Characterization of the productivity of basement aquifers at Bagoué region (North of Côte d’Ivoire)

O. Z. De Lasme, A. S. Koffi, Oscar Z Onetie, Lancine Diallo, Xavier T Ahondjo
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Abstract

This study aims to characterize the productivity of basement aquifers based on a database built by pumping test and drilling report from eighteen boreholes exploited in Bagoue region of Cote d’Ivoire. By using last version of a tool to assist in pumping test interpretation suggested by the French Mining and Geological Survey, Transmissivity parameter values of confined aquifers were determined through the well-known Theis method. In the same approach, critical yield value of borehole was determined at the equivalence point of linear and quadratic pressure drop from short-term pumping test data. Geostatistical analysis and kriging of transmissivity of aquifers were realized. Then, it was elaborated few predictive equations between hydrodynamic and hydraulic parameters based on their relationship level. Comparison of aquifers productivity and boreholes hydraulic capacity ended the methodology. Transmissivity ranged from 9.10-7 to 4.10-5 m2.h-1 while specific yield of boreholes reached between 0.34 and 23.07 m3.h-1. Yields from exploited boreholes varied between 0.5 m3.h-1 and 12 m3.h-1 with an average reaching 3.44 m3.h-1. Critical yield varied between 2.11 and 18.8 m3.h-1 with an average of 6.95 m3.h-1. According to geostatistical analysis of Transmissivity, its spatial spreading adjusted spherical model with a range reaching 0.13 meters. Findings highlighted 44 % of aquifer areas characterized by low value of transmissivity with great value of exploited outflow. That suggests a short-term availability of drinking water for living communities. In the same way, 11.11 % of boreholes were established into aquifer areas characterized by great transmissivity and low outflow values that suggests a better supply environment with long-term groundwater availability.
bagou地区(Côte科特迪瓦北部)地下含水层生产力特征
本研究旨在根据科特迪瓦Bagoue地区开采的18个钻孔的抽水试验和钻井报告建立的数据库来描述地下室含水层的生产力。利用法国采矿和地质调查局建议的辅助抽水试验解释工具的最新版本,通过著名的Theis方法确定了承压含水层的透射率参数值。采用同样的方法,根据短期泵送试验数据,在线性压降和二次压降等点处确定井眼临界屈服值。实现了含水层透过率的地质统计分析和克里格法。在此基础上,根据水动力参数与水力参数之间的关系水平,建立了几个预测方程。含水层产能与钻孔水力能力的比较结束了该方法。穿透率为9.10-7 ~ 4.10-5 m2.h-1,井眼比产率为0.34 ~ 23.07 m3.h-1。开采井的产量在0.5 m3 - h-1 ~ 12 m3 - h-1之间,平均可达3.44 m3 - h-1。临界产量变化在2.11 ~ 18.8 m3.h-1之间,平均为6.95 m3.h-1。通过对透射率的地统计学分析,得到了其空间扩展调整球面模型,其范围达到0.13米。研究结果突出表明,44%的含水层具有低透射率值和高开采流出值的特征。这表明生活社区可以短期获得饮用水。同样,11.11%的钻孔建在透水性大、流出量低的含水层区域,这表明地下水长期可用性较好,供应环境较好。
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