1. 中国地质调查局 成都地质调查中心,四川,成都,610081
2. 云南地质工程勘察设计研究院,云南,昆明,650041
3. 中国地质科学院 探矿工艺研究所,四川,成都,611734
4. 中国气象局 成都高原气象研究所,四川,成都,610072
5. 云南省地质环境监测院,云南,昆明,650200
6. 甘肃地质灾害防治工程勘查设计院,甘肃,兰州,730050
纸质出版:2021
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铁永波, 阮崇飞, 杨顺, 等. 云南省贡山县“5·25”暴雨诱发地质灾害的特征与形成机制[J]. 水土保持通报, 2021,41(2):10-15.
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.
铁永波, 阮崇飞, 杨顺, 等. 云南省贡山县“5·25”暴雨诱发地质灾害的特征与形成机制[J]. 水土保持通报, 2021,41(2):10-15. DOI: 10.13961/j.cnki.stbctb.2021.02.002.
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.
[目的] 查明2020年5月25日云南省贡山县“5·25”强降雨诱发地质灾害的发育分布特征、形成机制及发展趋势,为该县地质灾害防灾减灾规划提供科学依据。[方法] 基于灾后应急排查一手资料,在系统收集区域地质及降雨资料的基础上,对其灾害过程开展了深入分析与研究。[结果] 贡山县“5·25”群发性地质灾害以滑坡和泥石流为主,规模多为小型,主要沿怒江两岸公路沿线分布,滑坡多以浅表层为主,泥石流多以土力类泥石流启动模式为主,地质灾害表现出典型的高位远程及链式灾害特征,滑坡或崩塌发生后进入沟道转化为泥石流的现象极为普遍。[结论] 贡山县地质灾害调查评价中需充分考虑高位地质灾害的排查,同时科学评估地质灾害引发的链式效应及其影响区范围;由于境内植被覆盖率较高,泥石流发生后会携带大量的漂木冲出,在沟道狭窄处或沟口桥涵处易形成堵塞,对泥石流的瞬时流量会起到放大作用而翻越沟道造成灾害。泥石流防治工程设计中要充分考虑堵塞系数取值的合理性。建议对贡山县城开展大比例尺地质灾害风险调查与评价,将评价结果与国土空间规划有机融合,从源头上对地质灾害风险进行管控,同时提高县城后山已有泥石流防治工程设防等级和标准。
[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.
Lopez J L, Perez D, Garcia R. Hydrologic and geomorphologic evaluation of the 1999 debris flow event in Venezuela[C]//3 rd International Conference on Debris flow Hazard Mitigation:Mechanics, Prediction, and Assessment. Davos, Switzerland, 2003:13-15.
郭富赟,孟兴民,黎志恒,等.天水市"7·25"群发性地质灾害特征及成因[J].山地学报,2015,33(1):100-107.
黄润秋,李为乐."5·12"汶川大地震触发地质灾害的发育分布规律研究[J].岩石力学与工程学报,2009,27(12):2585-2592.
阮锡章,洪维群,陈延云,郑文君,等.一次群发性地质灾害气象成因分析[C]//第34届中国气象学会年会.2017:694-698.
简涛.云南省昌宁县"9·16"群发性地质灾害成因分析与防治对策[J]工程技术(引文版),2016,7(1):69-71.
铁永波,徐勇,张勇,等.南方山地丘陵区地质灾害调查工程主要进展与成果[J].中国地质调查,2020,7(2):1-12.
Ni Huayong, Zheng Wanmo, Li Zongliang, et al. Recent catastrophic debris flows in Luding county, SW China:Geological hazards, rainfall analysis and dynamic characteristics[J]. Natural Hazards, 2010,55(4):523-542.
铁永波,唐川,倪化勇.群发性泥石流的危害效应及防范探讨[J].山地学报,2010.28(6):753-757.
孔艳,王保云,杨昆,等.云南省泥石流灾害时空分布规律及典型区域孕灾特点分析[J].云南师范大学学报(自然科学版),2018.38(6):55-63.
唐川.云南怒江流域泥石流敏感性空间分析[J].地理研究,2005,24(2):178-185.
孔艳,王保云,王乃强,等.滇西高山峡谷区泥石流危险性评价:以怒江傈僳族自治州为例[J].云南师范大学学报(自然科学版),2019.39(3):63-70.
徐慧娟.怒江流域高山峡谷区泥石流活动规律及成灾驱动力研究[D].云南昆明:云南大学,2016.
郑师谊,张绪教,杨艳,等.层次分析法在滇西怒江河谷潞江盆地段崩塌与滑坡地质灾害危险性评价中的应用[J].地质通报,2012.31(Z1):356-365.
李益敏,杨蕾,魏苏杭.基于小流域单元的怒江州泥石流易发性评价[J].长江流域资源与环境,2019,28(10):2419-2428.
吕立群,王兆印,徐梦珍,等.怒江泥石流扇地貌特征与扇体堵江机理研究[J].水利学报,2016.47(10):1245-1252.
周东平.云南怒江贡山流域泥石流预警模型研究[D].河北石家庄:石家庄经济学院,2015.
苏鹏程,韦方强,谢涛.云南贡山8·18特大泥石流成因及其对矿产资源开发的危害[J].资源科学,2012.34(7):1248-1256.
张杰,李世凯,甘云兰,等.云南贡山8·18特大泥石流灾害调查分析与启示[J].工程地质学报,2015.23(3):373-382.
程德方.怒江六库-贡山河段泥石流初探[J].水土保持通报,1985,5(1):55-56.
Tie Yongbo Xu Ruge, Ba Renji. The formation of runoff-generated debris flow in Southwestern of China:Take Gangou as an example[J]. Environmental Earth Sciences, 2014,72(5):1479-1490.
铁永波,徐如阁,刘洪,等.西昌市泸山地区典型火后泥石流特征及成因机制研究:以响水沟左岸3
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支沟为例[J].中国地质调查,2020,7(3):82-88.
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