Slope stability analysis of colluvial deposits along the Muketuri-Alem Ketema Road, Northern Ethiopia

IF 2.9 Q2 GEOGRAPHY, PHYSICAL
Hirei Mohammed Hussen , Endalu Tadele Chala , Nagessa Zerihun Jilo
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Abstract

Slope failures are a significant natural geohazard in hilly and mountainous regions, often resulting in loss of life and infrastructure damage. The Muketuri-Alem Ketema road in Ethiopia is particularly vulnerable to landslides due to colluvial deposits on steep slopes from the higher northeastern plots to the lower Jemma River valley. This study investigates the characteristics of colluvial soil and evaluates the stability of slopes prone to landslides. It combines geophysical data, penetrometer tests, laboratory analyses, Google Earth images, and detailed field visits to assess the soil and bedrock composition and structure. Numerical methods, including limit equilibrium (Bishop, Janbu, Spencer, and Morgenstern-Price methods) and finite element methods, were used to analyze slope sections under various saturation conditions and simulate different rainfall patterns. The results indicate that the Bishop, Morgenstern-Price, and Spencer methods produce similar safety factors with minimal differences (<0.3%), while the Janbu method shows more significant variation (1.5%–5.6%). Safety factor differences for sections A-A and B-B range from 5.26% to 9.86% and 3.5%–4.7%, respectively. Simulations reveal that short-term saturation significantly reduces the stability of the upper slope layer by 20%–46.76%, and long-term saturation decreases the entire slope section by 26.81%–46.76% compared to dry conditions due to increased pore water pressure and self-weight. Long-term saturation effects, combined with dynamic loads, can further reduce colluvial soil stability by over 50% compared to a dry static state. The finite element method predicts larger failure zones than limit equilibrium methods, emphasizing the need for accurate predictions to characterize slope behavior during failure and inform stabilization decisions. This study provides crucial data for maintaining and planning the Muketuri-Alem Ketema Road, highlighting slope performance over time and the effectiveness of stabilization techniques.

埃塞俄比亚北部 Muketuri-Alem Ketema 公路沿线冲积层的边坡稳定性分析
斜坡崩塌是丘陵和山区的一种重大自然地质灾害,经常造成生命损失和基础设施破坏。埃塞俄比亚的 Muketuri-Alem Ketema 公路从东北部高地到杰马河谷下游的陡峭斜坡上的冲积土特别容易发生山体滑坡。本研究调查了冲积土的特征,并评估了易发生山体滑坡的斜坡的稳定性。研究结合了地球物理数据、渗透仪测试、实验室分析、谷歌地球图像和详细的实地考察,以评估土壤和基岩的组成和结构。数值方法包括极限平衡法(Bishop、Janbu、Spencer 和 Morgenstern-Price 方法)和有限元方法,用于分析各种饱和条件下的斜坡断面,并模拟不同的降雨模式。结果表明,Bishop 法、Morgenstern-Price 法和 Spencer 法产生的安全系数相似,差异很小(0.3%),而 Janbu 法的差异更大(1.5%-5.6%)。A-A 段和 B-B 段的安全系数差异分别为 5.26% 至 9.86% 和 3.5% 至 4.7%。模拟结果表明,与干燥条件相比,由于孔隙水压力和自重增加,短期饱和会使斜坡上层的稳定性明显降低 20%-46.76%,长期饱和会使整个斜坡断面的稳定性降低 26.81%-46.76%。与干燥静态相比,长期饱和效应加上动荷载会使冲积土稳定性进一步降低 50%以上。与极限平衡法相比,有限元法预测的破坏区域更大,这强调了准确预测的必要性,以描述破坏过程中的边坡行为,并为稳定决策提供依据。这项研究为维护和规划 Muketuri-Alem Ketema 公路提供了重要数据,突出了斜坡随时间变化的性能以及稳定技术的有效性。
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
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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