2017
DOI: 10.3390/su9071280
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Analysis of Rainfall-Induced Landslide on Unsaturated Soil Slopes

Abstract: This paper investigates rainfall-induced landslides on partially saturated soil slopes using the 2011 Umyeonsan landslides at the center of Seoul, Korea. An integrated analysis of rainfall-induced landslide was carried out through laboratory tests, field tests, and numerical analysis. The results of comprehensive investigations in the Umyeonsan region demonstrate that landslide activity is closely related primarily to rainfall and soil properties and slope geometry, and vegetation. Numerical analysis was also … Show more

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Cited by 74 publications
(50 citation statements)
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“…The stability of slopes is judged based on a computed safety factor [31][32][33][34][35], an assessment of slope deformation [36], or a partial safety factor [37]. Most of the computer programs used for slope stability analysis are based on the limiting equilibrium approach for a two-dimensional model [38].…”
Section: Slope Stability Analysismentioning
confidence: 99%
“…The stability of slopes is judged based on a computed safety factor [31][32][33][34][35], an assessment of slope deformation [36], or a partial safety factor [37]. Most of the computer programs used for slope stability analysis are based on the limiting equilibrium approach for a two-dimensional model [38].…”
Section: Slope Stability Analysismentioning
confidence: 99%
“…Although numerous empirically based approaches have been widely applied to large areas using simple methods, deterministic physics-based approaches are preferable for a better understanding of the mechanisms of shallow landslides [13]. Numerous physically based studies have investigated infiltration behavior during rainfall using various approaches: (1) Adopting assumptions for simplification to solve the differential equation of Richards [14] by applying a single-phase fluid (water) flow [3,10,15,16]; (2) assuming that the air pressure in the void spaces of an unsaturated soil slope is equal to the atmospheric pressure [9,17,18]; (3) applying a two-phase fluid (water and air) flow [19][20][21][22][23]; and (4) considering hydraulic hysteresis, including the effects of capillarity and/or air entrapment, reflecting different hydraulic states under wetting and drying conditions [24,25]. Such physically based numerical studies have mainly been applied at slope or watershed scales.…”
Section: Introductionmentioning
confidence: 99%
“…However, such simulation in a 3D scheme incurs an excessive amount of computation [16]. Park et al [30], Jeong et al [15], Tran et al [16], and Tran et al [31] assessed the slope failures that occurred at Umyeon Mountain in Seoul, South Korea in 2011 using SEEP/W and SLOPE/W [32], TRIGRS [33], TiVaSS [34], and Scoops3D [29], respectively. However, air flow was not considered.…”
Section: Introductionmentioning
confidence: 99%
“…Landslides-defined as the displacement of soil and rocks on slopes-are one of the most common natural hazards in many mountainous areas and greatly affect the social sustainability of human beings [1][2][3]. They can have natural causes, such as heavy rainfall and earthquakes, but also human causes, including urban encroachments and increased surface impermeability to water infiltration.…”
Section: Introductionmentioning
confidence: 99%