首页> 外文期刊>Accreditation and quality assurance >Assessing soil sampling uncertainty in heterogeneous historic metal ore mining sites
【24h】

Assessing soil sampling uncertainty in heterogeneous historic metal ore mining sites

机译:评估异类历史金属矿山采矿场地的土壤采样不确定性

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Eighteen duplicate, composite soil samples from heterogeneous remote historic metal ore mining sites (Miedzianka Mt. and Karczwka Mt., south-central Poland) were analyzed twice for As, Cd, Co, Cr, Cu, Mn, Ni, Pb and Zn by the ICP-MS method after aqua regia extraction. Subsequently, the results were tested for normality. The sampling uncertainty [expressed as the relative standard deviation s (rsamp) (%)] was computed using three different methods: ANOVA, RANOVA and range statistics. However, it was possible to use all three methods only for Cr and Pb (Miedzianka) and for Co (Karczwka). The obtained values were in the ranges of: 15.6-16.0 % for Cr, 17.0-20.2 % for Co and 24.6-38.7 % for Pb. The sampling uncertainty for these elements that revealed non-normally distributed data was calculated using the robust ANOVA. The results varied from 12.1 % (As) to 31.9 % (Ni) in soils from Karczwka, and from 9.2 % (Co) to 35.9 % (Cu) in soils from Miedzianka. The highest s (rsamp) values exceeding 20 % were noted for Cd (31.9 %) and Ni (26.0 %) in soils from Karczwka, and for Cu (20.5 %) and Mn (35.9 %) in soils from Miedzianka. Because traditional methods of transformation were insufficient to reduce non-normality, the Box-Cox model was applied to these four elements. The sampling uncertainty, computed for transformed data with a one-way ANOVA method, was as follows: 20.1 % (Cd), 7.3 % (Ni), 4.6 % (Cu) and 4.6 % (Mn) and for back-transformed data: 39.7 % (Cd), 12.8 % (Ni), 7.4 % (Cu) and 12.4 % (Mn). The sampling uncertainty was lower compared to the values calculated with raw data, but the interpretation of results obtained was problematic.
机译:分别分析了18个来自异地偏远历史金属矿山开采地点(波兰中南部的Miedzianka山和Karczwka山)的复合土壤样品的As,Cd,Co,Cr,Cu,Mn,Ni,Pb和Zn的含量,进行了两次分析。王水萃取后的ICP-MS方法。随后,对结果进行正常性测试。抽样不确定度[表示为相对标准偏差s(rsamp)(%)]是使用三种不同的方法计算的:ANOVA,RANOVA和范围统计。但是,可能仅对Cr和Pb(Miedzianka)和Co(Karczwka)使用全部三种方法。所获得的值在以下范围内:Cr为15.6-16.0%,Co为17.0-20.2%,Pb为24.6-38.7%。使用稳健的ANOVA计算得出揭示非正态分布数据的这些元素的采样不确定性。在Karczwka的土壤中,结果从12.1%(As)到31.9%(Ni),在Miedzianka的土壤中,结果从9.2%(Co)到35.9%(Cu)。 Karczwka土壤中的Cd(31.9%)和Ni(26.0%)以及Miedzianka土壤中的Cu(20.5%)和Mn(35.9%)的最高s(斜率)值超过20%。由于传统的转换方法不足以减少非正态性,因此将Box-Cox模型应用于这四个元素。使用单向方差分析方法为转换后的数据计算的采样不确定度如下:20.1%(Cd),7.3%(Ni),4.6%(Cu)和4.6%(Mn)以及反向转换数据:分别为39.7%(Cd),12.8%(Ni),7.4%(Cu)和12.4%(Mn)。与原始数据计算的值相比,采样不确定度要低,但是对结果的解释存在问题。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号