Abstract
Protective barriers provide crucial resistance against the impact of granular flows. However, the adoption of characterized flow depth and velocity values in impact force estimation remains unclear and requires further investigation, especially with consideration of unsteady flow dynamics. Previous practices suggest that the bulk flow velocity with the assumption of uniform distribution should be used in impact force estimation, while we observe the lower part of the flow consistently exhibits lower velocities than the upper part, because granular shear behavior is enhanced within the boundary layer, which strongly affects the flow velocity. As a result, using a bulk velocity in debris impact force estimation may result in that a larger dynamic pressure coefficient must be used in hydrodynamic model. We made a quantitative assessment. For rapid granular flows, the use of a bulk velocity to calculate the dynamic force component could result in underestimation of approximately 10–30%. Therefore, based on the numerical results, it is suggested that the average velocity of the upper 50% of the flow body can be adopted in impact force estimation. If the front flow depth is used to calculate the dynamic impact force component, the results may be approximately 50% lower than the true value, which indicates that the dynamic force on a barrier is likely not controlled by the granular flow front and that a maximum flow depth may be more appropriate if a hydrodynamic model is adopted. In addition, it seems that the strategy we proposed can be used for both of monodisperse and bidisperse granular flow when boulder impact is excluded.
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig1_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig2_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig3_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig4_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig5_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig6_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig7_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig8_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig9_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig10_HTML.png)
![](http://media.springernature.com/m312/springer-static/image/art%3A10.1007%2Fs10064-022-02573-7/MediaObjects/10064_2022_2573_Fig11_HTML.png)
Similar content being viewed by others
References
Ahmadipur A, Qiu T (2018) Impact force to a rigid obstruction from a granular mass sliding down a smooth incline. Acta Geotech 13(6):1433–1450. https://doi.org/10.1007/s11440-018-0727-5
Albaba A, Lambert S, Faug T (2018) Dry granular avalanche impact force on a rigid wall: analytic shock solution versus discrete element simulations. Phys Rev E 97(5–1):052903. https://doi.org/10.1103/PhysRevE.97.052903
Bi YZ, He SM, Du YJ, Sun XP, Li XP (2018) Effects of the configuration of a baffle–avalanche wall system on rock avalanches in Tibet Zhangmu: discrete element analysis. Bull Eng Geol Env 78(4):2267–2282. https://doi.org/10.1007/s10064-018-1284-8
Bryant SK, Take WA, Bowman ET (2015) Observations of grain-scale interactions and simulation of dry granular flows in a large-scale flume. Can Geotech J 52(5):638–655. https://doi.org/10.1139/cgj-2013-0425
Cagnoli B (2021) Stress level effect on mobility of dry granular flows of angular rock fragments. Landslides. https://doi.org/10.1007/s10346-021-01687-5
Cagnoli B, Piersanti A (2015) Grain size and flow volume effects on granular flow mobility in numerical simulations: 3-D discrete element modeling of flows of angular rock fragments. J Geophys Res Solid Earth 120(4):2350–2366. https://doi.org/10.1002/2014jb011729
Cagnoli B, Romano GP (2010) Effect of grain size on mobility of dry granular flows of angular rock fragments: an experimental determination. J Volcanol Geoth Res 193(1–2):18–24. https://doi.org/10.1016/j.jvolgeores.2010.03.003
Cagnoli B, Romano GP (2012a) Effects of flow volume and grain size on mobility of dry granular flows of angular rock fragments: a functional relationship of scaling parameters. J Geophys Res Solid Earth 117(B2). https://doi.org/10.1029/2011JB008926
Cagnoli B, Romano GP (2012b) Granular pressure at the base of dry flows of angular rock fragments as a function of grain size and flow volume: a relationship from laboratory experiments. J Geophys Res Solid Earth 117. https://doi.org/10.1029/2012jb009374
