尼日利亚南部翁多州一些必需微量元素的空间分布和生物利用度

W. B. Tomori, I. Amoo, A. Aiyesanmi, E. Yanful, Petrik Leslie
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引用次数: 0

摘要

土壤全元素含量虽然可以提供丰富的元素浓度,但科学界发现不适合预测环境的生物有效性和毒性。研究了尼日利亚南部Ondo州表层(0 ~ 30cm)和地下(60 ~ 90cm)土壤中必需微量元素(Cu、Fe、Mn、Zn)的空间分布、生物有效性和流动性。它们在地表和地下土壤环境中的空间分布非常相似,表明它们的分布可能与相似的地球化学因素有关。北部为基底杂岩,南部主要为未分化的沉积岩。从研究区中心到南部,铜、铁、锰和锌的浓度均较低。微量元素的空间富集可能受下伏基岩类型的影响。铜在表层和地下土壤环境中均具有潜在的生物可利用性,因为其总浓度的50%以上为非残留部分。其他微量元素不具有生物可利用性,因为它们总浓度的60%左右存在于残留馏分中。铜表面相对风险评价规范;地下)表明从低(2-10;1-6)通过介质(12-30;10-21)至高风险(25-40;表层和地下土壤环境中Zn(表层)的变化趋势相似(1-5;乳;22-35)只在表层土壤环境中。其他元素显示出一定程度的风险,甚至没有风险。铜和/或锰可能与人为来源有关。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial Distribution and Bioavailability of Some Essential Trace Elements in Southern Ondo State Nigeria
The total elemental content of soil though may give abundance of element concentration but have been found not to be suitable for prediction of environmental bioavailability and toxicity by scientific community. Surface (0-30cm) and subsurface (60-90cm) soil profile in the Southern Ondo State Nigeria were investigated for spatial distribution, bioavailability and mobility of some essential trace elements (Cu, Fe, Mn, Zn). Their spatial distribution were very similar in both surface and subsurface soil environment indicating that similar geochemical factors may be responsible for their distribution. The North was composed of basement complex while the South was largely undifferentiated sedimentary rock. Higher concentrations of Cu, Fe, Mn and Zn were recorded in the North through the centre of study area to lower concentrations in the South. The spatial concentration of the trace elements may have been influenced by the nature of underlying bedrock type. Cu was potentially bioavailable in both surface and subsurface soil environment considering the fact that >50% of its total concentration were in the nonresidual fraction. Other trace elements were not bioavailable because >60% of their total concentrations were found in residual fractions. The relative risk assessment code of Cu (surface; subsurface) indicated progressive risk (MoF1, MoF2, MoF3) from low (2-10; 1-6) through medium (12-30; 10-21) to high risk (25-40; 21-35) in both surface and subsurface soil environment while Zn (surface) shows similar trend (1-5; 11-21; 22-35) only in the surface soil environment. Other elements show some level of risk to no risk. There is likelihood that Cu and/or Mn may be associated with anthropogenic sources.
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