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Characterisation and quality assessment of surface and groundwater in and around Lake Bosumtwi impact craton (Ghana)

机译:博世湖湖(加纳)湖及周边地下水的特征及质量评估

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Conventional graphical methods have been used to classify water in Lake Bosumtwi and groundwater around the lake. The study also assessed the suitability of these water resources for agricultural use. Results indicate slightly acidic, moderately hard to very hard groundwater with alkaline earth concentrations exceeding alkali metals. In contrast, the lake water is alkaline, showing alkalis in excess over alkaline earth metals. Weak acids exceed strong acids in both lake/groundwater. Rock weathering largely controls groundwater and lake water chemical compositions, resulting mainly in Ca-Mg-HCO_3 groundwater and Na-HCO_3 lake water types. Thus, suggesting that there is no apparent incipient relationship, which benefits the primary aquifer system in terms of recharge. Water quality indices suggest groundwater of good to excellent quality for human consumption and other domestic use. An evaluation of lake/groundwater based on salinity, sodicity and bicarbonate hazard reveals that the groundwater is generally suitable for irrigation whiles the lake water is not suitable for irrigation. However, the lake water may be used in generous amounts on highly permeable soils and salt-tolerant crops under special soil and water management practices.
机译:常规的图形方法已被用于将水在博斯穆特威湖和湖泊周围地下水分类。该研究还评估了这些水资源用于农业使用的适用性。结果表明浅酸性,适度难以与碱土金属的碱土浓度相当坚硬。相比之下,湖水是碱性的,显示出碱性土壤中的过量碱。薄弱的酸在湖/地下水中超过强酸。岩石风化在很大程度上控制地下水和湖水化学成分,主要导致Ca-Mg-HCO_3地下水和Na-HCO_3湖水类型。因此,表明没有明显的初始关系,这使得主要含水层系统在充电方面受益。水质指数建议对人类消费等卓越品质的地下水等地。基于盐度,碳酸盐和碳酸氢盐危害的湖/地下水评价显示地下水通常适用于湖水不适合灌溉的灌溉。然而,在特殊的土壤和水管理实践下,湖水可用于高渗透性的土壤和耐盐作物。

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