Choi CE, Goodwin GR (2021) Effects of interactions between transient granular flows and macroscopically rough beds and their implications for bulk flow dynamics. 0(ja): null. https://doi.org/10.1139/cgj-2020-0160
Cui P, Zeng C, Lei Y (2015) Experimental analysis on the impact force of viscous debris flow. Earth Surf Proc Land 40(12):1644–1655. https://doi.org/10.1002/esp.3744
DEM solutions (2020) EDEM 2020.1 document. https://www.altair.com/edem/. Accessed 1 Jan 2022
Faug T (2021) Impact force of granular flows on walls normal to the bottom: slow versus fast impact dynamics. Can Geotech J 58(1):114–124. https://doi.org/10.1139/cgj-2019-0399
Faug T, Beguin R, Chanut B (2009) Mean steady granular force on a wall overflowed by free-surface gravity-driven dense flows. Phys Rev E Stat Nonlin Soft Matter Phys 80(2 Pt 1):021305. https://doi.org/10.1103/PhysRevE.80.021305
Goodwin GR, Choi CE (2020) Slit structures: fundamental mechanisms of mechanical trap** of granular flows. Comput Geotech 119. https://doi.org/10.1016/j.compgeo.2019.103376
Goodwin GR, Choi CE (2021) Translational inertial effects and scaling considerations for coarse granular flows impacting landslide-resisting barriers. J Geotech Geoenviron 147(12). https://doi.org/10.1061/(asce)gt.1943-5606.0002661
Ho KKS, Koo RCH, Kwan JSH (2021) Mitigation of debris flows—research and practice in Hong Kong. Environ Eng Geosci 27(2):231–243. https://doi.org/10.2113/EEG-D-20-00009%
Huang D, Li YQ, Song YX, Xu Q, Pei XJ (2019) Insights into the catastrophic **nmo rock avalanche in Maoxian county, China: combined effects of historical earthquakes and landslide amplification. Eng Geol 258. https://doi.org/10.1016/j.enggeo.2019.105158
Huang Y, Zhang B (2020a) Challenges and perspectives in designing engineering structures against debris-flow disaster. Eur J Environ Civ Eng. https://doi.org/10.1080/19648189.2020.1854126
Huang Y, Zhang B (2020b) Review on key issues in centrifuge modeling of flow-structure interaction. Eur J Environ Civ Eng. https://doi.org/10.1080/19648189.2020.1762751
Hübl J, Suda J, Proske D, Kaitna R, Scheidl C (2009) Debris flow impact estimation. Proceedings of the 11th international symposium on water management and hydraulic engineering. Ohrid, Macedonia, pp. 1–5
Hungr O, Leroueil S, Picarelli L (2014) The Varnes classification of landslide types, an update. Landslides 11(2):167–194. https://doi.org/10.1007/s10346-013-0436-y
Jiang Y-J, Fan X-Y, Su L-J, **ao S-y, Sui J, Zhang R-X, Song Y, Shen Z-W (2020) Experimental validation of a new semi-empirical impact force model of the dry granular flow impact against a rigid barrier. Landslides. https://doi.org/10.1007/s10346-020-01555-8
Jiang YJ, Towhata I (2013) Experimental study of dry granular flow and impact behavior against a rigid retaining wall. Rock Mech Rock Eng 46(4):713–729. https://doi.org/10.1007/s00603-012-0293-3
Jóhannesson T, Gauer P, Issler P, Lied K, Hákonardóttir KM (2009) The design of avalanche protection dams: recent practical and theoretical developments. In: B.E.C. Brussels (Editor)
Koo RCH, Kwan JSH, Ng CWW, Lam C, Choi CE, Song D, Pun WK (2016) Velocity attenuation of debris flows and a new momentum-based load model for rigid barriers. Landslides 14(2):617–629. https://doi.org/10.1007/s10346-016-0715-5
Kwan J (2012) Supplementary technical guidance on design of rigid debris-resisting barriers. In: H.K. Geotechnical Engineering Office (Editor), pp. 88
Li X, Zhao J, Soga K (2020) A new physically based impact model for debris flow. Géotechnique 1–12. https://doi.org/10.1680/jgeot.18.P.365
Ng CWW, Choi CE, Goodwin GR (2019) Froude characterization for unsteady single-surge dry granular flows: impact pressure and runup height. Can Geotech J 56(12):1968–1978. https://doi.org/10.1139/cgj-2018-0529
Ng CWW, Choi CE, Koo RCH, Goodwin GR, Song D, Kwan JSH (2018) Dry granular flow interaction with dual-barrier systems. Geotechnique 68(5):386–399. https://doi.org/10.1680/jgeot.16.P.273
Ng CWW, Liu H, Choi CE, Kwan JSH, Pun WK (2021) Impact dynamics of boulder-enriched debris flow on a rigid barrier. J Geotech Geoenviron 147(3). https://doi.org/10.1061/(asce)gt.1943-5606.0002485
Ng CWW, Song D, Choi CE, Liu LHD, Kwan JSH, Koo RCH, Pun WK (2016) Impact mechanisms of granular and viscous flows on rigid and flexible barriers. Can Geotech J 54(2):188–206. https://doi.org/10.1139/cgj-2016-0128
Pudasaini SP, Hutter K, Hsiau S-S, Tai S-C, Wang Y, Katzenbach R (2007) Rapid flow of dry granular materials down inclined chutes im**ing on rigid walls. Phys Fluids 19(5):053302. https://doi.org/10.1063/1.2726885
