Debris flow simulation 2D (DFS 2D): Numerical modelling of debris flows and calibration of friction parameters

被引:18
作者
Abrahama, Minu Treesa [1 ]
Satyama, Neelima [1 ]
Pradhan, Biswajeet [2 ,3 ,4 ]
Tian, Hongling [5 ]
机构
[1] Indian Inst Technol Indore, Dept Civil Engn, Indore, India
[2] Univ Technol Sydney, Sch Civil & Environm Engn, Fac Engn & Informat Technol, Ctr Adv Modelling & Geospatial Informat Syst CAMG, Sydney, NSW, Australia
[3] King Abdulaziz Univ, Ctr Excellence Climate Change Res, Jeddah, Saudi Arabia
[4] Univ Kebangsaan Malaysia, Inst Climate Change, Earth Observat Ctr, Bangi, Malaysia
[5] Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Surface Proc, Chengdu, Peoples R China
关键词
Debris flows; Numerical model; Rheology; Debris flow simulation 2D (DFS 2D); RUNOUT ANALYSIS; ENTRAINMENT; MOTION; MUD; LANDSLIDES; TRANSITION; MOBILITY;
D O I
10.1016/j.jrmge.2022.01.004
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Debris flows are rapid mass movements with a mixture of rock, soil and water. High-intensity rainfall events have triggered multiple debris flows around the globe, making it an important concern from the disaster management perspective. This study presents a numerical model called debris flow simulation 2D (DFS 2D) and applicability of the proposed model is investigated through the values of the model parameters used for the reproduction of an occurred debris flow at Yindongzi gully in China on 13 August 2010. The model can be used to simulate debris flows using three different rheologies and has a user-friendly interface for providing the inputs. Using DFS 2D, flow parameters can be estimated with respect to space and time. The values of the flow resistance parameters of model, dry-Coulomb and turbulent friction, were calibrated through the back analysis and the values obtained are 0.1 and 1000 m/s(2), respectively. Two new methods of calibration are proposed in this study, considering the cross-sectional area of flow and topographical changes induced by the debris flow. The proposed methods of calibration provide an effective solution to the cumulative errors induced by coarse-resolution digital elevation models (DEMs) in numerical modelling of debris flows. The statistical indices such as Willmott's index of agreement, mean-absolute-error, and normalized-root-mean-square-error of the calibrated model are 0.5, 1.02 and 1.44, respectively. The comparison between simulated and observed values of topographic changes indicates that DFS 2D provides satisfactory results and can be used for dynamic modelling of debris flows. (C) 2022 Institute of Rock and Soil Mechanics, Chinese Academy of Sciences. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
引用
收藏
页码:1747 / 1760
页数:14
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