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The Influence of Climatic, Geological and Hydrodynamic Factors on Slope Stability at Kekem in the West Region of Cameroon

Received: 12 August 2024     Accepted: 2 September 2024     Published: 23 September 2024
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Abstract

This study focuses on the influence of climatic, geological and hydrodynamic factors on slope stability of Kekem located in the Western Highlands of Cameroon. The methodological approach was based on the analysis of three factors: hydrological, geological and assessment of the hydrodynamic parameters influencing the stability of slopes. The hydrological factors indicate an average annual rainfall of 1,763.04 mm, generating 248.59 mm of runoff and around 402.61 mm of infiltrated water. Geologically, the soils have a high angle of friction at all three elevations, from 25.8° at the bottom of the slope to 27.2° at mid-slope and 26.2° at the top. On the other hand, the cohesion of these soils remains low, varying from 0.325 bar at the bottom of the slope to 0.265 bar at the top and 0.225 bar at mid-slope. Permeability analysis yielded values ranging from 1 x 10-9 to 1 x 10-11 m/s, with an overall porosity of around 55%. These conditions, combined with the morphology of the environment, are the main causes of slope instability in the Kekem district.

Published in International Journal of Environmental Protection and Policy (Volume 12, Issue 5)
DOI 10.11648/j.ijepp.20241205.12
Page(s) 129-138
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This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.

Copyright

Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Climatic, Geological, Hydrodynamic, Factors, Slope Stability, Kekem

References
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    Fotso, L. N., Katte, V. Y., Ntankouo, R. N., Emile, T. (2024). The Influence of Climatic, Geological and Hydrodynamic Factors on Slope Stability at Kekem in the West Region of Cameroon. International Journal of Environmental Protection and Policy, 12(5), 129-138. https://doi.org/10.11648/j.ijepp.20241205.12

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    ACS Style

    Fotso, L. N.; Katte, V. Y.; Ntankouo, R. N.; Emile, T. The Influence of Climatic, Geological and Hydrodynamic Factors on Slope Stability at Kekem in the West Region of Cameroon. Int. J. Environ. Prot. Policy 2024, 12(5), 129-138. doi: 10.11648/j.ijepp.20241205.12

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    AMA Style

    Fotso LN, Katte VY, Ntankouo RN, Emile T. The Influence of Climatic, Geological and Hydrodynamic Factors on Slope Stability at Kekem in the West Region of Cameroon. Int J Environ Prot Policy. 2024;12(5):129-138. doi: 10.11648/j.ijepp.20241205.12

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  • @article{10.11648/j.ijepp.20241205.12,
      author = {Leroy Ngadji Fotso and Valentine Yato Katte and Roger Njila Ntankouo and Temgoua Emile},
      title = {The Influence of Climatic, Geological and Hydrodynamic Factors on Slope Stability at Kekem in the West Region of Cameroon
    },
      journal = {International Journal of Environmental Protection and Policy},
      volume = {12},
      number = {5},
      pages = {129-138},
      doi = {10.11648/j.ijepp.20241205.12},
      url = {https://doi.org/10.11648/j.ijepp.20241205.12},
      eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ijepp.20241205.12},
      abstract = {This study focuses on the influence of climatic, geological and hydrodynamic factors on slope stability of Kekem located in the Western Highlands of Cameroon. The methodological approach was based on the analysis of three factors: hydrological, geological and assessment of the hydrodynamic parameters influencing the stability of slopes. The hydrological factors indicate an average annual rainfall of 1,763.04 mm, generating 248.59 mm of runoff and around 402.61 mm of infiltrated water. Geologically, the soils have a high angle of friction at all three elevations, from 25.8° at the bottom of the slope to 27.2° at mid-slope and 26.2° at the top. On the other hand, the cohesion of these soils remains low, varying from 0.325 bar at the bottom of the slope to 0.265 bar at the top and 0.225 bar at mid-slope. Permeability analysis yielded values ranging from 1 x 10-9 to 1 x 10-11 m/s, with an overall porosity of around 55%. These conditions, combined with the morphology of the environment, are the main causes of slope instability in the Kekem district.},
     year = {2024}
    }
    

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  • TY  - JOUR
    T1  - The Influence of Climatic, Geological and Hydrodynamic Factors on Slope Stability at Kekem in the West Region of Cameroon
    
    AU  - Leroy Ngadji Fotso
    AU  - Valentine Yato Katte
    AU  - Roger Njila Ntankouo
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    PB  - Science Publishing Group
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    UR  - https://doi.org/10.11648/j.ijepp.20241205.12
    AB  - This study focuses on the influence of climatic, geological and hydrodynamic factors on slope stability of Kekem located in the Western Highlands of Cameroon. The methodological approach was based on the analysis of three factors: hydrological, geological and assessment of the hydrodynamic parameters influencing the stability of slopes. The hydrological factors indicate an average annual rainfall of 1,763.04 mm, generating 248.59 mm of runoff and around 402.61 mm of infiltrated water. Geologically, the soils have a high angle of friction at all three elevations, from 25.8° at the bottom of the slope to 27.2° at mid-slope and 26.2° at the top. On the other hand, the cohesion of these soils remains low, varying from 0.325 bar at the bottom of the slope to 0.265 bar at the top and 0.225 bar at mid-slope. Permeability analysis yielded values ranging from 1 x 10-9 to 1 x 10-11 m/s, with an overall porosity of around 55%. These conditions, combined with the morphology of the environment, are the main causes of slope instability in the Kekem district.
    VL  - 12
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