Sequential Extraction and Geochemistry of Heavy Metals in Ayetoro Coastal Sediments, Southwestern Nigeria

Ayodele Olusiji Samuel
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Abstract

Previous geochemical investigation of Ayetoro area discovered that its coastal sediments are enriched with sulphide mineralization. However, in order to determine the geochemical phases of the heavy metals in the coastal sediments, random sampling method was utilized across 10 locations, at a depth of 40cm using Van grab sampler at a sampling density of 200m interval. Atomic Absorption Spectrophotometer (AAS) Buck Scientific Model 205A was used to analyze nine (9) heavy metal concentrations namely Ni, Zn, Co, Mn, Fe, Pb, Cr, Cd and Cu in the coastal sediments, followed by sequential extraction of the metals, using five fractional phases. The results revealed that the geochemical concentration of the heavy metals as follows: Ni (5.89ppm - 16.82ppm), Zn (2.59ppm - 115.65ppm.), Co (1.22ppm - 22.77ppm), Mn (30.95ppm - 186.49ppm), Fe (6.632ppm - 1925.96ppm), Pb (5.17ppm - 55.96ppm), Cr (0.26ppm - 28.06ppm), Cd (0.13ppm -22.23ppm), and Cu (2.26ppm - 41.94ppm) and showed the concentration order as Residual>Reducible>Organic>Exchangeable>Carbonate. Most of the heavy metals in carbonate and exchangeable phase have low concentration except for Cd. This implied that Cd is of low mobility and bioavailability which is very dangerous as its intake by man leads to kidney diseases and causes bones to become weaker. Also, Mobility factor of Cd stood out because of its high concentration in the exchangeable phase compared to other four non-residual phases. The mobility and bioavailability of the heavy metals are in this order: Cd>Co>Ni>Pb>Cr>Mn>Cu>Zn>Fe respectively. The analysis of variance (ANOVA) revealed that the heavy metals are significantly different in all the phases based on their accumulation index in the sediments while majority of the heavy metals lacked the ability to remobilize but can be released into the environment under reducing and oxidizing conditions.
尼日利亚西南部Ayetoro海岸沉积物中重金属的序贯提取及地球化学特征
以往对Ayetoro地区的地球化学调查发现,其海岸沉积物富含硫化物成矿作用。然而,为了确定沿海沉积物中重金属的地球化学相态,我们在10个地点使用Van grab采样器随机采样,采样深度为40cm,采样密度为200m间隔。采用Buck Scientific Model 205A原子吸收分光光度计(AAS)对沿海沉积物中Ni、Zn、Co、Mn、Fe、Pb、Cr、Cd和Cu 9种重金属浓度进行了分析,并采用5个分数相对重金属进行了顺序萃取。结果表明,重金属地球化学浓度为:Ni (5.89ppm ~ 16.82ppm)、Zn (2.59ppm ~ 115.65ppm)、Co (1.22ppm ~ 22.77ppm)、Mn (30.95ppm ~ 186.49ppm)、Fe (6.632ppm ~ 1925.96ppm)、Pb (5.17ppm ~ 55.96ppm)、Cr (0.26ppm ~ 28.06ppm)、Cd (0.13ppm ~ 22.23ppm)、Cu (2.26ppm ~ 41.94ppm),浓度顺序为残余>可还原>有机>可交换>碳酸盐。除Cd外,大多数碳酸盐和交换相的重金属浓度都很低,这意味着Cd的流动性和生物利用度都很低,人体摄入Cd会导致肾脏疾病和骨骼变弱,这是非常危险的。此外,由于Cd在交换相中的浓度高于其他四种非残留相,因此其迁移系数突出。重金属的迁移率和生物利用度依次为Cd>Co>Ni>Pb>Cr>Mn>Cu>Zn>Fe。方差分析(ANOVA)表明,沉积物中重金属在各阶段的积累指数存在显著差异,大部分重金属缺乏再活化能力,在还原和氧化条件下可以释放到环境中。
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