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Improved enrichment factor calculations through principal component analysis: Examples from soils near breccia pipe uranium mines, Arizona, USA

机译:通过主要成分分析改善了富集因子计算:来自布雷西亚管道铀矿山附近的土壤的例子,美国亚利桑那州

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The enrichment factor (EF) is a widely used metric for determining how much the presence of an element in a sampling media has increased relative to average natural abundance because of human activity. Calculation of an EF requires the selection of both a background composition and a reference element, choices that can strongly influence the result of the calculation. Here, it is shown how carefully applied, classical principal component analysis (PCA) examined via biplots can guide the selections of background compositions and reference elements. Elemental data were treated using the centered log ratio (CLR) transformation, and multiple subsets of major and trace elements were examined to gain different perspectives. The methodology was applied to a dataset of elemental soil concentrations from around breccia pipe uranium mines in Arizona, U.S.A., with most samples collected via incremental sampling methodology. Storage of ore at the surface creates the potential for wind dispersal of ore derived material. Uranium was found to be the best individual tracer of dispersal of ore-derived material to nearby soils, with EF values up to 75. Sulfur, As, Mo, and Cu were also enriched but to lesser degrees. The results demonstrate several practical benefits of a PCA in these situations: (1) the ability to identify one or more elements best suited to distinguish a specific source of enrichment from background composition; (2) understanding how background compositions vary within and between sites; (3) identification of samples containing enriched or anthropogenic materials based upon their integrated, multi-element composition. Calculating the most representative EF values is useful for numerical assessment of enrichment, whether anthropogenic or natural. As shown here, however, the PCA and biplot method provide a visual approach that integrates information from all elements for a given subset of data in a manner that yields geochemical insights beyond the power of the EF. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
机译:富集因子(EF)是广泛使用的指标,用于确定采样介质中的元素的存在相对于人类活动的平均天然丰度增加了多少。 EF的计算需要选择背景组合物和参考元素,可以强烈影响计算结果的选择。在这里,示出了通过双针检查的经典主成分分析(PCA)的经典主成分分析(PCA)如何指导背景组合物和参考元件的选择。使用以中心的日志比(CLR)转换处理元素数据,并检查多个主要和跟踪元素的子集以获得不同的观点。该方法应用于来自亚利桑那州的Breccia管铀矿周围的元素土壤浓度的数据集。,大多数通过增量采样方法收集的样本。矿石在表面上的储存会产生矿石衍生材料的风分散的可能性。发现铀是将矿石材料分散到附近土壤中的最佳单独示踪剂,高达75的EF值。硫,如MO和Cu也富集但是较小的程度。结果表明了在这些情况下PCA的几种实际效益:(1)能够确定最适合区分从背景组合物的特定富集来源的一个或多个元素; (2)了解背景组合物如何在地点内和之间变化; (3)鉴定基于其集成的多元素组成的含有富集或人为材料的样品。计算最代表性的EF值对于富集的数值评估是有用的,无论是人为的还是天然的。然而,如这里所示,PCA和Biplot方法提供了一种视觉方法,其以一种方式将来自所有元件的信息集成到给定的数据子集中的所有元素,以产生超出EF的功率的地球化学洞察。由elsevier有限公司发布这是CC下的开放式访问文章(http://creativecommomons.org/licenses/by/4.0/)。

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