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首页> 外文期刊>Environmental Earth Sciences >High cadmium concentrations in Jurassic limestone as the cause for elevated cadmium levels in deriving soils: a case study in Lower Burgundy, France
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High cadmium concentrations in Jurassic limestone as the cause for elevated cadmium levels in deriving soils: a case study in Lower Burgundy, France

机译:侏罗纪石灰岩中的高镉浓度是衍生土壤中镉水平升高的原因:以法国下勃艮第为例

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Cadmium (Cd) is a highly toxic element and its presence in the environment needs to be closely monitored. Recent systematic surveys in French soils have revealed the existence of areas in eastern and central France, which show systematically high cadmium concentrations. It has been suggested that at least part of these anomalous levels are of natural origin. For the Lower Burgundy area in particular, a direct heritage from the Jurassic limestone bedrock is highly suspected. This potential relationship has been studied in several localities around Avallon and this study reports new evidence for a direct link between anomalously elevated cadmium contents of Bajocian and Oxfordian limestone and high cadmium concentrations in deriving soils. Soils in this area show cadmium concentrations generally above the average national population values, with contents frequently higher than the ‘upper whisker’ value of 0.8 μg g−1 determined by statistical evaluation. In parallel, limestone rocks studied in the same area exhibit cadmium concentrations frequently exceeding the mean value of 0.030–0.065 μg g−1 previously given for similar rocks by one order of magnitude, with a maximum of 2.6 μg g−1. Mean ratios between the cadmium concentrations of limestone bedrock and deriving soils (Cdsoil/Cdrock), calculated for different areas, range from 4.6 to 5.7. Calculations based on the analyses of both soils from a restricted area and fragments of bedrock sampled in the immediate vicinity of high-concentration soils are around 5.5–5.7. Cdsoil/Cdrock is useful in determining the potential of soils in Lower Burgundy to reflect and exacerbate the high concentrations of cadmium present in parent bedrocks.
机译:镉(Cd)是一种剧毒元素,需要密切监测其在环境中的存在。最近在法国土壤中进行的系统性调查显示,法国东部和中部存在着一些区域,这些区域显示出系统性的高镉浓度。已经提出这些异常水平的至少一部分是自然起源的。特别是对于下勃艮第地区,人们强烈怀疑侏罗纪石灰岩基岩的直接遗产。已经在阿瓦隆附近的几个地方研究了这种潜在的关系,这项研究报告了新的证据,表明巴约西亚和牛津石灰石中异常升高的镉含量与衍生土壤中的高浓度镉之间存在直接联系。该地区的土壤中镉的浓度通常高于全国平均水平,其含量经常高于通过统计评估确定的“晶须上限值” 0.8μgg -1 。同时,在同一地区研究的石灰岩岩石显示出的镉浓度经常超过类似岩石先前给出的平均值0.030-0.065μgg -1 一个数量级,最大为2.6μg g -1 。计算出的不同地区的石灰岩基岩和衍生土壤(Cd 土壤 / Cd 岩石)中镉的平均比值范围为4.6至5.7。基于对有限区域土壤和高浓度土壤附近采样的基岩碎片的分析,计算值约为5.5-5.7。 Cd soil / Cd rock 可用于确定勃艮第下游地区土壤反映和加剧母体基岩中高浓度镉的潜力。

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