奈及利亚纳沙拉瓦州汉基牛-弓湖水中重金属(Cd和Cu)的风险评估、含量、形态和季节变化及沉积物颗粒大小

U. Augustine, R. Sha’Ato, R. Wuana, T. Tor-anyiin
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引用次数: 0

摘要

本研究采用原子吸收分光光度法(AAS)对纳萨拉瓦州阿威L.G.A Hunki牛弓湖水体和沉积物中重金属(Cd和Cu)含量、形态、风险评价指标及季节变化进行了评价。干湿季节水样中Cd的平均浓度均高于Cu,但整体(原始)底泥中Cu的浓度高于Cd。水样中Cd和Cu的基线水平(mg/L)分别为:Cd(0.354)和Cu(0.014),表明水中Cd水平高于世界卫生组织《饮用水水质指南》。沉积物样品中Cd和Cu的基线水平(mg/kg)如下:Cd(7.149)和Cu(8.363),表明Cd和Cu低于临时沉积物质量指南-高(Cd: 10和Cu: 270 mg/kg)。然而,沉积物中的Cd含量高于《临时沉积物质量指南》(低至1.5 mg/kg),但Cu含量较低(65 mg/kg)。Tessier五步顺序提取结果表明,Cd在顺序提取的前4步中含量较高(无残留),两季均占84.64 ~ 94.52%。干季和湿季沉积物有机质组分中以铜为主(48.17% ~ 85.54%)。丰水期生物利用度指数(BI)均值相对高于枯水期。迁移系数(MF)的平均值表明,无论季节如何,Cd都高于Cu。这表明Cd比Cu具有更强的可调动性和生物可利用性。土壤累积指数(I-geo)值表现为基本未污染(旱季1、2、5号点)、中度污染(旱季3、4号点)、重度污染(雨季1、2、4、5号点)至重度污染(雨季3号点)。Cu的I-geo值显示基本未受污染。在旱季,Cd的污染因子(Cf)值普遍处于中等水平。Cd的Cf值在雨季表现为较高的污染因子,Cu的Cf值在两个季节都表现为较低的污染因子。两季Cd生态风险指数(Er)旱季为低至中度生态风险,雨季为高至重度生态风险。Cu的Er值较低。研究表明:旱季沉积物和水样中Cd和Cu的浓度低于雨季;沉积物中Cd和Cu的浓度以人为源为主,自然源较少,多数生态风险指标评价表明Cd具有较大的生态风险。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
RISK ASSESSMENT, LEVELS, SPECIATION AND SEASONAL VARIATION OF HEAVY METALS (Cd and Cu) IN WATER AND PARTICLE SIZES OF SEDIMENTS FROM HUNKI OX-BOW LAKE, AWE LGA, NASARAWA STATE-NIGERIA
This research aimed at assessment of the levels, speciation, risk assessment indices and seasonal variation of heavy metals (Cd and Cu) in water and sediments from Hunki Ox-bow Lake in Awe L.G.A of Nasarawa State, using Atomic Absorption Spectrophotometer (AAS), during the dry and wet seasons. The mean concentration of Cd in water samples of both dry and wet seasons was higher than that of Cu, but Cu was higher than Cd on the whole (raw) sediment samples. The baseline levels of Cd and Cu in water samples (mg/L) were as follows: Cd (0.354) and Cu (0.014), which revealed that Cd level in water was higher than the WHO Guidelines for Drinking Water Quality. The baseline levels of Cd and Cu in sediment samples (mg/kg) were as follows: Cd (7.149) and Cu (8.363) which showed that Cd and Cu were lower than Interim Sediment Quality Guidelines – High of (Cd: 10 and Cu: 270 mg/kg). However, Cd level from sediment was higher than Interim Sediment Quality Guidelines – Low of 1.5 mg/kg but that of Cu was lower (65 mg/kg). Results of the Tessier five-step sequential extraction procedure indicated that Cd was more in the first four steps of the sequential extraction (non-residual) which accounted for 84.64 - 94.52 % in both seasons. Copper dominated more of the organic matter fraction of the sediments (48.17 – 85.54 %) for both dry and wet seasons. The mean of Bioavailability Index (BI) for wet season was relatively higher than that of dry season. The mean values of Mobility Factor (MF) revealed that Cd had higher values than Cu irrespective of seasons. This indicated that Cd was more mobilizable and bioavailable to this aquatic ecosystem compared to Cu. The geo-accumulation Index (I-geo) values of Cd showed practically unpolluted (sites 1, 2 and 5 of dry season), moderately polluted (sites 3 and 4 of dry season), heavily polluted (sites 1, 2, 4 and 5 of wet season) to very heavily polluted (site 3of wet season). The I-geo values of Cu indicated practically unpolluted. In dry season generally, Contamination Factor (Cf) values for Cd were all moderate in dry season. The Cf values of Cd indicated very high contamination factor for wet season, while that of Cu was low in both seasons. In both seasons, the ecological risk index (Er) of Cd in dry season had low to moderate ecological risk, and high to serious ecological risk in wet season. The Er values of Cu were low. This study revealed that: sediments and water samples of the dry season had lower concentration of Cd and Cu than in wet season; concentrations of Cd and Cu from sediments were more of manmade sources rather than natural sources and most ecological risk indices evaluated revealed that Cd had greater ecological risk.  
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