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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=24861"><dc:title>Evaluation of cut slope stability in the Lesser Himalaya of Nepal</dc:title><dc:creator>Shrestha,	Krishna Kumar	(Avtor)
	</dc:creator><dc:creator>Paudyal,	Kabi Raj	(Avtor)
	</dc:creator><dc:creator>Pathak,	Dinesh	(Avtor)
	</dc:creator><dc:creator>Franci,	Alessandro	(Avtor)
	</dc:creator><dc:creator>Thapa,	Prem Bahadur	(Avtor)
	</dc:creator><dc:subject>cut slope</dc:subject><dc:subject>slope stability</dc:subject><dc:subject>numerical modelling</dc:subject><dc:subject>evaluation and validation</dc:subject><dc:subject>Lesser Himalaya</dc:subject><dc:subject>Nepal</dc:subject><dc:description>A spatial inventory of cut slopes in the central and western Lesser Himalaya of Nepal was prepared and characterised to evaluate their stability. The stability of these cut slopes is governed by the geotechnical properties of rock/soil together with  slope  geometry,  groundwater  conditions  and  human  interventions.  Numerous  cut  slope  failures  were  observed  in  areas  where  slope  geometry  is  modified  for  engineering  developments  such  as  roads,  dams,  powerhouses,  industrial  development, etc. Two modelling sites were evaluated using the Limit Equilibrium Method (LEM), Finite Element Method (FEM), and Particle Finite Element Method (PFEM). Pre-failure analyses using LEM and FEM under dry and saturated conditions revealed that the stability of the Lesser Himalayan hillslopes with considerable soil thickness is predominantly controlled  by  the  depth  of  groundwater  level  (GWL).  Slopes  remain  stable  with  a  factor  of  safety  (FoS)&gt;1.3  when  the  GWL  lies  below  7  m  from  the  surface  and  gradually  become  unstable  as  it  approaches  the  surface.  This  trend  for  both  slopes confirms that elevated groundwater during the rainy season is the major cause of frequent cut slope failures in the Himalayan regions. The comparison of FoS from LEM and Strength Reduction Factor (SRF) from FEM showed a strong cross-correlation (90–99 %), revealing minimal variation which affirmed the validity of the adopted modelling techniques used in this study. Post-failure simulations of these sites were further analysed using an innovative approach, the robust PFEM modelling technique, to compute the dynamic failure mechanism. Sensitivity analysis of both modelled sites showed that friction angle and cohesion are the most significant parameters for slope stability evaluation. Moreover, forward and back analyses indicated that computed results are in good agreement, thus depicting reliability and performances along with the model validation.</dc:description><dc:publisher>Geološki zavod Slovenije</dc:publisher><dc:date>2025</dc:date><dc:date>2025-12-23 03:58:33</dc:date><dc:type>Neznano</dc:type><dc:identifier>24861</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
