Reproduction of the chain process of debris flow blocking river at a catchment scale: a numerical study

IF 3.7 2区 工程技术 Q3 ENGINEERING, ENVIRONMENTAL Bulletin of Engineering Geology and the Environment Pub Date : 2024-11-05 DOI:10.1007/s10064-024-03974-6
Wei Liu, Chaojun Ouyang, Yao Tang, Siming He
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Abstract

Debris flow blocking river is a common mountain disaster chain, and however, there is a scarcity of quantitative approaches for assessing this particular disaster chain. To tackle this issue, we have developed a mathematical model using the framework of depth-averaged theory and its associated computational method. The model effectively captures the multistage process of debris flow blocking river at a catchment scale. It encompasses the dynamics of runoff, debris flow, and the river, ensuring the transfer of mass and momentum throughout the entire chain. To facilitate a more intuitive transition between the various secondary induced disasters associated with debris flow blocking river, two additional state variables are introduced. The presented computing method solves the model equations by integrating an HLLC Riemann solver into a second-order accurate finite volume method. To validate the effectiveness of this approach, two laboratory experiments and the 2020 Meilong debris flow blocking river event are simulated, and the obtained results are consistent with the available data. Moreover, this approach is employed to estimate the impact of scission on the chain process of debris flow blocking river. The simulated results showcase whether the transition between the various sub-disasters can successfully transpire under the influence of chain scission. This study can provide a basis for quantitatively assessing the chain process of debris flow blocking river as well as finding the optimization scheme to prevent this disaster chain.

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在集水区范围内再现泥石流阻塞河流的连锁过程:数值研究
泥石流堵塞河道是一种常见的山地灾害链,但目前还缺乏对这种特殊灾害链进行评估的定量方法。针对这一问题,我们利用深度平均理论框架及其相关计算方法建立了一个数学模型。该模型能有效捕捉集水区范围内泥石流堵塞河流的多阶段过程。它涵盖了径流、泥石流和河流的动态变化,确保了整个链条中质量和动量的传递。为便于更直观地转换泥石流阻塞河流所引发的各种次生灾害,模型还引入了两个额外的状态变量。所介绍的计算方法通过将 HLLC 黎曼求解器集成到二阶精确有限体积法中来求解模型方程。为了验证该方法的有效性,模拟了两次实验室实验和 2020 年梅龙镇泥石流堵河事件,结果与现有数据一致。此外,该方法还用于估算泥石流阻塞河道链过程中裂隙的影响。模拟结果表明,在链式裂解的影响下,各次灾害之间能否顺利过渡。该研究可为定量评估泥石流堵塞河道的连锁过程以及寻找预防该灾害连锁的优化方案提供依据。
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来源期刊
Bulletin of Engineering Geology and the Environment
Bulletin of Engineering Geology and the Environment 工程技术-地球科学综合
CiteScore
7.10
自引率
11.90%
发文量
445
审稿时长
4.1 months
期刊介绍: Engineering geology is defined in the statutes of the IAEG as the science devoted to the investigation, study and solution of engineering and environmental problems which may arise as the result of the interaction between geology and the works or activities of man, as well as of the prediction of and development of measures for the prevention or remediation of geological hazards. Engineering geology embraces: • the applications/implications of the geomorphology, structural geology, and hydrogeological conditions of geological formations; • the characterisation of the mineralogical, physico-geomechanical, chemical and hydraulic properties of all earth materials involved in construction, resource recovery and environmental change; • the assessment of the mechanical and hydrological behaviour of soil and rock masses; • the prediction of changes to the above properties with time; • the determination of the parameters to be considered in the stability analysis of engineering works and earth masses.
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