首页> 外文期刊>Geoderma: An International Journal of Soil Science >Spatial distribution and sources of trace elements in surface soils, Changchun, China: Insights from stochastic models and geostatistical analyses
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Spatial distribution and sources of trace elements in surface soils, Changchun, China: Insights from stochastic models and geostatistical analyses

机译:表土中微量元素的空间分布和来源,中国长春:随机模型和地统计分析的启示

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Trace elements As, Cd, Cu, Hg, and Pb in soils originate from both natural and anthropogenic sources, and intense anthropogenic activity can lead to excessive trace element levels, which are harmful to the environment. We investigated the trace elements in the topsoil of Changchun, China, using stochastic models and the indicator kriging method. The influence of anthropogenic and natural variables on the distribution of trace elements was evaluated, with the proportions of background and anthropogenic sources identified using stochastic models. High-risk maps were constructed using indicator kriging. The results showed that the anthropogenic variables significantly influenced the spatial variations of trace elements. The relative influence of natural variables differed for the different elements. The median values of background As, Cd, Cu, Hg, and Pb were 10.55 mg kg(-1), 0.114 mg kg(-1), 21.80 mg kg(-1), 0.036 mg kg(-1), and 25.88 mg kg(-1), respectively; while the threshold values were 12.90 mg kg(-1), 0200 mg kg(-1), 29.40 mg kg(-1), 0.046 mg kg(-1), and 29.49 mg kg(-1), respectively. The relative contributions of background values to total values of As, Cd, and Cu were greater than 95%, while those for Pb were 91%. In contrast, Hg showed serious pollution, with less than 75% of the total Hg derived from background sources. The geographically extensive Hg pollution is likely influenced by emissions from coal-fired plants and boilers, while other trace elemental pollutants primarily originate from factory emissions. Furthermore, the atmospheric diffusion of Pb and Hg is significant, resulting in their migration to agricultural areas. (C) 2016 Elsevier B.V. All rights reserved.
机译:土壤中的痕量元素As,Cd,Cu,Hg和Pb均来自自然和人为来源,强烈的人为活动会导致痕量元素含量过高,对环境有害。我们使用随机模型和指标克里金法研究了中国长春表层土壤中的微量元素。评估了人为和自然变量对微量元素分布的影响,并使用随机模型确定了背景和人为来源的比例。使用指标克里金法绘制高风险地图。结果表明,人为变量显着影响微量元素的空间变化。自然变量的相对影响因要素而异。背景砷,镉,铜,汞和铅的中位数分别为10.55 mg kg(-1),0.114 mg kg(-1),21.80 mg kg(-1),0.036 mg kg(-1)和25.88分别为mg kg(-1);而阈值分别为12.90 mg kg(-1),0200 mg kg(-1),29.40 mg kg(-1),0.046 mg kg(-1)和29.49 mg kg(-1)。背景值对As,Cd和Cu总值的相对贡献大于95%,而Pb的相对贡献为91%。相比之下,汞显示出严重的污染,不到总汞的75%来自背景。地理上广泛的汞污染很可能受到燃煤电厂和锅炉排放的影响,而其他微量元素污染物主要来自工厂排放。此外,铅和汞在大气中的扩散非常显着,导致它们迁移到农业地区。 (C)2016 Elsevier B.V.保留所有权利。

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