Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions

Slope instability has been identified as one of the most natural and man-made disasters that can lead to the life of humans in danger and enormous loss of capital. The roads which pass on the hilly and mountainous terrains are frequently affected by slope failures since hilly and mountainous areas a...

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Main Authors: Meko Leta, Chemeda Yadeta C., Meko Bikila
Format: Article
Language:English
Published: De Gruyter 2023-11-01
Series:Open Geosciences
Subjects:
Online Access:https://doi.org/10.1515/geo-2022-0561
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author Meko Leta
Chemeda Yadeta C.
Meko Bikila
author_facet Meko Leta
Chemeda Yadeta C.
Meko Bikila
author_sort Meko Leta
collection DOAJ
description Slope instability has been identified as one of the most natural and man-made disasters that can lead to the life of humans in danger and enormous loss of capital. The roads which pass on the hilly and mountainous terrains are frequently affected by slope failures since hilly and mountainous areas are characterized by variable topographical, geological, hydrological, and land-use conditions. Slope stability analysis was carried out using FEM (plaxis 2D) and LEM (slide software). The stability analysis covers both static and dynamic (in pseudo-static analysis) loading conditions on soil and rock material along selected critical slope sections. Two soil-critical slope sections and two rock-critical slope sections are analyzed in this study. The strength reduction method and method of the slice with Mohr–Coulomb model were used in FEM and LEM, respectively. The slope stability analysis was carried out for both dry and wet states of the soil and rock material along the critical slope sections (i.e., static dry, dynamic dry, static wet, and dynamic wet). The analysis result shows that the total displacement of the slope along soil critical slope section one is (0.58703, 0.58755, 2.35, and 2.38 m), along soil critical slope section two is (0.6574, 0.6621, 1.2841, and 1.2872 m), along rock-critical slope section one is (4.8624, 4.8672, 17.8463, and 17.8512 m) and total displacement along rock-critical slope section two is (3.8365, 3.8391, 11.437, and 11.6275 m) during static dry, dynamic dry, static wet, and dynamic wet loading conditions, respectively. In general, the result shows soil critical slope sections one and two are stable in dry conditions and unstable in wet conditions. Rock-critical slope sections are stable during the dry and wet states of the slope.
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spelling doaj.art-76613442c2a141c48a42e57cf5b024b32023-11-20T07:16:05ZengDe GruyterOpen Geosciences2391-54472023-11-0115159360210.1515/geo-2022-0561Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditionsMeko Leta0Chemeda Yadeta C.1Meko Bikila2Department of Civil Engineering, Adama Science and Technology University, Adama, EthiopiaDepartment of Geology, Adama Science and Technology University, Adama, EthiopiaDepartment of Construction Technology and Management, Wolkite University, Wolkite, EthiopiaSlope instability has been identified as one of the most natural and man-made disasters that can lead to the life of humans in danger and enormous loss of capital. The roads which pass on the hilly and mountainous terrains are frequently affected by slope failures since hilly and mountainous areas are characterized by variable topographical, geological, hydrological, and land-use conditions. Slope stability analysis was carried out using FEM (plaxis 2D) and LEM (slide software). The stability analysis covers both static and dynamic (in pseudo-static analysis) loading conditions on soil and rock material along selected critical slope sections. Two soil-critical slope sections and two rock-critical slope sections are analyzed in this study. The strength reduction method and method of the slice with Mohr–Coulomb model were used in FEM and LEM, respectively. The slope stability analysis was carried out for both dry and wet states of the soil and rock material along the critical slope sections (i.e., static dry, dynamic dry, static wet, and dynamic wet). The analysis result shows that the total displacement of the slope along soil critical slope section one is (0.58703, 0.58755, 2.35, and 2.38 m), along soil critical slope section two is (0.6574, 0.6621, 1.2841, and 1.2872 m), along rock-critical slope section one is (4.8624, 4.8672, 17.8463, and 17.8512 m) and total displacement along rock-critical slope section two is (3.8365, 3.8391, 11.437, and 11.6275 m) during static dry, dynamic dry, static wet, and dynamic wet loading conditions, respectively. In general, the result shows soil critical slope sections one and two are stable in dry conditions and unstable in wet conditions. Rock-critical slope sections are stable during the dry and wet states of the slope.https://doi.org/10.1515/geo-2022-0561slope stabilityslope failurecritical slope sectionpseudo-static analysis
spellingShingle Meko Leta
Chemeda Yadeta C.
Meko Bikila
Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
Open Geosciences
slope stability
slope failure
critical slope section
pseudo-static analysis
title Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
title_full Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
title_fullStr Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
title_full_unstemmed Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
title_short Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
title_sort road cut slope stability analysis for static and dynamic pseudo static analysis loading conditions
topic slope stability
slope failure
critical slope section
pseudo-static analysis
url https://doi.org/10.1515/geo-2022-0561
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