Tie Yongbo, Ruan Chongfei, Yang Shun, et al. Characteristics and Mechanism of Geological Disasters Induced by “5·25” Rainstorm in Gongshan County of Yunnan Province[J]. Bulletin of Soiland Water Conservation, 2021, 41(2): 10-15.
DOI:
Tie Yongbo, Ruan Chongfei, Yang Shun, et al. Characteristics and Mechanism of Geological Disasters Induced by “5·25” Rainstorm in Gongshan County of Yunnan Province[J]. Bulletin of Soiland Water Conservation, 2021, 41(2): 10-15. DOI: 10.13961/j.cnki.stbctb.2021.02.002.
Characteristics and Mechanism of Geological Disasters Induced by “5·25” Rainstorm in Gongshan County of Yunnan Province
[Objective] The development and distribution characteristics
formation mechanism and development trend of geological hazards induced by "5·25" heavy rainfall on May 25
2020 in Gongshan County
Yunnan Province were studied
in order to provide scientific basis for geological hazards prevention and mitigation planning in this area.[Methods] Based on the first-hand data of the post-disaster emergency survey and the systematic collection of regional geological and rainfall data
the hazard process was analyzed and studied.[Results] The concurrence geological hazards in Gongshan County were mainly small landslides and debris flows
which were mainly distributed along the road and on both sides of Nujiang River. Most of the landslides were shallow surface
and debris flows were mainly initiated by landslide. The geological hazards showed typical characteristics of high-location
long-range and chain type disasters. It was very common for landslide or collapse to enter the channel and turn into debris flow.[Conclusion] In the investigation and assessment of geological hazards in Gongshan County
it is necessary to fully consider the investigation of high-location geological hazards
and scientifically evaluate the chain effect caused by geological hazards and the scope of the affected areas; due to the high vegetation coverage in the territory
debris flow will carry a large number of driftwood to rush out
which is easy to form blockage in narrow gully or at the bridge and culvert at the mouth of the gully
which will enlarge the instantaneous volume of debris flow. It is suggested to carry out large-scale geological hazard risk investigation and evaluation in Gongshan County
and organically integrate the evaluation results with the land spatial planning
so as to control the geological hazard risk from the source
and improve the protection standard of debris flow control engineering in the back mountain of the town.
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references
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Characteristics and Countermeasures of Nuozha Debris-flow in Huili County,Sichuan Province
Formation Mechanism of Rainstorm-induced Debris Flow in Yushu State of Qinghai Province——A Case Study on Debris Flow of Lalong Gully in Chengduo County
Landslide Formation Mechanism at Dingdong Primary School of Guiding County in Guizhou Province
Development Characteristics and Formation Mechanism of Geological Disasters in Jian'ou City, Fujian Province
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Related Institution
CAS Key Laboratory of Mountain Hazards and Surface Processes,Institute of Mountain Hazards and Environment, CAS,,Sichan
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