首页> 外文期刊>Science of the total environment >Soil-plant interactions and the uptake of Pb at abandoned mining sites in the Rookhope catchment of the N. Pennines, UK — A Pb isotope study
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Soil-plant interactions and the uptake of Pb at abandoned mining sites in the Rookhope catchment of the N. Pennines, UK — A Pb isotope study

机译:英国N. Pennines的Rookhope集水区废弃矿场的土壤植物相互作用和Pb的吸收— Pb同位素研究

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摘要

This paper examines Pb concentrations and sources in soil, grass and heather from the Rookhope catchment in the North Pennines, UK, an area of historical Pb and Zn mining and smelting. Currently, the area has extensive livestock and sports shooting industries. Risk assessment, using the source-pathway-receptor paradigm, requires the quantification of source terms and an understanding of the many factors determining the concentration of Pb in plants. A paired soil and vegetation (grass and heather) geochemical survey was undertaken. Results showed no direct correlation between soil (total or EDTA extractable Pb) and vegetation Pb concentration. However, regression modelling based on the Free-Ion Activity Model (FIAM) suggested that the underlying mechanism determining grass Pb concentration across the catchment was largely through root uptake. Spatial patterns of ~(206/207)pb isotopes suggested greater aerosol deposition of Pb on high moorland and prevailing wind facing slopes. This was evident in the isotopic ratios of the heather plants. Pb isotope analysis showed that new growth heather tips typically had ~(206/207)pb values of-1.14, whilst grass shoots typically had values -1.16 and bulk soil and peat -1.18. However, the ~(206/207)pb ratio in the top few cm of peat was -1.16 suggesting that grass was accessing Pb from a historical/recent pool of Pb in soil/peat profiles and consisting of both Pennine ore Pb and long-range Pb deposition. Isotope Dilution assays on the peat showed a lability of between 40 and 60%. A simple source apportionment model applied to samples where the isotope ratios was not within the range of the local Pennine Pb, suggested that grass samples contained up to 31 % of non-Pennine Pb. This suggests that the historical/recent reservoir of non-Pennine Pb accessed by roots continues to be a persistent contaminant source despite the principal petrol Pb source being phased out over a decade ago.
机译:本文研究了英国北彭尼山脉Rookhope集水区土壤,草和石南花中的Pb浓度和来源,该地区是历史悠久的Pb和Zn开采和冶炼地区。目前,该地区拥有广泛的畜牧和体育射击产业。使用源-途径-受体范式进行风险评估,需要对源术语进行量化,并且需要了解决定植物中Pb浓度的许多因素。进行了成对的土壤和植被(草和石南花)地球化学调查。结果表明,土壤(总或EDTA可萃取铅)与植被铅浓度之间没有直接关系。但是,基于自由离子活度模型(FIAM)的回归模型表明,确定流域中草Pb浓度的潜在机制主要是通过根系吸收。 〜(206/207)pb同位素的空间格局表明,高沼地和盛行的风向斜坡上Pb的气溶胶沉积量更大。这在石南花植物的同位素比率中是明显的。铅同位素分析显示,新的生长石南花尖端的〜(206/207)pb值通常为1.14,而草梢的值通常为-1.16,散装土壤和泥炭的值为-1.18。但是,泥炭最上面几厘米的〜(206/207)pb比为-1.16,这表明草是从土壤/豌豆剖面中历史/最近的Pb库中获取Pb的,包括Pennine矿石Pb和长Pb范围铅沉积。泥炭的同位素稀释分析显示不稳定性介于40%和60%之间。对于同位素比不在本地Pennine Pb范围内的样品,采用简单的源分配模型,表明草样品中的非Pennine Pb含量高达31%。这表明尽管十年前已逐步淘汰了主要的汽油铅源,但通过根获得的非石榴石铅的历史/最近储集层仍然是持久的污染物源。

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  • 来源
    《Science of the total environment》 |2012年第1期|p.547-560|共14页
  • 作者单位

    British Geological Survey, Keyworth Nottingham, NG12 5GG, UK;

    British Geological Survey, Keyworth Nottingham, NG12 5GG, UK;

    School of Biosciences, Sutton Botmington Campus, University of Nottingham, LE12 5RD, UK;

    British Geological Survey, Keyworth Nottingham, NG12 5GG, UK;

    British Geological Survey, Keyworth Nottingham, NG12 5GG, UK;

    British Geological Survey, Keyworth Nottingham, NG12 5GG, UK;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    lead; mining; isotopic dilution; plants; Pb isotopes; UK;

    机译:铅;矿业;同位素稀释植物;铅同位素;英国;
  • 入库时间 2022-08-17 13:54:47

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