圣卡塔琳娜州南部地区地表水资源——煤炭开采地区的地球化学背景

Pub Date : 2022-01-01 DOI:10.1590/2318-0331.272220220084
Albert Teixeira Cardoso, F. Fan, Melissa Franzen, G. Simão, Guilherme Casarotto Troian
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引用次数: 0

摘要

在环境复垦过程中,区分水资源中自然产生的化学元素浓度(地球化学背景)与人为活动产生的化学元素浓度是至关重要的。尽管在受煤矿开采影响的巴西南部地区进行了二十多年的环境努力,但其地球化学背景仍然不完全清楚。填补这一环境知识空白是这项工作的目标,该工作系统地分析了巴西地质调查局(SGB/CPRM)三年来开展的监测工作的结果。分析了未受人为影响的河川水质参数分布。利用数据库进行主成分分析(PCA)和聚类分析,并通过箱线图(boxplot)和±2 MAD (Median Absolute Deviation)方法确定背景值。多元统计分析结果将监测点分为两组,一组与帕拉南盆地的沉积岩有关,另一组与结晶基底岩有关。沉积组与Eh、SO42-、Ca、Mg、EC、Mn、酸度、Zn、Na等参数相关性较强;结晶岩组与pH、Cu、Al、K、Fe的相关性较好。两种方法的地球化学背景结果相似,pH、Fe、Al和Mn的值与巴西立法(CONAMA 357/05和MS 888/21)中定义的值略有不同。
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Surface water resources of Santa Catarina state’s southern region - geochemical background of the coal mining territory
ABSTRACT In the environmental reclaiming process, it is essential to distinguish between chemical elements concentrations that occur naturally in water resources (geochemical background), from those originated from anthropogenic activities. Despite the environmental efforts that have been carried out for more than two decades in the southern Brazilian region impacted by coal mining, its geochemical background is still not completely known. Filling this environmental knowledge gap was the objective of this work, which systematically analyzed the results of monitoring efforts carried out by the Geological Survey of Brazil (SGB/CPRM) across three years. Quality parameter distributions of rivers and streams unaffected by anthropogenic impact were analyzed. The database was used to perform principal component analysis (PCA) and cluster analysis, and to define the background values, which was done through the boxplot and ± 2 MAD (Median Absolute Deviation) methods. The results of multivariate statistical analyses clustered the monitoring sites into two groups, one related to the sedimentary rocks of the Paraná Basin and another to the crystalline basement rocks. The sedimentary group had a greater correlation with the parameters Eh, SO42-, Ca, Mg, EC, Mn, Acidity, Zn and Na; while, and the crystalline rocks group were better correlated with pH, Cu, Al, K, and Fe. The results of the geochemical background were similar for both methods, with values of pH, Fe, Al, and Mn being slightly different from those defined in Brazilian legislation (CONAMA 357/05 and MS 888/21).
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