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泥炭土作为高地河流系统铅污染的一个来源。

Peat soils as a source of lead contamination to upland fluvial systems.

作者信息

Rothwell James J, Evans Martin G, Daniels Stephen M, Allott Timothy E H

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. 2008 Jun;153(3):582-9. doi: 10.1016/j.envpol.2007.09.009. Epub 2007 Oct 18.

Abstract

Upland peat soils are generally regarded as effective sinks of atmospherically deposited lead. However, the physical process of erosion has the potential to transform peat soils from sinks to sources of lead contamination. Lead input and fluvial lead outputs (dissolved+particulate) were estimated for a contaminated and severely eroding peatland catchment in the southern Pennines, UK. Lead input to the catchment is 30.0+/-6.0gha(-1)a(-1) and the output from the catchment is 317+/-22.4gha(-1)a(-1). Suspended particulate matter accounts for 85% of lead export. Contaminated peat soils of the catchment are a significant source of lead to the fluvial system. This study has demonstrated strong coupling between the physical process of erosion and the mobilization of lead into the fluvial system. The process of peat erosion should therefore be considered when estimating lead outputs from peatland catchments, especially in the context of climate change.

摘要

高地泥炭土通常被视为大气沉降铅的有效汇。然而,侵蚀的物理过程有可能将泥炭土从铅的汇转变为铅污染的源。对英国奔宁山脉南部一个受污染且严重侵蚀的泥炭地集水区的铅输入和河流铅输出(溶解态+颗粒态)进行了估算。该集水区的铅输入为30.0±6.0 g ha⁻¹ a⁻¹,集水区的铅输出为317±22.4 g ha⁻¹ a⁻¹。悬浮颗粒物占铅输出的85%。集水区受污染的泥炭土是河流系统中铅的重要来源。这项研究表明侵蚀的物理过程与铅向河流系统的迁移之间存在强耦合。因此,在估算泥炭地集水区的铅输出时,尤其是在气候变化的背景下,应考虑泥炭侵蚀过程。

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