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Hydrogeology of Eastern Niger Delta: A Review

机译:东部尼日尔三角洲的水文地质:评论

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This paper characterizes the aquifer system of the Niger Delta for sustainable development of the groundwater resource. The heavy-dependence on groundwater in the region and the fears of its unsustainability triggered by the weak regulations, pollution, increasing user population and industrialization coupled with the present limited knowledge of the true geological condition prevailing within the groundwater domain of the Niger Delta are the considerations that compelled this review study. The hydraulic properties of the region's aquifers are discussed. The Niger Delta is characterized by a complex multilayered aquifer system hosted in the Benin Formation with the main body of fresh water, with increasing occurrence of intercalating clay units towards the coast. Lithological analysis indicates the prevalence of unconsolidated sand and sandy gravels in the aquiferous horizons, presenting them as pervious and prolific aquifers. Reported hydro-chemical data gathered from wells drilled suggest that the quality of groundwater in the Niger Delta is considered generally very good and compares favorably with WHO standards for drinking water. However, relatively high iron/manganese and chloride values are localized in time and space. In the coastal areas however, seawater intrusion has been identified as one of the major influences on hydrochemistry of groundwater in the shallow unconfined aquifers. Regional groundwater flow direction is from north to south. Changes in groundwater flow directions which occur at some places generally serve localized discharge areas. The resultant flow path eventually joins and feeds the major regional north-south flow direction. The increasing pressure on groundwater, the need for urgent attention and the absence of strong institutions and regulations have made the management of groundwater resources in the region a difficult task. Therefore, future ground water resources development in the Niger Delta requires adequate observational data, investments in infrastructure and an integrated management approach to ensure optimal basin-wide benefits.
机译:本文表征了尼日尔三角洲的可持续发展地下水资源的含水层系统。对该地区地下水的沉重依赖性以及由弱规定,污染,增加用户人口和产业化引发的不可持续性的担忧与当前有限的尼日尔特域内的真实地质条件的现实地质条件有限的知识是迫使这项评论研究的考虑因素。讨论了该地区含水层的液压特性。尼日尔三角洲的特征在于托管在幸存的鲜水主体中的复杂多层含水层系统,随着倒置粘土单元朝向海岸的发生而增加。岩性分析表明,未溶解的沙子和桑迪砾石在含水层视野中的患病率,将它们呈现为透水和多产的含水层。报道从井中收集的水化学数据钻取表明,尼日尔三角洲地下水的质量通常被认为是非常好的,并与饮用水标准有利地进行比较。然而,相对高的铁/锰和氯化物值是在时间和空间的局部化的。然而,在沿海地区,海水入侵已经被确定为浅不合适的含水层对地下水水化学的主要影响之一。区域地下水流向是从北到南方的。在某些地方发生的地下水流动方向的变化通常为局部排出区域。由此产生的流动路径最终加入并喂养主要区域南北流动方向。地下水的压力越来越大,需要紧急关注和缺乏强大的机构和法规,使该地区地下水资源管理成为一项艰巨的任务。因此,尼日尔三角洲未来的地面水资源开发需要足够的观测数据,对基础设施的投资和综合管理方法,以确保最佳的盆地益处。

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