Water Quality Assessment and Resource Potentials: the Case of Aba–Urban and its Environs, Niger Delta Basin


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The quest for improved water supply to cater for the ever increasing population has given rise to the assessment of water quality and resource potentials in Aba-Urban and its environments. The area, which lies within the Niger Delta Basin is underlain by the Benin Formation that is highly aquiferous. Samples of sands and water were subjected to sedimentological and hydrochemical analysis, respectively. Result reveals that the aquifer is thick (over 100 m) and unconfined. The computed aquifer parameters indicate high yielding clean-sands with hydraulic conductivity values ranging from 1.13 × 10–4 to 5.70 × 10–3 m/s. The specific discharge is about 14.2 m/year while the average linear groundwater velocity is calculated to be 53.46 m/year. Hydrochemical investigations carried out on water samples from Aba River and the groundwater system revealed low dissolved geochemical constituents. Although, there is a slight increase from the north to the southern part along the flow path. In general, the groundwater is relatively enriched in Ca, Mg−HCO-3ions and is predominantly of bicarbonate constituents. However, in some places Cl ions dominate over HCO-3ions. This is common where the water has come in contact with domestic sewage. This kind of contamination is also accompanied by elevated concentration of NO-3ions. Generally, the groundwater in most cases meets the standard for human consumption and is a better alternative to surface water. Consequently an increase exploitation of the prolific Benin aquifer through more hygienic and safe methods will surely be the best way of improving the domestic water supply situation in Aba City.

作者简介

Ugochukwu Agharanya

Department of Geology, Faculty of Physical Sciences

Email: princeton.dim@gmail.com
尼日利亚, Nsukka, Enugu State, 410001

Chidozie DIM

Department of Geology, Faculty of Physical Sciences

编辑信件的主要联系方式.
Email: princeton.dim@gmail.com
尼日利亚, Nsukka, Enugu State, 410001

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