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Using indicator kriging for evaluating heavy metal contents of a soil over serpentines

机译:使用指示克里格法评估蛇纹石上土壤的重金属含量

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Geostatistical interpolation, kriging, is increasingly used to estimate spatial variability of soil properties and attributes. The kriging-based approach, indicator kriging (IK), may be used to model the uncertainty of mapping heavy metals. Soil samples were obtained at 53 points from the top layer of a soil developed over serpentine. Total and EDTA- extractable contents of Fe, Mn, Cr, Ni, Cu, Zn and Co were determined. The soil data were coded as 0 or 1 when higher or lower than the threshold value established as the median. Using the coded data, indicator semivariograms were computed and modelled by a nugget component plus a structure. Counter maps of probability of meeting the critical threshold value for each of the individual heavy metals were drawn by IK. Advantages of IK for assessing local uncertainty when compared with ordinary kriging were shown.
机译:地统计插值法,克里金法越来越多地用于估算土壤特性和属性的空间变异性。基于克里金法的指标克里金法(IK)可用于对重金属映射的不确定性建模。从在蛇纹石上发育的土壤的顶层的53个点获得土壤样品。确定了铁,锰,铬,镍,铜,锌和钴的总含量和EDTA萃取量。当高于或低于确定为中位数的阈值时,土壤数据被编码为0或1。使用编码后的数据,指标值的半变异函数通过块状部件加结构进行计算和建模。 IK绘制了每种重金属达到临界阈值的概率的对应图。与常规克里金法相比,IK具有评估局部不确定性的优势。

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