拉各斯大都市的水文地质

E.O. Longe , S. Malomo, M.A. Olorunniwo
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引用次数: 149

摘要

对拉各斯大都市的地下水资源和地下含水层进行了研究。这是基于测井、泵送测试、油井生产和水质数据。这些数据是在建造和使用拉各斯州小型供水工程方案的最近钻孔期间获得的。地下地质显示出砂、粘土交替层序的复杂岩性。圈定了三个含水层。首先,地下含水层(平均厚度8米)主要通过挖井开采。另外两个承压含水层(厚度分别为10-25米和10-35米)是通过钻孔利用的,是小型供水工程的基础。透射率(T)和存储系数(S)的平均值分别为3.53 × 10−3 m2 S−1和2.95 × 10−4,17.44 × 10−3 m2 S−1和3.29 × 10−4。透光率、蓄水系数和渗透率的变化范围表明含水层具有相当大的不均匀性。化学质量测定表明,利用的含水层水一般是软的。如果去除过量的铁,它们适用于家庭,农业和工业过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hydrogeology of Lagos metropolis

A study of the groundwater resources and aquifers underlying Lagos metropolis has been made. This is based on well-logs, pumping tests, well-production and water quality data. The data were obtained during construction and use of recent boreholes of the Lagos State mini water works programme.

The sub-surface geology indicates a complex lithology of alternating sequence of sand and clay deposits. Three aquifer horizons were delineated. The first, a water table aquifer (average thickness of 8 m) is mostly exploited through dug wells. The other two, confined aquifers (thickness of 10–25 and 10–35 m respectively), are harnessed through boreholes and are the basis of the mini water works.

Average values of transmissivity (T) and storage coefficients (S) are 3.53 × 10−3 m2 s−1 and 2.95 × 10−4 respectively for the second and 17.44 × 10−3 m2 s−1 and 3.29 × 10−4 for the third. The range of transmissitivity, the storage coefficient and also permeability indicate considerable inhomogeneity in the aquifers.

Chemical quality determinations show that the harnessed aquifers waters are generally soft. They are suitable for use in domestic, agricultural and industrial processes, if the excessive iron occurring is removed.

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