Citation: | ZHANG Xianzheng, TIE Yongbo, NING Zhijie, YANG Chang, LI Zongliang, LI Minghui, LIANG Jingtao, LU Jiayan, LU Tuo, LI Guanghui, LI Guo, XIANG Binglin. Characteristics and activity analysis of the catastrophic “6•26” debris flow in the Banzi catchment, Wenchuan County of Sichuan Province[J]. Hydrogeology & Engineering Geology, 2023, 50(5): 134-145. doi: 10.16030/j.cnki.issn.1000-3665.202307003 |
On 26 June 2023, a catastrophic debris flow occurred in the Banzi Catchment in Wenchuan county of Sichuan province. This debris flow event is a viscous debris flow triggered by short duration heavy rainfall. The volume of debris which transported out of the catchment by debris flow is more than 8.3×105 m3, and the debris flow blocked the Minjiang River. The river blockage formed a barrier lake with an area of about 0.4 km2. To reveal the formation mechanism of the occurrence of the extremely large debris flow events 15 years after the Wenchuan earthquake, This paper adopts a comprehensive method of field investigation, image interpretation, topographic superposition and calculation of forced vortex. This paper also analyzes the formation mechanism of debris flow and the characteristics of river blocking. Based on the results, this paper gives some suggestions of investigation and prevention of debris flow in the Banzi catchment. The research results show that (1) the triggering rainfall is characterized by short duration and high intensity. The main initiation positions are in the channel. The main debris supply is from the debris deposition along the channel. (2) The peak discharge of debris flow is as high as 755.5 m3/s, which is the main cause of river blockage. (3) Since the Wenchuan earthquake, the debris flow activity of the Banzi Catchment has the characteristics of lag and long-term because of the coupled transport of debris on the slope and along the channel. (4) The volume of the debris source which can be eroded along the channel should be paid more attention in subsequent investigation and prevention. The research results are helpful in better understanding of the activity evolution of the post-seismic debris flow. They can also provide scientific references for the prevention of the post-seismic debris flow..
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Debris fan of the Banzi catchment (taken on 27 June, 2023)
Geological overview of the study area
Loss characteristic of debris flow in the Banzi catchment (taken on 29 June, 2023)
Definition of the geomorphometric parameters for the forced vortex equation
Comparison of images before and after debris flow
Initiation positions in the No. 4 branch channel of Banzi catchment and the characteristic of erosion at the intersection of the main channel and the No. 4 branch channel
Distribution of debris source in the Banzi catchment
Statistical map of elevation and debris source on the slope in the Banzi catchment
Statistical map of slope and the debris source on the slope in the Banzi catchment
Sampling particle size distribution in the debris deposition area
Characteristics of the trigging rainfall in the study area
Distribution map of the erosion and deposition along the channel
Shape and the profiles of debris fans
Distribution of profiles used for the calculation of forced vortex
Photography showing the largest blocks deposited on the fan exceeded a diameter of 2.5 m