School of Science and Engineering, University of Ballarat, Mt Helen Campus, University Drive, Mt Helen, Victoria 3350, Australia.
Sci Total Environ. 2010 May 15;408(12):2590-9. doi: 10.1016/j.scitotenv.2009.12.039. Epub 2010 Jan 13.
Arsenic is naturally associated with gold mineralisation and elevated in some soils and mine waste around historical gold mining activity in Victoria, Australia. To explore uptake, arsenic concentrations in children's toenail clippings and household soils were measured, and the microdistribution and speciation of arsenic in situ in toenail clipping thin sections investigated using synchrotron-based X-ray microprobe techniques. The ability to differentiate exogenous arsenic was explored by investigating surface contamination on cleaned clippings using depth profiling, and direct diffusion of arsenic into incubated clippings. Total arsenic concentrations ranged from 0.15 to 2.1 microg/g (n=29) in clipping samples and from 3.3 to 130 microg/g (n=22) in household soils, with significant correlation between transformed arsenic concentrations (Pearson's r=0.42, P=0.023) when household soil was treated as independent. In clipping thin sections (n=2), X-ray fluorescence (XRF) mapping showed discrete layering of arsenic consistent with nail structure, and irregular arsenic incorporation along the nail growth axis. Arsenic concentrations were heterogeneous at 10x10 microm microprobe spot locations investigated (<0.1 to 13.3 microg/g). X-ray absorption near-edge structure (XANES) spectra suggested the presence of two distinct arsenic species: a lower oxidation state species, possibly with mixed sulphur and methyl coordination (denoted As(approximately III)(-S, -CH3)); and a higher oxidation state species (denoted As(approximately V)(-O)). Depth profiling suggested that surface contamination was unlikely (n=4), and XRF and XANES analyses of thin sections of clippings incubated in dry or wet mine waste, or untreated, suggested direct diffusion of arsenic occurred under moist conditions. These findings suggest that arsenic in soil contributes to some systemic absorption associated with periodic exposures among children resident in areas of historic gold mining activity in Victoria, Australia. Future studies are required to ascertain if adverse health effects are associated with current levels of arsenic uptake.
砷通常与金矿化作用有关,在澳大利亚维多利亚州历史上的金矿开采活动周围的一些土壤和矿山废石中含量较高。为了研究砷的吸收情况,测量了儿童趾甲屑和家庭土壤中的砷浓度,并使用基于同步加速器的 X 射线微探针技术原位研究了趾甲屑薄片中砷的微观分布和形态。通过对清洁后的趾甲屑进行深度剖析和砷的直接扩散来研究表面污染,探讨了区分外源性砷的能力。在剪取样本中,总砷浓度范围为 0.15 至 2.1 微克/克(n=29),在家庭土壤中为 3.3 至 130 微克/克(n=22),当家庭土壤被视为独立时,转化砷浓度之间存在显著相关性(Pearson r=0.42,P=0.023)。在趾甲薄片中(n=2),X 射线荧光(XRF)图谱显示出与指甲结构一致的砷离散分层,以及沿着指甲生长轴不规则的砷掺入。在 10x10 微米微探针点位置的砷浓度存在不均匀性(<0.1 至 13.3 微克/克)。X 射线吸收近边结构(XANES)谱表明存在两种不同的砷物种:一种较低氧化态的物种,可能具有混合硫和甲基配位(表示为 As(approx III)(-S,-CH3));一种较高氧化态的物种(表示为 As(approx V)(-O))。深度剖析表明表面污染不太可能(n=4),对在干燥或湿润的矿山废石中培养或未处理的趾甲屑薄片的 XRF 和 XANES 分析表明,在潮湿条件下砷直接扩散。这些发现表明,土壤中的砷与澳大利亚维多利亚州历史上金矿开采活动地区儿童定期暴露相关的一些系统性吸收有关。需要进一步研究以确定当前砷吸收水平是否与不良健康影响相关。