...
首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Soil-geochemical factors controlling the distribution and oral bioaccessibility of nickel, vanadium and chromium in soil
【24h】

Soil-geochemical factors controlling the distribution and oral bioaccessibility of nickel, vanadium and chromium in soil

机译:控制镍,钒和铬在土壤中的分布和口腔生物可及性的土壤地球化学因素

获取原文
获取原文并翻译 | 示例

摘要

Geogenic nickel (Ni), vanadium (V) and chromium (Cr) are present at elevated levels in soils in Northern Ireland. Whilst Ni, V and Cr total soil concentrations share common geological origins, their respective levels of oral bioaccessibility are influenced by different soil-geochemical factors. Oral bioaccessibility extractions were carried out on 145 soil samples overlying 9 different bedrock types to measure the bioaccessible portions of Ni, V and Cr. Principal component analysis identified two components (PC1 and PC2) accounting for 69% of variance across 13 variables from the Northern Ireland Tellus Survey geochemical data. PC1 was associated with underlying basalt bedrock, higher bioaccessible Cr concentrations and lower Ni bioaccessibility. PC2 was associated with regional variance in soil chemistry and hosted factors accounting for higher Ni and V bioaccessibility. Eight percent of total V was solubilised by gastric extraction on average across the study area. High median proportions of bioaccessible Ni were observed in soils overlying sedimentary rock types. Whilst Cr bioaccessible fractions were low (max = 5.4%), the highest measured bioaccessible Cr concentration reached 10.0 mg kg~(-1), explained by factors linked to PC1 including high total Cr concentrations in soils overlying basalt bedrock.
机译:在北爱尔兰的土壤中,成矿的镍(Ni),钒(V)和铬(Cr)含量较高。尽管Ni,V和Cr的总土壤浓度具有共同的地质起源,但它们各自的口腔生物可及性水平受不同的土壤地球化学因素影响。对覆盖9种不同基岩类型的145个土壤样品进行了口服生物可及性提取,以测量Ni,V和Cr的可生物可及部分。主成分分析确定了两个成分(PC1和PC2),占北爱尔兰Tellus调查地球化学数据中13个变量的69%的方差。 PC1与潜在的玄武岩基岩,较高的可生物利用的Cr浓度和较低的Ni的可利用性有关。 PC2与土壤化学成分的区域差异有关,并且是导致较高Ni和V生物可及性的主要因素。在整个研究区域中,平均有8%的总V通过胃抽提溶解。在覆盖沉积岩类型的土壤中观察到了高中位数可生物利用的镍。虽然Cr的可生物利用分数较低(最大值= 5.4%),但测得的最高可生物利用Cr浓度却达到了10.0 mg kg〜(-1),这与PC1有关,包括玄武岩基岩上层土壤中的总Cr浓度很高。

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