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Failure mechanism analysis of rainfall-induced landslide at Pingguang stream in Taiwan: mapping, investigation, and numerical simulation

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Abstract

On September 15, 2012, torrential rains carried by the peripheral circulation of Typhoon Sanba and the northeast monsoon induced a translational landslide near Pingguang Road in Xindian District of New Taipei City, Taiwan. The total volume of the landslide was ~162,000 m3. The sliding mass destroyed two houses across the stream and formed a landslide dam at the toe of the slope, constricting the stream. For the purpose of reducing sediment-relative hazard around mountainous area, the paper attempts to explore the dynamics and phenomenon of the landslide on dip slope. This study interpreted remote sensing images and terrestrial LiDAR scanning, conducted onsite surveys to obtain material parameters, and performed simulations using the discrete element method to reconstruction the post-event, in order to elucidate the mechanisms involved in the landslide process. Survey results revealed complex geological conditions with tension cracks spreading in all directions at source area. This facilitated the infiltration of surface runoff into weak surfaces and raised groundwater levels. Slope failure may occur along the stratum boundary once the intrinsic shear strength of regolith drops below a critical value. The results of numerical simulation reveal that at 80 s after the Pingguang stream landslide began, a maximum deposition depth of 20 m had been reached. The sliding mass cut off the stream and pushed the stream flow roughly 35 m to the southeast. Because the slope materials surrounding the study area and the landslide-inducing mechanisms are similar, the top of the slopes to the northwest of the study area requires close monitoring. Finally, a detailed potential landslide mapping and interpretation from the high-resolution digital elevation model also present to prevent further landslides. The investigation indicates that the occurrence of landslide is highly related to seepage effect of accumulated rainfall, toe erosion by surface runoff, and local unstable geological structure.

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References

  • Aleotti P (2004) A warning system for rainfall-induced shallow failures. Eng Geol 73:247–265

    Article  Google Scholar 

  • Central Geological Survey (2000) Explanatory text of the Geological Map of Taiwan, scale 1:50,000. Central Geological Survey, Xindian (in Chinese)

    Google Scholar 

  • Chang KT, Chiang SH, Lei F (2007) Analysing the relationship between Typhoon triggered landslides and critical rainfall conditions. Earth Surf Proc Land 33(8):1261–1271

    Article  Google Scholar 

  • Chang KT, Lin ML, Dong JJ, Chien CH (2012) The Hungtsaiping landslides: from ancient to recent. Landslides 9(2):205–214

    Article  Google Scholar 

  • Chen CY (2009) Sedimentary impacts from landslides in the Tachia River Basin, Taiwan. Geomorphology 105(3–4):355–365

    Article  Google Scholar 

  • Chigira M (2014) Geological and geomorphological features of deep-seated catastrophic landslides in tectonically active regions of Asia and implications for hazard mapping. Episodes 37(4):284–294

    Google Scholar 

  • Chou HT, Lee CF, Lo CM, Lin CP (2012)1 Landslide and alluvial fan caused by an extreme rainfall in Suao, Taiwan. 11th International symposium on landslides (ISL) and the 2nd North American symposium on landslides, Banff, Alberta, Canada, pp 487–44

  • Chou HT, Lee CF, Chung YC, Hsiau SS (2012b)2 Discrete element modelling and experimental validation for the falling process of dry granular steps. Powder Technol 231:122–134

    Google Scholar 

  • Cundall PA, Strack ODL (1979) A discrete numerical model for granular assemblies. Geotechnique 29:47–65

    Article  Google Scholar 

  • Hoek E (1994) Strength of rock and rock masses. ISRM News J 2(2):4–16

    Google Scholar 

  • Hsu HH, Chen CT (2002) Observed and projected climate change in Taiwan. Meteorol Atmos Phys 79:87–104

    Article  Google Scholar 

  • Hungr O (2007) Dynamics of rapid landslides. Prog Landslide Sci, Chapter 4:47–56

    Article  Google Scholar 

  • Ikeya H, Mizuyama T (1982) Debris flow and deposition related study. Soil Res J 157:88–153 (in Japanese)

    Google Scholar 

  • Itasca Consulting Group Inc. (2002) PFC3D (particle flow code in three dimensions) theory and background. Version 3.0. Minneapolis, pp 1–26

  • Iverson RM (2005) Regulation of landslide motion by dilatancy and pore pressure feedback. J Geophys Res 110:F02015

    Article  Google Scholar 

  • Koc O (2008) Numerical analysis of rock mass falls using PFC3D. A comparison of two cases: Thurwieser rock avalanche and Frank slide. Master Thesis, Institute for Engineering Geology, Vienna University of Technology

