利用无监督机器学习和成分数据分析识别不同土壤类型中潜在有毒元素的空间集群

Gevorg Tepanosyan, Zhenya Poghosyan, Lilit Sahakyan
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引用次数: 0

摘要

土壤健康非常重要,包括潜在有毒元素在内的土壤化学成分数据是其概念组成部分之一。本研究旨在揭示亚美尼亚阿拉加措滕地区土壤潜在有毒元素含量的空间分布模式,确定其潜在来源,并揭示其地球化学关联。为此,使用 X 射线荧光光谱仪测定了 Cr、V、Ti、As、Zn、Cu、Co、Fe、Mn、Ba 和 Pb 的含量。铬和砷的平均含量分别超出大陆地壳上限的 1.5 倍和 3.1 倍,超出最大可接受值的 1.5 倍和 1.5 倍。分析表明,在一些地点,所有这些元素的含量都相对较高。成分数据分析和地理空间制图的综合应用揭示了多变量异常值,这些异常值位于矿石开采活跃的构造-成矿带。无监督机器学习算法的应用揭示了主数据集中的三个组,clr-biplot 确定了特定来源元素。其中,I 组包括铜,其平均值在已确定的各组中最高。I 组中的土壤样本位于钙质土壤发达的地区,相对较高的铜含量归因于农业活动和汽车尾气排放。第二组以铁、钴、铬、锰、锌和砷的地球化学组合为代表。该组的形成受当地地质起源的火山岩影响。不过,第二组的分布与土壤类型并不一致。第 III 组包括钛、钒、铅和钡,可能有混合来源,因为其空间分布在区域高速公路经过的地区,而第 II 组元素也在这些地区显示出较高的数值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Identification of spatial clusters of potentially toxic elements in different soil types using unsupervised machine learning and compositional data analysis

Identification of spatial clusters of potentially toxic elements in different soil types using unsupervised machine learning and compositional data analysis

Soil health is important, with soil chemical composition data, including potentially toxic elements (PTEs) being one of its conceptual components. This study aims to reveal the spatial distribution patterns of soil PTEs contents, identify their potential sources, and unveil their geochemical associations in Aragatsotn region, Armenia. For that purpose, the contents of Cr, V, Ti, As, Zn, Cu, Co, Fe, Mn, Ba, and Pb were determined using an X-ray fluorescence spectrometer. The mean contents of Cr and As exceeded their upper continental crust by 1.5 and 3.1 times and their maximum acceptable values by 1.5 and 1.5 times. The analysis demonstrated the presence of sites where all these elements displayed comparatively higher values. The combined application of compositional data analysis and geospatial mapping revealed multivariate outliers, which were located in structural-metallogenic zones with active ore exploitation . The application of unsupervised machine learning algorithm unveiled three groups within the main dataset and the clr-biplot identified the source-specific elements. Particularly, Group I included Cu and displayed the highest mean value among the identified groups. The soil samples included in Group I were in areas where Calcisols were developed and comparatively high Cu contents were attributed to agricultural activities and vehicle emissions. Group II is represented by the geochemical association of Fe, Co, Cr, Mn, Zn, and As. The formation of this group is conditioned by volcanic rocks of the local geological origin. However, no spatial pattern was identified in Group II distribution aligned with soil types. Group III included Ti, V, Pb, and Ba, which may have a mixed origin as it is spatially distributed in areas where regional highways pass through and where Group II elements also exhibit their higher values.

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