets for a degraded peatland catchment in Northern England.

机构信息

Upland Environments Research Unit, School of Environment and Development, The University of Manchester, Manchester M13 9PL, UK.

出版信息

Environ Pollut. 2011 Oct;159(10):3129-33. doi: 10.1016/j.envpol.2011.05.026. Epub 2011 Jun 16.

Abstract

Atmospheric deposition of trace metals and metalloids from anthropogenic sources has led to the contamination of many European peatlands. To assess the fate and behaviour of previously deposited arsenic and lead, we constructed catchment-scale mass budgets for a degraded peatland in Northern England. Our results show a large net export of both lead and arsenic via runoff (282 ± 21.3 gPb ha(-1) y(-1) and 60.4 ± 10.5 gAs ha(-1) y(-1)), but contrasting controls on this release. Suspended particulates account for the majority of lead export, whereas the aqueous phase dominates arsenic export. Lead release is driven by geomorphological processes and is a primary effect of erosion. Arsenic release is driven by the formation of a redox-dynamic zone in the peat associated with water table drawdown, a secondary effect of gully erosion. Degradation of peatland environments by natural and anthropogenic processes has the potential to release the accumulated pool of legacy contaminants to surface waters.

摘要

人为源大气沉降的痕量金属和类金属已导致许多欧洲泥炭地受到污染。为了评估先前沉积的砷和铅的命运和行为,我们为英格兰北部一个退化的泥炭地构建了流域尺度的物质预算。我们的结果表明,通过径流水(282 ± 21.3 gPb ha(-1) y(-1) 和 60.4 ± 10.5 gAs ha(-1) y(-1))大量净输出铅和砷,但释放的控制因素相反。悬浮颗粒是铅输出的主要原因,而水相则主导砷的输出。铅的释放是由地貌过程驱动的,是侵蚀的主要影响。砷的释放是由与地下水位下降相关的泥炭中氧化还原动态带的形成驱动的,这是沟壑侵蚀的次要影响。自然和人为过程对泥炭地环境的退化有可能将积累的遗留污染物库释放到地表水。

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