首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Exploring uni-element geochemical data under a compositional perspective
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Exploring uni-element geochemical data under a compositional perspective

机译:在组成视角下探索UNI元素地球化学数据

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Different features of geochemical information were studied by comparing spatial distribution of concentration values and compositional data values. Geochemical data are compositional and should be treated as such to avoid spurious correlations and misleading interpretations. However, geochemists are also interested to discuss in terms of elemental concentrations. In this work the spatial distribution of Fe, Mn, Ti, Co, Cr, Ni and V based on 3535 topsoil samples collected in Campania region (Southern Italy) and analysed by ICP-MS after aqua regia digestion, is studied. Unielement maps and CoDA based maps, namely of ilr-transformed data and of two sub-compositions of 3 components have been produced and interpreted. Results show that the ilr maps often show different geochemical patterns from those provided by the maps based on raw concentrations, namely for V, Fe and Co. This is not surprising as each studied ilr is a (log) ratio of an element against the others and account for the compositional variability. Nevertheless, the geochemical patterns of both raw and ilr based maps relate mostly with the geolithological features of the region: (1) (Ti, Ni, Cr) log-ratio variables are the best pathfinder in differentiating between volcanic (relative enrichment in Ti) and non-volcanic (relative enrichment in Ni and Cr) areas. (2) Soil alteration phenomena could locally enhance log-ratios of Ti due its high geochemical stability. (3) The spatial analysis of ilr-Fe and ilr Mn variables amplifies their relative degree of enrichment in correspondence of silici-clastic formations suggesting that Mn-Fe oxides of clay minerals mainly dominate the geochemical composition of the soils of the survey area. (4) Local enrichments of Cr and Ni at the main rivers' mouths and in the metropolitan areas of Naples and Salerno, possibly of anthropogenic origin, are highlighted in the 3-part subcomposition analysis. The developed exploration methodology of uni-element geochemical data under a co
机译:通过比较浓度值的空间分布和组成数据值来研究地球化学信息的不同特征。地球化学数据是组成的,应该被视为为止,以避免杂散的相关性和误导性解释。然而,地球化学家也有兴趣在元素浓度方面讨论。在这项工作中,研究了基于在坎帕尼亚地区(意大利南部)收集的3535个Topsoil样品的Fe,Mn,Ti,Co,Cr,Ni和V的空间分布,并在Aqua Regia消化后由ICP-MS分析。基于UNIEREMENT地图和基于CODA的地图,即ILR转换数据和3个组分的两个子组合物的制作和解释。结果表明,ILR地图通常显示基于原始浓度的地图提供的不同地球化学模式,即V,FE和Co.这并不令人惊讶,因为每个研究ILR是对其他元素的元素的(对数)比率并占组合变异性。然而,基于原始和ILR的地图的地球化学模式主要与该区域的地铁学特征有关:(1)(Ti,Ni,Cr)对数变量是区分火山(相对富集)之间的最佳探测器。和非火山(NI和CR)区域的相对富集(相对富集)。 (2)土壤改变现象可以在地球化学稳定性高的情况下局部增强TI的逻辑比率。 (3)ILR-FE和ILR MN变量的空间分析在硅片形成的对应关系中放大了它们相对富集的富集程度,提示粘土矿物的MN-FE氧化物主要统治调查区域的土壤的地球化学组成。 (4)在3部分小组课题分析中突出了(4)主要河口嘴巴和NI,那不勒斯和萨洛诺的大都市和萨洛诺的大都市区的浓缩,并在3部分亚组织分析中突出显示。 CO下的UNI元地球化学数据发达的探索方法论

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