Abstract
Bed entrainment changes the rheology of the sliding mass and the topography of the sliding surface, finally influencing the propagation of flow-like landslides. In previous studies, both empirical methods and physically based methods have been used to simulate bed entrainment. However, the influences of bed entrainment on the rheology and topography of flow-like landslides were not deeply explored. In this paper, the physically based model proposed by Fraccarollo and Capart (J Fluid Mech 461:183–228, 2002) is adopted to calculate the bed entrainment rate, and a new method is proposed to consider the rheology change associated with bed entrainment in flow-like landslides. The new rheology change method and the Fraccarollo and Capart model are incorporated into a quasi-3D finite difference code to analyze an ideal case and two typical flow-like landslides. The two real landslides are the Dabaozi landslide and the Dagou landslide in the Chinese Loess Plateau. They represent two different bed entrainment scenarios: the erodible mass is relatively thick in the Dabaozi landslide, while that of the Dagou landslide is relatively thin. The results show that both the topography and rheology changes have a significant influence on the propagation of flow-like landslides: (1) the rheology change mainly influences the run-out distance of a landslide, while the topography change mainly impacts the lateral spreading; (2) entraining soft materials can significantly increase the run-out distance of a flow-like landslide; (3) the topography change can obviously constrain the lateral spreading of those landslides when the erodible mass is relatively thick. In addition, it shows that the rheology change and topography change influence each other in the propagation of a flow-like landslide, and the proposed rheology change method in this paper can properly reflect this interactive process.
Similar content being viewed by others
References
Blanc T, Pastor M, Drempetic MSV, Haddad B (2011) Depth integrated modelling of fast landslide propagation. Eur J Environ Civil Eng 15:51–72
Breien H, De Blasio FV, Elverhøi A, Høeg K (2008) Erosion and morphology of a debris flow caused by a glacial lake outburst flood, Western Norway. Landslides 5:271–280
Chen H, Crosta GB, Lee CF (2006) Erosional effects on runout of fast landslides, debris flows and avalanches: a numerical investigation. Géotechnique 56:305–322
Crosta GB, Imposimato S, Roddeman D (2009) Numerical modelling of entrainment/deposition in rock and debris-avalanches. Eng Geol 109:135–145
Crosta GB, De Blasio FV, De Caro M, Volpi G, Imposimato S, Roddeman D (2017) Modes of propagation and deposition of granular flows onto an erodible substrate: experimental, analytical, and numerical study. Landslides 14:47–68
Cuomo S, Pastor M, Cascini L, Castorino GC (2014) Interplay of rheology and entrainment in debris avalanches: a numerical study. Can Geotech J 51:1318–1330
Cuomo S, Pastor M, Capobianco V, Cascini L (2016) Modelling the space–time evolution of bed entrainment for flow-like landslides. Eng Geol 212:10–20
Dai ZL, Huang Y, Cheng HL, Xu Q (2014) 3D numerical modeling using smoothed particle hydrodynamics of flow-like landslide propagation triggered by the 2008 Wenchuan earthquake. Eng Geol 180:21–33
Egashira S, Honda N, Itoh T (2001) Experimental study on the entrainment of bed material into debris flow. Phys Chem Earth C Sol Terr Planet Sci 26:645–650
Evans SG, Tutubalina OV, Drobyshev VN et al (2009a) Catastrophic detachment and high-velocity long-runout flow of Kolka Glacier, Caucasus Mountains, Russia in 2002. Geomorphology 105:314–321
Evans SG, Roberts NJ, Ischuk A, Delaney KB, Morozova GS, Tutubalina O (2009b) Landslides triggered by the 1949 Khait earthquake, Tajikistan, and associated loss of life. Eng Geol 109:195–212
Fraccarollo L, Capart H (2002) Riemann wave description of erosional dam-break flows. J Fluid Mech 461:183–228
Haque U, Blum P, da Silva PF et al (2016) Fatal landslides in Europe. Landslides 13:1545–1554
Hou XK, Vanapalli SK, Li TL (2018) Water infiltration characteristics in loess associated with irrigation activities and its influence on the slope stability in Heifangtai loess highland, China. Eng Geol 234:27–37
Huang Y, Cheng HL, Dai ZL et al (2015) SPH-based numerical simulation of catastrophic debris flows after the 2008 Wenchuan earthquake. Bull Eng Geol Environ 74:1137–1151
Hungr O, Evans SG (2004) Entrainment of debris in rock avalanches: an analysis of a long run-out mechanism. Geol Soc Am Bull 116:1240–1252
Hungr O, Leroueil S, Picarelli L (2014) The Varnes classification of landslide types, an update. Landslides 11:167–194
Iverson RM (1997) The physics of debris flows. Rev Geophys 35:245–296
Iverson RM (2000) Landslide triggering by rain infiltration. Water Resour Res 36:1897–1910
