首页> 外文期刊>Geoderma: An International Journal of Soil Science >Combining marginal and spatial outliers identification to optimize the mapping of the regional geochemical baseline concentration of soil heavy metals
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Combining marginal and spatial outliers identification to optimize the mapping of the regional geochemical baseline concentration of soil heavy metals

机译:结合边缘和空间离群值识别来优化土壤重金属区域地球化学基线浓度的制图

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The geochemical baseline concentration is used as a reference to determine the state of an area in relation to soil pollution. Various methods have been developed to determine this concentration based on filtering either the marginal or the spatial outliers. Marginal outlier identification (MOI) classifies data as belonging to the geochemical baseline or representing pollution using a globally defined single threshold value. As a result it neglects the local scale variability of the geochemical baseline level that arises from possible differences in parent material and the presence of multiple pollutants with variable degrees of influence. Hence it might lead to the identification of enrichments below the globally defined threshold but still larger than the local geochemical baseline level as belonging to the geochemical baseline. Spatial outlier identification (SOI) focuses on detecting unusual values in a local neighbourhood. As SOI is strongly dependent on data configuration, clusters of high values might wrongly be accepted as being geochemical baseline data that can inflate geochemical baseline level in pollution risk areas. The limitations of MOI and SOI can be severe when applied for a large scale study. To avoid these limitations and maximize the benefit of the two methods we proposed a combined methodology: integrated outliers identification (IOI) using fuzzy and robust means to determine the geochemical baseline measurements of Cr for Flanders, Belgium. Through the use of IOI it was possible to identify both scattered and clustered outliers resulting in determination of Cr geochemical baseline level that does not deny the local as well as the regional scale variability and display a higher degree of spatial structure as expected for the geochemical baseline data.
机译:地球化学基线浓度被用作确定与土壤污染有关的区域状态的参考。已经开发出各种方法来基于对边缘或空间离群值的过滤来确定该浓度。边缘异常值识别(MOI)使用全局定义的单个阈值将数据分类为属于地球化学基线或表示污染。结果,它忽略了地球化学基线水平的局部尺度变化,这是由于母体材料的可能差异以及影响程度不同的多种污染物的存在而引起的。因此,它可能导致对富集的识别低于全球定义的阈值,但仍大于属于地球化学基线的本地地球化学基线水平。空间离群值识别(SOI)专注于检测本地社区中的异常值。由于SOI严重依赖于数据配置,因此可能会错误地接受高价值的簇作为地球化学基准数据,这些数据可能会增加污染风险地区的地球化学基准水平。当用于大规模研究时,MOI和SOI的局限性可能很严重。为了避免这些局限性并最大限度地利用这两种方法,我们提出了一种组合方法:采用模糊稳健方法进行综合离群值识别(IOI),以确定比利时法兰德斯的Cr的地球化学基线测量值。通过使用IOI,可以识别零散的和聚类的离群值,从而确定Cr地球化学基线水平,而这并不否认局部和区域尺度的变化,并显示出对地球化学基线预期更高的空间结构程度数据。

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