喀麦隆东部矿化洛美盆地潜在有毒微量金属的区域地球化学基线浓度:污染评估工具

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemical Transactions Pub Date : 2018-05-02 DOI:10.1186/s12932-018-0056-5
Mumbfu Ernestine Mimba, Takeshi Ohba, Salomon César Nguemhe Fils, Melvin Tamnta Nforba, Nozomi Numanami, Tasin Godlove Bafon, Festus Tongwa Aka, Cheo Emmanuel Suh
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引用次数: 34

摘要

评价了洛美盆地矿化活动水系沉积物中微量金属的分布。收集了55个底部沉积物,用XRD测定了6个粉碎样品的矿物学成分。采用全消解法(HClO4 + HF + HCl)消解细粒(<?150 μm),结合ICP-MS和原子吸收光谱(AAS)分析痕量金属。结果表明:水系沉积物矿物学以石英(39 ~ 86%)、层状硅酸盐(0 ~ 45%)和长石(0 ~ 27%)为主;所分析金属的平均浓度很低(如As = 99.40?573.24μg / kg、锌= ? ?963.14μg / kg, V = ? ?Cr = 763.93 μg/kg)。铁和锰的平均浓度分别为28.325和442?毫克/公斤。统计计算了微量金属的背景值和阈值,以确定地质或人为来源的地球化学异常,特别是采矿活动。对标准化数据进行因子分析,确定了三种关联:Ni-Cr-V-Co-As-Se-pH, Cu-Zn-Hg-Pb-Cd-Sc和Fe-Mn。第一类组合受矿源地质和中性pH控制,第二类组合受硫化物成矿作用控制,最后一类组合受氧化铁矿物化学风化作用控制。空间分析显示,Co-Cr-V-Ni和Cu-Zn-Pb-Sc的分布趋势相似,反映了盆地的岩性和硫化物成矿作用。相对较高的砷含量与已报道的金矿相一致,而铁和锰的分布与含铁变质岩的来源相一致。这些发现为喀麦隆东部地区的共同和平行地质域提供了基线地球化学值。虽然本研究表明水系沉积物没有受到污染,但强烈建议对废弃和活跃矿区的环境样品进行金属成分评价,以进行比较和环境健康风险评估。
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Regional geochemical baseline concentration of potentially toxic trace metals in the mineralized Lom Basin, East Cameroon: a tool for contamination assessment

The distribution of trace metals in active stream sediments from the mineralized Lom Basin has been evaluated. Fifty-five bottom sediments were collected and the mineralogical composition of six pulverized samples determined by XRD. The fine fraction (<?150?μm) was subjected to total digestion (HClO4?+?HF?+?HCl) and analyzed for trace metals using a combination of ICP-MS and AAS analytical methods. Results show that the mineralogy of stream sediments is dominated by quartz (39–86%), phyllosilicates (0–45%) and feldspars (0–27%). Mean concentrations of the analyzed metals are low (e.g. As?=?99.40?μg/kg, Zn?=?573.24?μg/kg, V?=?963.14?μg/kg and Cr?=?763.93?μg/kg). Iron and Mn have significant average concentrations of 28.325 and 442?mg/kg, respectively. Background and threshold values of the trace metals were computed statistically to determine geochemical anomalies of geologic or anthropogenic origin, particularly mining activity. Factor analysis, applied on normalized data, identified three associations: Ni–Cr–V–Co–As–Se–pH, Cu–Zn–Hg–Pb–Cd–Sc and Fe–Mn. The first association is controlled by source geology and the neutral pH, the second by sulphide mineralization and the last by chemical weathering of ferromagnesian minerals. Spatial analysis reveals similar distribution trends for Co–Cr–V–Ni and Cu–Zn–Pb–Sc reflecting the lithology and sulphide mineralization in the basin. Relatively high levels of As were concordant with reported gold occurrences in the area while Fe and Mn distribution are consistent with their source from the Fe-bearing metamorphic rocks. These findings provide baseline geochemical values for common and parallel geological domains in the eastern region of Cameroon. Although this study shows that the stream sediments are not polluted, the evaluation of metal composition in environmental samples from abandoned and active mine sites for comparison and environmental health risk assessment is highly recommended.

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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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