Engineering geological investigation of Gololcha dam for evaluation of leakage and abutment slope stability, Eastern Ethiopia

IF 2.7 Q2 MULTIDISCIPLINARY SCIENCES
Sishaw Merdassa , Tola Garo , Yadeta C. Chemeda , Shankar Karuppannan , Mahlet Tesfaye
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Abstract

The Ethiopian economy is primarily dependent on agriculture, making the construction of water harvesting facilities, such as dams, crucial for improving the productivity of this sector. The ongoing construction of the Gololcha dam on the Kurkura River located in Eastern Ethiopia aims to enhance irrigation schemes in the region. However, the dam site's complex geological and structural conditions pose challenges related to leakage and slope instability. Hence, this study focuses on addressing the abutment slope stability and leakage condition of this dam. This study employed kinematic analysis and the Limit Equilibrium Method (LEM) to assess slope stability. Additionally, engineering geological mapping, discontinuity surveys, seismic refraction tomography (SRT), and in-situ permeability testing were used to evaluate the leakage condition of the dam site. Notably, the permeability and SRT survey results identified potential leakage zones to the depth of 35, 30, and 35 m at the left, right, and central foundations of the dam, respectively. The kinematic method revealed one planar and two wedge modes of failure in the slope section covered by slightly weathered and fractured basalt rock at the right abutment. Further stability analysis of these two modes of failures via LEM analysis indicated slope instability under saturated conditions, emphasizing the role of pore water pressure. Furthermore, LEM modeling was directly utilized using the Slide 6.0 software to analyze the slope stability condition of the left abutment of the dam. This modeling also uncovered instability under saturated conditions. Based on the study findings, this study recommended curtain grouting to address potential leakage, as well as slope flattening and removing unstable rock wedges and loose material to stabilize unstable slope sections.
为评估埃塞俄比亚东部 Gololcha 大坝的渗漏和坝基边坡稳定性而进行的工程地质调查
埃塞俄比亚的经济主要依赖农业,因此建造水坝等集水设施对于提高农业生产率至关重要。正在埃塞俄比亚东部库尔库拉河上修建的 Gololcha 大坝旨在加强该地区的灌溉计划。然而,坝址复杂的地质和结构条件带来了与渗漏和斜坡不稳定性有关的挑战。因此,本研究重点关注该大坝的坝基边坡稳定性和渗漏状况。本研究采用运动分析和极限平衡法(LEM)来评估边坡稳定性。此外,还采用了工程地质测绘、不连续性勘测、地震折射断层扫描(SRT)和原位渗透性测试来评估坝址的渗漏状况。值得注意的是,渗透性和 SRT 勘测结果表明,大坝左、右和中央地基的潜在渗漏区深度分别为 35 米、30 米和 35 米。运动学方法显示,在右侧坝基被轻微风化和断裂的玄武岩覆盖的斜坡部分,存在一种平面溃坝模式和两种楔形溃坝模式。通过 LEM 分析法对这两种破坏模式进行的进一步稳定性分析表明,边坡在饱和条件下不稳定,强调了孔隙水压力的作用。此外,还使用 Slide 6.0 软件直接利用 LEM 模型分析了大坝左侧支墩的边坡稳定性状况。该模型还揭示了饱和条件下的不稳定性。根据研究结果,本研究建议采用帷幕灌浆法来解决潜在的渗漏问题,并对斜坡进行平整,清除不稳定的岩楔和松散材料,以稳定不稳定的斜坡部分。
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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来源期刊
Scientific African
Scientific African Multidisciplinary-Multidisciplinary
CiteScore
5.60
自引率
3.40%
发文量
332
审稿时长
10 weeks
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