尼日利亚灌溉地地下水补给研究:对流域可持续性的影响

A. Sobowale , A.A. Ramalan , O.J. Mudiare , M.A. Oyebode
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引用次数: 13

摘要

以尼日利亚卡诺河灌溉项目(KRIP)为例,评价了尼日利亚半干旱地区含水层管理补给(MAR)的潜力。采用水位波动(wlf)法对3年(2009-2011)地下水补给进行了逐日评价。利用Microsoft Excel®电子表格和ArcGIS®9.0软件对回灌量进行时空分析。结果表明,农田土壤日补给量在17 ~ 32 mm之间。进一步的分析表明,降雨和灌溉每天平均增加8毫米的水。观测到的内涝问题对该地区的盐积累有影响,可以通过农田地表水和地下水的联合利用来改善。这将节约大量的水,这些水可以从Tiga大坝释放出来,通过渗透盆地系统地实施MAR,为Hadejia河下游的乍得地层含水层补充水分。然而,要实现这一目标,还需要进行额外的建模研究和含水层特征描述。
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Groundwater recharge studies in irrigated lands in Nigeria: Implications for basin sustainability

The potential of managed aquifer recharge (MAR) in semi-arid areas of Nigeria was evaluated using the Kano River irrigation Project (KRIP) as a case study. Groundwater recharge was evaluated daily for 3 years (2009–2011) using the water level fluctuation (wlf) method. Temporal and spatial analyses of recharge were carried out using Microsoft Excel® spread sheet and ArcGIS® 9.0 software. Results show that recharge range from 17 to 32 mm daily on the farmland. Further analysis showed that an average of 8 mm of water is added to storage daily from both rainfall and irrigation. The observed waterlogging problems has implication for salt build up in the area and could be ameliorated by conjunctive use of both surface water and groundwater from the farmland. This will lead to huge water savings that could be released from the Tiga dam to recharge the Chad formation aquifers downstream of the Hadejia River in a systematic MAR implementation via infiltration basin. However, additional modelling studies and aquifer characterization are required to implement this.

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