利用极限平衡和有限元方法建立斜坡稳定性模型:埃塞俄比亚北部主裂谷阿达玛市案例研究

IF 2.9 Q2 GEOGRAPHY, PHYSICAL
Tola Garo , Mahlet Tesfaye , Shankar Karuppannan
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引用次数: 0

摘要

斜坡崩塌是埃塞俄比亚许多地区经常出现的一种突出地质灾害,包括位于埃塞俄比亚北部主裂谷(NMER)的阿达玛市。该市被东北-西南走向的两条山脊环绕,很容易发生斜坡失稳。因此,本研究旨在使用有限元法(FEM)和极限平衡法(LEM)对这两条山脊沿线的斜坡稳定性进行建模。建模是在由冲积土、浮石和中度至高度风化的火烧云组成的多层面几何斜坡上进行的。利用卫星图像以及坡脚状况和坡面倾斜等实地表现,确定了关键坡段。然后根据实地数据从详细的地质横截面推断出它们的几何形状。建模的输入参数,如内聚力、摩擦角和弹性模量,是通过使用 Hoek-Brown 准则的回溯分析计算得出的,而单位重量和泊松比则是根据经验公式确定的。土层参数则通过标准实验室实验确定。然后在不同条件下进行建模,包括干燥、饱和、静态和动态条件。LEM 和 FEM 模型的结果表明,在动态和饱和条件下,所分析的四个坡段中有三个不稳定,这突出了降水和地震作为触发变量的影响和重要性。在两种模型中,当临界滑移面通过单一地质材料时,两种方法的结果趋于一致。然而,当滑移面涉及多种地质材料时,两种方法的结果就会出现明显差异。在这种情况下,LEM 的 FOS 值往往高于 FEM。研究结果还显示,根据两种模型和实地数据生成的崩塌面推断,所有不稳定斜坡都与研究区域的 NNE-SSW 走向断层有关。研究得出结论,不稳定斜坡对附近居民和基础设施构成严重威胁,作为补救措施,研究设计并推荐了耦合台阶和斜坡平整。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Slope stability modeling using limit equilibrium and finite element methods: A case study of the Adama City, Northern Main Ethiopian Rift

Slope failure is a prominent and recurring geohazard in numerous parts of Ethiopia, including Adama City, which is located in the Northern Main Ethiopian Rift (NMER). The city is surrounded by two ridges oriented in the NNE-SSW direction, which are susceptible to slope instability. Thus, this study is aimed at modeling slope stability along these two ridges using Finite Element Method (FEM) and Limit Equilibrium Method (LEM). The modeling was carried out on slopes of multifaceted geometry composed of eluvium soil, pumice, and moderately to highly-weathered ignimbrites. Critical slope sections were identified using satellite imagery and field manifestations such as slope toe condition and slope face tilting. Their geometries were then inferred from detailed geological cross-sections based on field data. Input parameters for the modeling, such as cohesion, friction angle, and elastic modulus, were calculated via Back Analysis using the Hoek-Brown criterion while unit weight and Poisson ratio were determined from empirical equations. For soil formations, the parameters were determined via standard laboratory experiments. The modeling was then carried out under different conditions, including dry, saturated, static, and dynamic conditions. Results from both LEM and FEM models revealed that three of the four analyzed slope segments were unstable under dynamic and saturated conditions, highlighting the influence and importance of precipitation and seismicity as triggering variables. Results from both methods tend to agree when the critical slip surface passes through a single geological material in both models. However, notable differences arise when the slip surface involves multiple geological materials. Under such conditions, LEM tends to yield higher FOS values compared to FEM. The results also showed that all unstable slopes were associated with the NNE-SSW striking fault of the study area, as inferred from failure surfaces generated from both models and field data. The study concluded that unstable slopes pose a serious risk to nearby residents and infrastructure, and as a remedy, it designed and recommended coupled benching and slope flattening.

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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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