Department of Earth Sciences, Faculty of Science, University of Yaoundé 1, PO Box: 812, Yaoundé, Cameroon; Department of Mines, Advanced School of Engineering of Antananarivo, University of Antananarivo, PO Box: 566, Madagascar.
Department of Earth Sciences, Faculty of Science, University of Yaoundé 1, PO Box: 812, Yaoundé, Cameroon.
Sci Total Environ. 2018 Jan 1;610-611:831-844. doi: 10.1016/j.scitotenv.2017.08.080. Epub 2017 Aug 18.
The influence of gold mining activities on the water quality in the Mari catchment in Bétaré-Oya (East Cameroon) was assessed in this study. Sampling was performed within the period of one hydrological year (2015 to 2016), with 22 sampling sites consisting of groundwater (06) and surface water (16). In addition to measuring the physicochemical parameters, such as pH, electrical conductivity, alkalinity, turbidity, suspended solids and CN, eleven major elements (Na, K, Ca, Mg, NH, Cl, NO, HCO, SO, PO and F) and eight heavy metals (Pb, Zn, Cd, Fe, Cu, As, Mn and Cr) were also analyzed using conventional hydrochemical methods, Multivariate Statistical Analysis and the Heavy metal Pollution Index (HPI). The results showed that the water from Mari catchment and Lom River was acidic to basic (5.40<pH<8.84), weakly mineralized (6.3<EC<160.8μS/cm) and had a high concentration of total suspended solids (TSS) (2<TSS<8996.00mg/L). The major elements were all within the World Health Organization (WHO) guidelines for drinking water quality, except for nitrates in some wells, which was found at a concentration >50mg NO/L. This water was found as two main types: calcium magnesium bicarbonate (CaMg-HCO), which was the most represented, and sodium bicarbonate potassium (NaK-HCO). As for trace elements in surface water, the contents of Pb, Cd, Mn, Cr and Fe were higher than recommended by the WHO guidelines, and therefore, the surface water was unsuitable for human consumption. Three phenomena were responsible for controlling the quality of the water in the study area: hydrolysis of silicate minerals of plutono-metamorphic rocks, which constitute the geological basement of this area; vegetation and soil leaching; and mining activities. The high concentrations of TSS and trace elements found in this basin were mainly due to gold mining activities (exploration and exploitation) as well as digging of rivers beds, excavation and gold amalgamation.
本研究评估了贝塔雷-奥亚(喀麦隆东部)马里流域的金矿开采活动对水质的影响。采样是在一个水文年(2015 年至 2016 年)内进行的,共有 22 个采样点,包括地下水(06 个)和地表水(16 个)。除了测量物理化学参数,如 pH 值、电导率、碱度、浊度、悬浮物和 CN 外,还使用常规水化学方法、多元统计分析和重金属污染指数(HPI)分析了 11 种主要元素(Na、K、Ca、Mg、NH、Cl、NO、HCO、SO、PO 和 F)和 8 种重金属(Pb、Zn、Cd、Fe、Cu、As、Mn 和 Cr)。结果表明,马里流域和洛姆河的水呈酸性至碱性(5.40<pH<8.84),弱矿化(6.3<EC<160.8μS/cm),总悬浮物(TSS)浓度较高(2<TSS<8996.00mg/L)。除了一些井中的硝酸盐浓度超过 50mg NO/L 外,主要元素均在世界卫生组织(WHO)饮用水质量指南范围内。这种水被发现有两种主要类型:钙镁重碳酸盐(CaMg-HCO),是最主要的类型,以及碳酸钠钾(NaK-HCO)。至于地表水的微量元素,Pb、Cd、Mn、Cr 和 Fe 的含量高于 WHO 指南推荐值,因此地表水不适宜人类饮用。有三种现象控制着研究区的水质:造山变质岩中的硅酸盐矿物水解,构成了该地区的地质基底;植被和土壤淋溶;以及采矿活动。该盆地中发现的高浓度 TSS 和微量元素主要是由于金矿开采活动(勘探和开采)以及河床挖掘、挖掘和金汞齐化。