Graduate School of Science and Technology, Isotope Hydrology Laboratory, Kumamoto University, Japan.
Environ Geochem Health. 2011 Dec;33(6):559-75. doi: 10.1007/s10653-010-9371-1. Epub 2011 Mar 4.
Groundwater quality of the Banana Plain (Mbanga, Njombe, Penja-Cameroon) was assessed for its suitability for drinking, domestic, and agricultural uses. A total of 67 groundwater samples were collected from open wells, springs, and boreholes. Samples were analyzed for physicochemical properties, major ions, and dissolved silica. In 95% of groundwater samples, calcium is the dominant cation, while sodium dominates in 5% of the samples. Eighty percent of the samples have HCO(3) as major anion, and in 20%, NO(3) is the major anion. Main water types in the study area are CaHCO(3), CaMgHCO(3), CaNaHCO(3), and CaNaNO(3)ClHCO(3). CO(2)-driven weathering of silicate minerals followed by cation exchange seemingly controls largely the concentrations of major ions in the groundwaters of this area. Nitrate, sulfate, and chloride concentrations strongly express the impact of anthropogenic activities (agriculture and domestic activities) on groundwater quality. Sixty-four percent of the waters have nitrate concentrations higher than the drinking water limit. Also limiting groundwater use for potable and domestic purposes are contents of Ca(2+), Mg(2+) and HCO(3) (-) and total hardness (TH) that exceed World Health Organization (WHO) standards. Irrigational suitability of groundwaters in the study area was also evaluated, and results show that all the samples are fit for irrigation. Groundwater quality in the Banana Plain is impeded by natural geology and anthropogenic activities, and proper groundwater management strategies are necessary to protect sustainably this valuable resource.
对香蕉平原(姆班加、恩琼贝、彭贾-喀麦隆)的地下水质量进行了评估,以确定其是否适合饮用、家庭和农业用途。从露天井、泉水和钻孔中采集了 67 个地下水样本。对样本进行了物理化学性质、主要离子和溶解硅的分析。在 95%的地下水样本中,钙是主要的阳离子,而在 5%的样本中,钠占主导地位。80%的样本中主要阴离子是 HCO(3),而在 20%的样本中,NO(3)是主要阴离子。研究区主要的水类型是 CaHCO(3)、CaMgHCO(3)、CaNaHCO(3)和 CaNaNO(3)ClHCO(3)。碳酸酐酶驱动的硅酸盐矿物风化,随后是阳离子交换,似乎控制了该地区地下水中主要离子的浓度。硝酸盐、硫酸盐和氯化物浓度强烈表明人为活动(农业和家庭活动)对地下水质量的影响。64%的水的硝酸盐浓度高于饮用水限值。此外,限制地下水用于饮用水和家庭用途的还有 Ca(2+)、Mg(2+)和 HCO(3) (-)和总硬度(TH)的含量,这些都超过了世界卫生组织(WHO)的标准。还评估了研究区地下水的灌溉适宜性,结果表明所有样本都适合灌溉。香蕉平原的地下水质量受到自然地质和人为活动的影响,需要采取适当的地下水管理策略来保护这一宝贵资源的可持续性。