Evaluation of watertightness and slope stability analysis of Upper Guder dam, West Showa, Central Ethiopia

IF 2.9 Q2 GEOGRAPHY, PHYSICAL Quaternary Science Advances Pub Date : 2024-08-13 DOI:10.1016/j.qsa.2024.100230
Belay Birhanu , Yadeta C. Chemeda , Tola Garo , Shankar Karuppannan
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Abstract

Ethiopia is currently emphasizing the construction of micro dams to enhance agricultural productivity and assure food security. The Upper Guder Dam, situated in the West Shoa Zone, Central Ethiopia, is one such project. However, the dam faces challenges due to complex geological and structural conditions, including leakage and slope instability. Hence, this study focuses on addressing the abutment slope stability and watertightness condition of this dam. Accordingly, the study employed discontinuity surveying, Seismic Refraction Tomography (SRT), Rock Quality Designation (RQD), and Lugeon testing to assess the water tightness. Additionally, kinematic analysis and the Limit Equilibrium Method (LEM) were used to evaluate abutment slope stability. Results from surface geological mapping and core drilling showed that the dam site is constituted by quaternary soil, tuff, and basalt. The Lugeon test results indicate that the left abutment of the dam is susceptible to leakage down to a depth of 40 m, which suggests that the permeable zone extends deeper than the results revealed by the SRT. Furthermore, this test demonstrated that the dam's right and central foundations are susceptible to leakage to the drilled depths. The SRT revealed that the central foundation, right, and left abutments of the dam are susceptible to leakage to the depth of 35 m, 30 m, and 34 m, respectively. Moreover, the kinematic analysis revealed that a section of the left abutment of the dam is susceptible to wedge mode of failure due to the intersection of JS1 and JS2. The LEM modeling of the right abutment of the dam also depicted that this section of the dam is unstable under saturated conditions which illustrates the importance of precipitation as the major slope destabilizing factor in the study area. Based on the study findings, this study recommended the use of curtain grouting to address the water tightness issue and slope angle reduction to mitigate the slope instability problem.

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埃塞俄比亚中部西昭和上古德大坝的水密性评估和边坡稳定性分析
埃塞俄比亚目前正在大力建设微型水坝,以提高农业生产力,确保粮食安全。位于埃塞俄比亚中部西肖亚区的上古德水坝就是这样一个项目。然而,由于复杂的地质和结构条件,包括渗漏和斜坡不稳定性,大坝面临着挑战。因此,本研究的重点是解决该大坝的坝基边坡稳定性和水密性问题。因此,研究采用了不连续性测量、地震折射层析成像(SRT)、岩质指定(RQD)和 Lugeon 测试来评估水密性。此外,还采用了运动学分析和极限平衡法 (LEM) 评估桥墩边坡的稳定性。地表地质绘图和岩心钻探结果表明,坝址由第四纪土壤、凝灰岩和玄武岩构成。Lugeon 试验结果表明,大坝左侧坝台的渗漏深度可达 40 米,这表明渗透带的深度比 SRT 揭示的结果更深。此外,该试验还表明,大坝的右侧和中央地基在钻探深度范围内容易发生渗漏。SRT 显示,大坝的中央地基、右侧和左侧桥墩的渗漏深度分别为 35 米、30 米和 34 米。此外,运动学分析表明,由于 JS1 和 JS2 相交,大坝左侧桥墩的一部分容易发生楔形破坏。大坝右侧墩台的 LEM 模型也显示,该段大坝在饱和条件下不稳定,这说明降水是研究区域内破坏斜坡稳定的主要因素。根据研究结果,本研究建议使用帷幕灌浆来解决水密性问题,并通过减小斜坡角度来缓解斜坡不稳定问题。
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来源期刊
Quaternary Science Advances
Quaternary Science Advances Earth and Planetary Sciences-Earth-Surface Processes
CiteScore
4.00
自引率
13.30%
发文量
16
审稿时长
61 days
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