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Correlation analysis as a tool to investigate the bioaccessibility of nickel, vanadium and zinc in Northern Ireland soils

机译:相关分析作为研究北爱尔兰土壤中镍,钒和锌生物可及性的工具

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Correlation analyses were conducted on nickel (Ni), vanadium (V) and zinc (Zn) oral bioaccessible fractions (BAFs) and selected geochemistry parameters to identify specific controls exerted over trace element bioaccessibility. BAFs were determined by previous research using the unified BARGE method. Total trace element concentrations and soil geochemical parameters were analysed as part of the Geological Survey of Northern Ireland Tellus Project. Correlation analysis included Ni, V and Zn BAFs against their total concentrations, pH, estimated soil organic carbon (SOC) and a further eight element oxides. BAF data were divided into three separate generic bedrock classifications of basalt, lithic arenite and mudstone prior to analysis, resulting in an increase in average correlation coefficients between BAFs and geochemical parameters. Sulphur trioxide and SOC, spatially correlated with upland peat soils, exhibited significant positive correlations with all BAFs in gastric and gastro-intestinal digestion phases, with such effects being strongest in the lithic arenite bedrock group. Significant negative relationships with bioaccessible Ni, V and Zn and their associated total concentrations were observed for the basalt group. Major element oxides were associated with reduced oral trace element bioaccessibility, with Al2O3 resulting in the highest number of significant negative correlations followed by Fe2O3. spatial mapping showed that metal oxides were present at reduced levels in peat soils. The findings illustrate how specific geology and soil geochemistry exert controls over trace element bioaccessibility, with soil chemical factors having a stronger influence on BAF results than relative geogenic abundance. In general, higher Ni, V and Zn bioaccessibility is expected in peat soil types.
机译:对镍(Ni),钒(V)和锌(Zn)口服生物可及级分(BAF)和选定的地球化学参数进行了相关分析,以鉴定对微量元素生物可及性施加的特定控制。 BAF由先前的研究使用统一BARGE方法确定。作为北爱尔兰Tellus项目地质调查的一部分,分析了总微量元素浓度和土壤地球化学参数。相关分析包括Ni,V和Zn BAF与其总浓度,pH,估计的土壤有机碳(SOC)以及另外八种元素氧化物的关系。在分析之前,BAF数据被分为玄武岩,岩质砂岩和泥岩的三个单独的通用基岩分类,从而导致BAF与地球化学参数之间的平均相关系数增加。三氧化硫和SOC与高地泥炭土壤在空间上相关,在胃和胃肠道消化阶段与所有BAF呈显着正相关,在石质砂岩基岩组中这种作用最强。玄武岩组与生物可利用的镍,钒和锌及其相关的总浓度之间存在显着的负相关关系。主要元素氧化物与口服微量元素生物可及性降低有关,其中Al2O3导致最大数量的显着负相关,其次是Fe2O3。空间测绘表明,泥炭土中金属氧化物的含量降低。这些发现说明了特定的地质和土壤地球化学如何控制微量元素的生物可及性,而土壤化学因子对BAF结果的影响要比相对地源丰富度更大。通常,在泥炭土壤类型中,镍,钒和锌的生物可及性更高。

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