Integrated Geophysical and Packer Test for the Water Tightness Evaluation of Gullele Botanic Garden Dam Site, Northwest of Addis Ababa, Ethiopia

B. Moges, M. Meten, H. Solomon
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Abstract

Gullele Botanic Garden is one of the largest botanical gardens in Ethiopia, which is found northwest of Addis Ababa. For this garden, a dam was proposed to be constructed for irrigation and recreational purposes. The intended dam will have a height of 30 m and a dam axis length of around 180 m. The main objective of this work is to investigate and evaluate the engineering geological aspects of the proposed dam site based on detailed geological, geotechnical and geophysical investigations. The investigation conducted in the area includes, electrical resistivity imaging, VES, borehole drilling and single packer permeability test. Geologically the area is covered by the different volcanic rock such as ignimbrite, rhyolite, tuff, basalt, and residual soil; and geological structures such as joint, fracture, flow banding, and cooling joint. The dominant orientations of geological structures are N-S and E-W directions. Results from different investigations revealed that three geotechnical layers were identified. These are overburden (completely weathered ignimbrite and soil), highly to moderately weathered ignimbrite and moderately to slightly weathered ignimbrite rock mass. The rock mass permeability test from six boreholes has Lugeon values ranging from 0 to 9. The maximum Lugeon (permeability of the rock mass) values investigated at the left abutment and riverbed of the proposed dam site showed wash out and dilation behavior respectively. The permeability result indicates that possible seepage problem at left abutment, riverbed and reserviour of the proposed dam. Therefore, during the construction of the dam, those specific locations, which are identified as problematic areas, need effective ground improvement works and special monitoring.
埃塞俄比亚亚的斯亚贝巴西北部Gullele植物园坝址水密性评价的综合地球物理和封隔器测试
Gullele植物园是埃塞俄比亚最大的植物园之一,位于亚的斯亚贝巴西北部。对于这个花园,建议建造一个水坝用于灌溉和娱乐目的。拟建的大坝高30米,坝轴长约180米。这项工作的主要目的是在详细的地质、岩土和地球物理调查的基础上,对拟建坝址的工程地质方面进行调查和评价。在该地区进行的调查包括电阻率成像、VES、钻孔和单个封隔器渗透率测试。地质上,该地区被不同的火山岩覆盖,如火成岩、流纹岩、凝灰岩、玄武岩和残余土壤;地质构造如节理、裂隙、流带、冷却节理等。地质构造以南北向和东西向为主。不同的调查结果表明,确定了三个岩土层。这些是覆盖层(完全风化的褐煤和土壤),高度至中度风化的褐煤和中度至轻度风化的褐煤岩体。6个钻孔岩体渗透性试验的吕根值范围为0 ~ 9。坝址左坝肩和河床的最大岩体渗透性值分别表现为冲蚀和扩容行为。渗透性分析结果表明,拟建大坝的左坝肩、河床和水库可能存在渗流问题。因此,在大坝建设过程中,那些被确定为问题区域的特定位置,需要进行有效的地面改善工程和专门的监测。
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