Iverson RM, Ouyang CJ (2015) Entrainment of bed material by Earth-surface mass flows: review and reformulation of depth-integrated theory. Rev Geophys 53:27–58
Iverson RM, Reid ME, Logan M, LaHusen RG, Godt JW, Griswold JP (2011) Positive feedback and momentum growth during debris-flow entrainment of wet bed sediment. Nat Geosci 4:116–121
Iverson RM, George DL, Allstadt K et al (2015) Landslide mobility and hazards: implications of the 2014 Oso disaster. Earth Planet Sci Lett 412:197–208
King JP (1996) The Tsing Shan debris flow. Special Project Report SPR6/96. Geotechnical Engineering Office, Hong Kong
Mangeney A (2011) Geomorphology: landslide boost from entrainment. Nat Geosci 4:77–78
Mangeney A, Roche O, Hungr O, Mangold N, Faccanoni G, Lucas A (2010) Erosion and mobility in granular collapse over sloping beds. J Geophys Res 115:F03040
McDougall S, Hungr O (2005) Dynamic modelling of entrainment in rapid landslides. Can Geotech J 42:1437–1448
Medina V, Hürlimann M, Bateman A (2008) Application of FLATModel, a 2D finite volume code, to debris flows in the northeastern part of the Iberian Peninsula. Landslides 5:127–142
Meyer NK, Dyrrdal AV, Frauenfelder R, Etzelmüller B, Nadim F (2012) Hydrometeorological threshold conditions for debris flow initiation in Norway. Nat Hazards Earth Syst Sci 12:3059–3073
Okada Y, Ochiai H, Kurokawa U, Ogawa Y, Asano S (2008) A channelised long run-out debris slide triggered by the Noto Hanto Earthquake in 2007, Japan. Landslides 5:235–239
Ouyang CJ, He SM, Tang C (2015) Numerical analysis of dynamics of debris flow over erodible beds in Wenchuan earthquake-induced area. Eng Geol 194:62–72
Pastor M, Haddad B, Sorbino G, Cuomo S, Drempetic V (2009) A depth-integrated, coupled SPH model for flow-like landslides and related phenomena. Int J Numer Anal Methods Geomech 33:143–172
Peng JB, Wang GH, Wang QY, Zhang FY (2017) Shear wave velocity imaging of landslide debris deposited on an erodible bed and possible movement mechanism for a loess landslide in Jingyang, Xi’an, China. Landslides 14:1503–1512
Peng XY, Yu PC, Zhang YB, Chen GQ (2018) Applying modified discontinuous deformation analysis to assess the dynamic response of sites containing discontinuities. Eng Geol 246:349–360
Pirulli M, Pastor M (2012) Numerical study on the entrainment of bed material into rapid landslides. Géotechnique 62:959–972
Pitman EB, Nichita CC, Patra AK, Bauer AC, Bursik M, Weber A (2003) A model of granular flows over an erodible surface. Discret Contin Dyn Syst B 3:589–599
Rossano S, Mastrolorenzo G, De Natale G, Pingue F (1996) Computer simulation of pyroclastic flow movement: an inverse approach. Geophys Res Lett 23:3779–3782
Sassa K, Nagai O, Solidum R, Yamazaki Y, Ohta H (2010) An integrated model simulating the initiation and motion of earthquake and rain induced rapid landslides and its application to the 2006 Leyte landslide. Landslides 7:219–236
Savage SB, Hutter K (1989) The motion of a finite mass of granular material down a rough incline. J Fluid Mech 199:177–215
Shen W, Zhai ZH, Li TL, Zhao QL, Wang FW (2016) Simulation of propagation process for the Dabaozi rapid long run-out loess landslide in the south bank of the Jing River, Shaanxi Province. J Eng Geol 24:1309–1317 (in Chinese with English abstract)
Shen W, Li TL, Li P, Guo J (2018) A modified finite difference model for the modeling of flowslides. Landslides 15:1577–1593
Sovilla B, Burlando P, Bartelt P (2006) Field experiments and numerical modeling of mass entrainment in snow avalanches. J Geophys Res 111:F03007. https://doi.org/10.1029/2005JF000391
Takahashi T, Kuang SF (1986) Formation of debris flow on varied slope bed. Annual of Disaster Prevention Research Institute, Kyoto University, 29B-2, pp 343–359
Wang GH, Sassa K (2003) Pore-pressure generation and movement of rainfall-induced landslides: effects of grain size and fine-particle content. Eng Geol 69:109–125
Yin YP, Zheng WM, Li XC, Sun P, Li B (2011) Catastrophic landslides associated with the M8.0 Wenchuan earthquake. Bull Eng Geol Environ 70:15–32
Zhang X, Krabbenhoft K, Sheng DC, Li WC (2015) Numerical simulation of a flow-like landslide using the particle finite element method. Comput Mech 55:167–177
Acknowledgements
The authors acknowledge the funding received from the National Key R&D Program of China (2017YFC1501302), the China Scholarship Council (CSC)–University of Bologna Joint Scholarship (file no. 201806560011), and the National Natural Science Foundation of China (no. 41877242), which supported this study.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Shen, W., Li, T., Li, P. et al. The influence of the bed entrainment-induced rheology and topography changes on the propagation of flow-like landslides: a numerical investigation. Bull Eng Geol Environ 78, 4771–4785 (2019). https://doi.org/10.1007/s10064-018-01447-1
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s10064-018-01447-1