Constructing Rainfall Threshold for Debris Flows of a Defined Hazardous Magnitude

Author:

Li Yajun123,Wang Mengyu123,Ma Fukang123,Zhang Jun123,Li Guowei123,Meng Xingmin123ORCID,Chen Guan123,Yue Dongxia4,Guo Fuyun5,Zhao Yan123ORCID

Affiliation:

1. School of Earth Sciences, Lanzhou University, Lanzhou 730000, China

2. Gansu Tech Innovation Centre for Environmental Geology and Geohazard Prevention, Lanzhou 730000, China

3. International Science & Technology Cooperation Base for Geohazards Monitoring, Warning & Prevention, Lanzhou 730000, China

4. MOE Key Laboratory of Western China’s Environment Systems, College of Earth and Environment Science, Lanzhou University, Lanzhou 730000, China

5. Geological Environment Monitoring Institute of Gansu Province, Lanzhou 730050, China

Abstract

Debris flow can cause damage only when its discharge exceeds the drainage capacity of the prevention engineering. At present, most rainfall thresholds for debris flows mainly focus on the initiation of debris flow and do not adequately consider the magnitude and drainage measures of debris flows. These thresholds are likely to initiate numerous warnings that may not be related to hazardous processes. This study proposes a method for calculating the rainfall threshold that is related to a defined level of debris flow magnitude, over which certain damage may be caused. This method is constructed by using the transient rainfall infiltration analysis slope stability model (TRIGRS) and the fluid dynamics process simulation model (MassFlow). We first use the TRIGRS model to analyze slope stability in the study area and obtain the distribution of unstable slopes under different rainfall conditions. Afterward, the MassFlow model is employed to simulate the movement process of unstable slope units and to predict the depositional processes at the mouth of the catchment. Lastly a rainfall threshold is constructed by statistically analyzing the rainfall conditions that cause debris flows flushing out of the given drainage ditch. This method is useful to predict debris flow events of a hazardous magnitude, especially for areas with limited historical observational data.

Funder

Key Technology Research and Development Program of the Ministry of Gansu Province, China

National Natural Science Foundation of China

Fundamental Research Funds for the Central Universities

Publisher

MDPI AG

Reference69 articles.

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2. Jakob, M., Hungr, O., and Jakob, D.M. (2005). Debris-Flow Hazards and Related Phenomena, Springer.

3. Xu, H. (2009). Environmental Geology, Geology Press-Beijing.

4. Wahab, M.K.A., Zainol, M.R.R.M.A., Ikhsan, J., Zawawi, M.H., Abas, M.A., Mohamed Noor, N., Abdul Razak, N., and Sholichin, M. (2023). Assessment of Debris Flow Impact Based on Experimental Analysis along a Deposition Area. Sustainability, 15.

5. Rainfall thresholds for the initiation of landslides in central and southern Europe;Guzzetti;Meteorol. Atmos. Phys.,2007

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