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Heterogeneous areas—identification of outliers and calculation of soil sampling uncertainty using the modified RANOVA method

机译:异质区域—异常值的识别和使用改良的RANOVA方法计算土壤采样不确定度

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摘要

We modified the robust analysis of variance (RANOVA) method to calculate sampling uncertainty of selected trace elements determined in soil samples from two heterogeneous remote historic metal ore mining areas. Classical RANOVA is down-weighting the outlying values by replacing them during the calculation process with mean ± c·σ r. Because the arithmetic mean is greatly influenced by outliers, it cannot represent a robust statistic. The main novel contribution of this work is use of median value that is independent on outliers and replace all extreme values during the calculation process with median ± 2·σ r. In our work, 18 duplicate, composite soil samples were collected, digested with aqua regia in a closed microwave system, and analyzed twice for selected trace elements. To extract homogenous groups within sampling areas and make the results more accessible for interpretation, a cluster analysis was done. Subsequently, histograms of each element were prepared and statistical tests were applied to determine the normal distribution of datasets. For abnormally distributed elements, the outlying values were identified by four different methods: boxplot, mean ± c·σ r, mean ± c·σ, and median ± 2·σ r. For five elements, the amount of outliers identified by the median ± 2·σ r procedure was less than 10 %, and for these elements, the sampling uncertainty was computed using a modified RANOVA method. The sampling uncertainty computed with this method was 28.9 % for Cd, 15.2 % for Co, 14.5 % for Mn, 12.7 % for Ni, and 16.3 % for Zn, whereas that computed with a traditional model was 16.7 % for Cd, 9.2 % for Co, 20.5 % for Mn, 17.9 % for Ni, and 16.3 % for Zn.Electronic supplementary materialThe online version of this article (doi:10.1007/s10661-016-5584-9) contains supplementary material, which is available to authorized users.
机译:我们修改了方差分析(RANOVA)的稳健性分析方法,以计算在两个不同的偏远历史金属矿石开采区的土壤样品中确定的选定微量元素的采样不确定性。古典RANOVA通过在计算过程中将平均值替换为平均值±c·σr来降低外围值的权重。由于算术平均值受异常值的影响很大,因此它不能表示可靠的统计量。这项工作的主要新颖贡献是使用独立于离群值的中值,并在计算过程中将所有极值替换为中值±2·σr。在我们的工作中,收集了18个重复的复合土壤样品,在一个封闭的微波系统中用王水消化,并两次分析了选定的痕量元素。为了提取采样区域内的同质基团并使结果更易于解释,进行了聚类分析。随后,准备每个元素的直方图,并进行统计检验以确定数据集的正态分布。对于异常分布的元素,通过四种不同的方法来标识离群值:箱线图,均值±c·σr,均值±c·σ和中位数±2·σr。对于五个元素,通过中位数±2·σr程序确定的异常值小于10%,对于这些元素,使用改进的RANOVA方法计算采样不确定度。用这种方法计算的样品不确定度为Cd为28.9%,Co为15.2%,Mn为14.5%,Ni为12.7%,Zn为16.3%,而传统模型计算的不确定度为Cd为16.7%,Cd为9.2% Co,Mn占20.5%,Ni占17.9%,Zn占16.3%电子补充材料本文的在线版本(doi:10.1007 / s10661-016-5584-9)包含补充材料,可供授权用户使用。

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