Pudasaini SP, Kroner C (2008) Shock waves in rapid flows of dense granular materials: theoretical predictions and experimental results. Phys Rev E 78(4):041308. https://doi.org/10.1103/PhysRevE.78.041308
Sanvitale N, Bowman ET (2017) Visualization of dominant stress-transfer mechanisms in experimental debris flows of different particle-size distribution. Can Geotech J 54(2):258–269. https://doi.org/10.1139/cgj-2015-0532
Scheidl C, Chiari M, Kaitna R, Müllegger M, Krawtschuk A, Zimmermann T, Proske D (2013) Analysing debris-flow impact models, Based on a Small Scale Modelling Approach. Surv Geophys 34(1):121–140. https://doi.org/10.1007/s10712-012-9199-6
Song D, Choi CE, Zhou GGD, Kwan JSH, Sze HY (2018) Impulse load characteristics of bouldery debris flow impact. Géotechnique Letters 8(2):111–117. https://doi.org/10.1680/jgele.17.00159
Thouret JC, Antoine S, Magill C, Ollier C (2020) Lahars and debris flows: characteristics and impacts. Earth Sci Rev 201. https://doi.org/10.1016/j.earscirev.2019.103003
Wang W, Yin Y, Zhu S, Wang L, Zhang N, Zhao R (2019) Investigation and numerical modeling of the overloading-induced catastrophic rockslide avalanche in Baige, Tibet, China. Bull Eng Geol Env 79(4):1765–1779. https://doi.org/10.1007/s10064-019-01664-2
Zhang B, Huang Y, Lu P, Li C (2020) Numerical investigation of multiple-impact behavior of granular flow on a rigid barrier. Water 12(11). https://doi.org/10.3390/w12113228
Zhou GGD, Sun QC (2013) Three-dimensional numerical study on flow regimes of dry granular flows by DEM. Powder Technol 239:115–127. https://doi.org/10.1016/j.powtec.2013.01.057
Funding
This work was supported by the National Natural Science Foundation of China (Grant No. 41831291).
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Appendix. DEM contact model and input parameters
Appendix. DEM contact model and input parameters
The DEM is a promising tool because it directly deals with each individual particle (Bi et al. 2018; Cagnoli and Piersanti 2015; Goodwin and Choi 2021; Ng et al. 2019; Wang et al. 2019). In this study, a non-linear contact model, named Hertz-Mindlin (no slip) model, is adopted to calculate the particle contact force including both the normal and tangential component. And a mature software EDEM is used to run simulations (DEM solutions 2020).
The normal force (\({F}_{n}\)) between two contact objects is given as
where \({E}^{*}\), \({R}^{*}\), and \({\lambda }_{n}\) are respectively the equivalent Young’s modulus, equivalent radius, and normal contact overlap. \({E}^{*}\) and \({R}^{*}\) are formulated as follows:
where subscripts i and j, respectively, represent two contact objects (e.g., particle–particle or particle–wall), and \(E\), \(\nu\), and \(R\) are the Young’s modulus, Poisson’s ratio, and radius, respectively.
The tangential force (\({F}_{t}\)) is calculated as
where \({S}_{t}\) is the tangential stiffness, \({\lambda }_{t}\) denotes the tangential overlap, and \({S}_{t}\) is a function of the equivalent shear modulus (\({G}^{*}\)):
A dam** component is respectively applied to the normal and tangential directions:
where \({m}^{*}\) is the equivalent mass given in Eq. (16), \(\gamma\) and \({S}_{n}\) are given in Eqs. (17) and (18), respectively, and \({v}_{n}^{\mathrm{rel}}\) and \({v}_{t}^{\mathrm{rel}}\) are the normal and tangential components of the relative velocity, respectively.
where \({m}_{i}\) and \({m}_{j}\) are the mass of the interacting elements and e is the restitution coefficient.
The magnitude of \({F}_{t}\) is limited by \({\mu }_{s}{F}_{n}\), where \({\mu }_{s}\) is the Coulomb’s friction coefficient of the particles. A torque is also applied to the contact surfaces to account for the effect of rolling friction:
where \({\mu }_{r}\) is the coefficient of rolling friction, \({d}_{i}\) is the distance between the contact point and center of mass, and \({\widehat{\omega }}_{i}\) is the unit angular velocity vector of particle i at the contact point.
Detailed calibration process could be accessed in Supplementary Material S1. And DEM input parameters are presented in Table 4.
Rights and permissions
About this article
Cite this article
Zhang, B., Huang, Y. Effect of unsteady flow dynamics on the impact of monodisperse and bidisperse granular flow. Bull Eng Geol Environ 81, 77 (2022). https://doi.org/10.1007/s10064-022-02573-7
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s10064-022-02573-7