  • Kou CY, Tai YC, Chen CC, Chang KJ, Siau AY, Dong JJ, Han RH, Shimamoto T, Lee CT (2011) The landslide stage of the Hsiaolin catastrophe: simulation and validation. J Geophys Res 116:F04007

    Google Scholar 

  • Lee CC, Yang CH, Liu HC, Wen KL, Wang ZB, Chen YJ (2008) A Study of the hydrogeological environment of the lishan landslide area using resistivity image profiling and borehole data. Eng Geol 98:115–125

    Article  Google Scholar 

  • Lee CF, Huang CM, Tsao TC, Wei LW, Huang WK, Cheng CT, Chi CC (2016) Combining rainfall parameter and landslide susceptibility to forecast shallow landslide in Taiwan. Geotech Eng J SEAGS AGSSEA 47(2):72–82

    Google Scholar 

  • Lin GW, Chena H, Chen YH, Horng MJ (2008) Influence of Typhoons and earthquakes on rainfall-induced landslides and suspended sediments discharge. Eng Geol 97:32–41

    Article  Google Scholar 

  • Lo CM, Lin ML, Tang CL, Hu JC (2011) A kinematic model of the Hsiaolin landslide calibrated to the morphology of the landslide deposit. Eng Geol 123:22–39

    Article  Google Scholar 

  • Lo CM, Lee CF, Chou HT, Lin ML (2014) Landslide at Su-Hua highway 115.9 k triggered by Typhoon Megi in Taiwan. Landslides 11(2):293–304

    Article  Google Scholar 

  • Potyondy D, Cundall P (2004) A bonded-particle model for rock. Int J Rock Mech Min Sci 41:1329–1364

    Article  Google Scholar 

  • Sassa K, Wang G (2003) Pore-pressure generation and movement of rainfall-induced landslides: effects of grain size and fine-particle content. Eng Geol 69:109–125

    Article  Google Scholar 

  • Serafim JL, Pereira JP (1983) Consideration of the geomechanical classification of Bieniawski. In: Proceedings international symposium on engineering geology and underground construction. Lisbon, vol 1(II), pp 33–44

  • Shou K, Chen Y, Liu H (2009) Hazard analysis of Li-shan landslide in Taiwan. Geomorphology 103(1):143–153

    Article  Google Scholar 

  • Steven NW, Simon D (2006) Particulate kinematic simulations of debris avalanches: interpretation of deposits and landslide seismic signals of Mount Saint Helens, 1980 May 18. Int J Geophys 167:991–1004

    Article  Google Scholar 

  • Tu JY, Chou C, Chu PS (2009) The Abrupt shift of Typhoon activity in the vicinity of Taiwan and its association with Western North Pacific-East Asian climate change. J Clim 22:3617–3628

    Article  Google Scholar 

  • Wang CC, Lin BX, Chen CT, Lo SH (2014) Quantifying the effects of long-term climate change on tropical cyclone rainfall using a cloud-resolving model: examples of two landfall Typhoons in Taiwan. J Clim 28:66–85

    Article  Google Scholar 

  • Water Resources Planning Institute (2015) Hydrology analysis of Tamsui River. Water Resources Agency, Ministry of Economic (in Chinese)

  • Wu CH, Chen SC (2004) The evaluation of the landslide potential prediction models used in Taiwan. J Soil Water Conserv 36(4):295–306 (in Chinese)

    Google Scholar 

  • Wu JH, Chen JH, Lu CW (2013) Investigation of the Hsien-du-Shan rock avalanche caused by typhoon Morakot in 2009 at Kaohsiung county, Taiwan. Int J Rock Mech Mining Sci 60:148–159

    Article  Google Scholar 

  • Wu CH, Chen SC, Feng ZY (2014) Formation, failure, and consequences of the Xiaolin landslide dam, triggered by extreme rainfall from Typhoon Morakot, Taiwan. Landslides 11:357–367

    Article  Google Scholar 

  • Yu CW (2007) Empirical method for estimating geomechanical parameters of rock mass in tunneling. J Taiwan Soc Public Works 3(2):61–68 (in Chinese)

    Google Scholar 

Download references

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Lo, CM., Lee, CF. & Huang, WK. Failure mechanism analysis of rainfall-induced landslide at Pingguang stream in Taiwan: mapping, investigation, and numerical simulation. Environ Earth Sci 75, 1422 (2016). https://doi.org/10.1007/s12665-016-6228-7

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