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Effective radium concentration in topsoils contaminated by lead and zinc smelters

机译:铅和锌冶炼厂污染的表层土壤中有效镭浓度

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Trace elements (TE) are indicative of industrial pollution in soils, but geochemical methods are difficult to implement in contaminated sites with large numbers of samples. Therefore, measurement of soil magnetic susceptibility (MS) has been used to map TE pollutions, albeit with contrasted results in some cases. Effective radium concentration (EC_(Ra)), product of radium concentration by the emanation factor, can be measured in a cost-effective manner in the Laboratory, and could then provide a useful addition. We evaluate this possibility using 186 topsoils sampled over about 783 km~(-2) around two former lead and zinc smelters in Northern France. The EC_(Ra) values, obtained from 319 measurements, range from 0.70 ± 0.06 to 12.53 ± 0.49 Bq·kg~(-1), and are remarkably organized spatially, away from the smelters, in domains corresponding to geographical units. Lead-contaminated soils, with lead concentrations above 100 mg·kg~(-1) <3 km from the smelters, are characterized on average by larger peak EC_(Ra) values and larger dispersion. At large scales, away from the smelters, spatial variations of EC_(Ra) correlate well with spatial variations of MS, thus suggesting that, at distance larger than 5 km, variability of MS contains a significant natural component Larger EC_(Ra) values are correlated with larger fine fraction and, possibly, mercury concentration. While MS is enhanced in the vicinity of the smelters and is associated with the presence of soft ferrimagnetic minerals such as magnetite, it does not correlate systematically with metal concentrations. When multiple industrial and urban sources are present, EC_(Ra) mapping, thus, can help in identifying at least part of the natural spatial variability of MS. More generally, this study shows that EC_(Ra) mapping provides an independent and reliable assessment of the background spatial structure which underlies the structure of a given contamination. Furthermore, EC_(Ra) may provide a novel index to identify soils potentially able to fix leached components.
机译:痕量元素(TE)指示土壤工业污染,但地球化学方法难以在有大量样品的受污染场地中实施。因此,尽管在某些情况下具有对比结果,但土壤磁化率(MS)的测量已用于绘制TE污染图。有效镭浓度(EC_(Ra)),即镭浓度与发射因子的乘积,可以在实验室中以经济有效的方式进行测量,然后可以提供有用的添加。我们使用法国北部两个前铅锌冶炼厂周围约783 km〜(-2)采样的186种表土评估了这种可能性。通过319次测量获得的EC_(Ra)值在0.70±0.06到12.53±0.49 Bq·kg〜(-1)范围内,并且在远离冶炼厂的位置上在明显的空间结构中对应于地理单位。距冶炼厂铅浓度大于100 mg·kg〜(-1)<3 km的铅污染土壤的平均特征是具有较大的EC_(Ra)峰值和较大的分散度。在远离冶炼厂的大范围内,EC_(Ra)的空间变化与MS的空间变化密切相关,因此表明,在大于5 km的距离处,MS的可变性包含显着的自然成分。EC_(Ra)值较大。与较大的细颗粒含量以及可能的汞浓度相关。虽然MS在冶炼厂附近得到增强,并且与软亚铁磁性矿物(如磁铁矿)的存在相关,但它与金属浓度没有系统地关联。因此,当存在多个工业和城市来源时,EC_(Ra)映射可以帮助识别MS的自然空间变异性的至少一部分。更广泛地说,这项研究表明EC_(Ra)映射可对背景空间结构进行独立而可靠的评估,而背景空间结构是给定污染物结构的基础。此外,EC_(Ra)可以提供一种新颖的指标来识别潜在地能够修复沥滤成分的土壤。

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