HYDROLOGICAL ASSESSMENT FOR SUSTAINABLE GROUNDWATER ABSTRACTION USING VES, MRS, SR AND MODFLOW: A CASE OF NAMANVE INDUSTRIAL AND BUSINESS PARK, MUKONO DISTRICT, UGANDA

J. Nyende
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Abstract

The increase in demand for water supply in Uganda as a result of high population growth, agricultural and industrial expansion has triggered unplanned groundwater development and use in many parts of the country. This has put the future yield and sustainability of groundwater abstraction in some of these parts into question. This paper investigated a hydrogeological assessment for sustainable groundwater abstraction in Kampala Industrial and Business Park, Namanve. The main aim was to establish the behavioral response of the groundwater system to increased abstraction. This investigation was done using pre-existing groundwater/ borehole data from the area to generate the various aquifer parameters in the area: aquifer geometry, hydraulic properties and finally the hydrogeological conceptual model of the area. These values were further adjusted during the modeling processes to suit the current hydraulic heads in the area. The final modeling results demonstrated that an average recharge of 42 mm year-m/day maintains the natural equilibrium of non-pumping and the model result with pumping scenario shows that the current estimated groundwater abstraction of 2871 m3day-1 in the area did not cause any significant effect on the groundwater levels in the area. Significant effect on the water levels was however, realized after increasing the current abstraction rate by 500%. The sensitivity of the model was tested by systematically changing one parameter or input values at a time and it was found that the model is highly sensitive to changes of transmissivity of the aquifer system and the recharge rate. 
利用ves、mrs、sr和modflow对可持续地下水抽取进行水文评价:以乌干达穆科诺地区纳曼纳工业和商业园区为例
由于人口高速增长、农业和工业扩张,乌干达对水供应的需求增加,导致该国许多地区对地下水进行了计划外的开发和使用。这使得这些地区地下水开采的未来产量和可持续性受到质疑。本文对纳曼省坎帕拉工业和商业园区地下水可持续抽取的水文地质评价进行了研究。主要目的是建立地下水系统对增加抽水量的行为反应。这项调查使用了该地区已有的地下水/钻孔数据来生成该地区的各种含水层参数:含水层几何形状、水力特性,最后是该地区的水文地质概念模型。这些值在建模过程中进一步调整,以适应该地区当前的水力水头。最终模拟结果表明,42 mm年-m/d的平均补给维持了非抽水的自然平衡,抽水情景下的模型结果表明,该地区目前估计的地下水抽取量为2871 m3day-1,对该地区的地下水位没有任何显著影响。然而,在将目前的抽水量提高500%后,对水位产生了显著影响。通过一次系统地改变一个参数或输入值来检验模型的灵敏度,发现该模型对含水层系统透过率和补给速率的变化高度敏感。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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