2015
DOI: 10.1016/j.enggeo.2015.05.011
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The influence of the unsaturated soil zone on 2-D and 3-D slope stability analyses

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Cited by 45 publications
(9 citation statements)
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“…a) b) Figure 13. 3D numerical models of slopes of a more complex geometry with the sliding mass of the soil separately shown [35] Na slici 14 prikazani su 3D numerički modeli kosina nešto složenije geometrije, s prikazanom izdvojenom kliznom masom tla i položajima proračunatih tačaka faktora sigurnosti, dobijenih optimizacijom za konkavnu i konveksnu kliznu površ. Konkavna klizna površ formirana je iz 3D prostornih konačnih elemenata, dok je konveksna klizna površ formirana kombinacijom 3D prostornih i 2D površinskih konačnih elemenata.…”
Section: A) B)unclassified
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“…a) b) Figure 13. 3D numerical models of slopes of a more complex geometry with the sliding mass of the soil separately shown [35] Na slici 14 prikazani su 3D numerički modeli kosina nešto složenije geometrije, s prikazanom izdvojenom kliznom masom tla i položajima proračunatih tačaka faktora sigurnosti, dobijenih optimizacijom za konkavnu i konveksnu kliznu površ. Konkavna klizna površ formirana je iz 3D prostornih konačnih elemenata, dok je konveksna klizna površ formirana kombinacijom 3D prostornih i 2D površinskih konačnih elemenata.…”
Section: A) B)unclassified
“…The concave sliding surface is formed from 3D spatial finite elements, while the convex sliding surface is formed by combining 3D spatial and 2D surface finite elements. sliding surface [35] Modeliranje omekšanja i diskontinuiteta u tlu sprovodi se korekcijom parametara konstitutivnog modela ponašanja tla i eliminacijom veze određenih konačnih elemenata ili čak redukcijom određenog broja konačnih elemenata koji se nalaze u posebnoj zoni progušćenja mreže konačnih elemenata. Aproksimacija se odnosi na izbor optimalnog tipa konačnog elementa kojim se efikasno modelira polje pomeranja tla u modelu kosine.…”
Section: A) B)unclassified
“…In order to simplify the calculation process for FS , a vast majority of slope stability analyses in engineering practice are performed in two‐dimensions (2D) under plane strain assumption, in which the slope is assumed to be infinitely wide such that three‐dimensional (3D) end effects are negligible. However, numerous natural and constructed practical slopes exhibit a complex geometric configuration and a 3D state 1–4 . From reported slopes in the literature, 2,5,6 relative differences between the two‐dimensional factor of safety ( FS2D ) and three‐dimensional factor of safety ( FS3D ) are found greater than 50%.…”
Section: Introductionmentioning
confidence: 99%
“…However, numerous natural and constructed practical slopes exhibit a complex geometric configuration and a 3D state 1–4 . From reported slopes in the literature, 2,5,6 relative differences between the two‐dimensional factor of safety ( FS2D ) and three‐dimensional factor of safety ( FS3D ) are found greater than 50%. Therefore, the prediction based on 2D analysis can be excessively conservative and economically unjustified.…”
Section: Introductionmentioning
confidence: 99%
“…It is widely considered that hydraulic factors such as atmospheric precipitation, fluctuation, and the change rate of the water level of the reservoir, as well as river wave erosion, etc., could reduce the stability of bank slopes, even leading to landslide disasters. Landslides often occur after long rainy periods due to the increase in the positive pore pressure on a potential sliding surface and the decrease in the stability of deeper slopes [9][10][11]. If intense rainfall occurs or the water level of the reservoir fluctuates rapidly, shallow landslides can occur as the moisture content in the soil becomes close to saturation, resulting in a considerable reduction in soil strength [12,13].…”
Section: Introductionmentioning
confidence: 99%