China Geological Environment Monitoring Institute, China Geological Disaster Prevention Engineering Industry AssociationHost
2023 Vol. 34, No. 1
Article Contents

LU Ming, LIU Jinfeng, SUN Hao, ZHAO Wanyu. Process and characteristics of “7·5” Huangniba gully debris flow in Muli County of Sichuan Province and and prevention suggestions[J]. The Chinese Journal of Geological Hazard and Control, 2023, 34(1): 102-109. doi: 10.16031/j.cnki.issn.1003-8035.202204005
Citation: LU Ming, LIU Jinfeng, SUN Hao, ZHAO Wanyu. Process and characteristics of “7·5” Huangniba gully debris flow in Muli County of Sichuan Province and and prevention suggestions[J]. The Chinese Journal of Geological Hazard and Control, 2023, 34(1): 102-109. doi: 10.16031/j.cnki.issn.1003-8035.202204005

Process and characteristics of “7·5” Huangniba gully debris flow in Muli County of Sichuan Province and and prevention suggestions

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  • On July 5, 2021, debris flow disasters broke out in the seven branch ditches of Xiangjiao gully under the condition of consecutive days of rain. Due to the efficient operation of the mass prediction and disaster prevention system, 20 households with 118 casualties and 14.21 million yuan of economic losses were avoided. Huangniba gully was one of the tributaries of debris flow outbreaks, with a drainage are of 14.47 km2. The scale of the debris flow flushed out objects was 12×104 m3, and several houses were damaged. During the "3·28" forest fire in 2020, the surface vegetation in Huangniba gully was severely burned, which led to dramatic changes in its debris flow disaster-pregnant environment. In the background of few debris flow activities in Huangniba gully, debris flow disasters broke out several times in 2020 and 2021. Through field investigation, it was concluded that the contradiction between the drastically changed disaster-pregnancy environment of the debris flow and the old layout of the villages was the key reason for the serious disaster in Xiapingzi Village. The entire disaster process is as follows: after the debris flow blocked the internal ditches of the village, the outflowing mountain torrents were not able to be discharged smoothly, causing a large area of flooding, which caused doubled the losses to the village. The primary treatment measures were to build a drainage channel connecting the ditch mouth and the main river and re-plan the layout of the village, so that the debris flow can be smoothly discharged into the main river and the village buildings were kept away from the direct range of the debris flow. Finally, the successful practice of the mass people monitoring and prevention system was analyzed, and the experience was summarized for reference.

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  • [1] 暴雨致凉山木里项脚沟流域7条支沟齐发泥石流1246人安全转移[N].四川省应急管理厅官网之新闻动态[2021-07-08].

    Google Scholar

    Heavy rain caused debris flows in 7 branch ditches of the Xiangjiao Valley in Liangshan[N].The official website of the Sichuan Provincial Department of Emergency Management[2021-07-08].

    Google Scholar

    [2] WONDZELL S M,KING J G. Postfire erosional processes in the Pacific Northwest and Rocky Mountain regions[J]. Forest Ecology and Management,2003,178(1/2):75 − 87.

    Google Scholar

    [3] 殷万清,曹希超,胡卸文,等. 木里县项脚沟火后泥石流发育特征及应急处置对策[J]. 地质灾害与环境保护,2021,32(1):12 − 17. [YIN Wanqing,CAO Xichao,HU Xiewen,etal. Development characteristics of post-fire debris flow and emergency response measures in Xiangjiao township,Muli[J]. Journal of Geological Hazards and Environment Preservation,2021,32(1):12 − 17. (in Chinese with English abstract) doi: 10.3969/j.issn.1006-4362.2021.01.002

    CrossRef Google Scholar

    [4] 李潇. 木里成功避险群发性泥石流灾害[N]. 凉山新闻网讯, 2021-07-06

    Google Scholar

    LI Xiao. Muli successfully avoided mass debris flow disasters[N]. Liangshan News Network News, 2021-07-06. (in Chinese)

    Google Scholar

    [5] PROCHASKA A B,SANTI P M,HIGGINS J D. Debris basin and deflection berm design for fire-related debris-flow mitigation[J]. Environmental and Engineering Geoscience,2008,14(4):297 − 313. doi: 10.2113/gseegeosci.14.4.297

    CrossRef Google Scholar

    [6] CANNON S H,GARTNER J E,WILSON R C,et al. Storm rainfall conditions for floods and debris flows from recently burned areas in southwestern Colorado and southern California[J]. Geomorphology,2008,96(3/4):250 − 269.

    Google Scholar

    [7] 崔鹏,杨坤,陈杰. 前期降雨对泥石流形成的贡献:以蒋家沟泥石流形成为例[J]. 中国水土保持科学,2003,1(1):11 − 15. [CUI Peng,YANG Kun,CHEN Jie. Relationship between occurrence of debris flow and antecedent precipitation:Taking the Jiangjia gully as an example[J]. Science of Soil and Water Conservation,2003,1(1):11 − 15. (in Chinese with English abstract) doi: 10.3969/j.issn.1672-3007.2003.01.005

    CrossRef Google Scholar

    [8] 陈景武. 云南东川蒋家沟泥石流暴发与暴雨关系的初步分析[M]. 北京: 科学出版社, 1985

    Google Scholar

    CHEN Jingwu. Preliminary analysis on the relationship between Jiangjiagou debris flow and heavy rain in Dongchuan, Yunnan[M]. Beijing: Science Press, 1985. (in Chinese)

    Google Scholar

    [9] 薛宁波, 马清文, 王成华. 地质灾害易发山区群测群防体系与突发性灾害预警[J]. 中国水土保持科学, 2008, 6(增刊 1): 12 − 15

    Google Scholar

    XUE Ningbo, MA Qingwen, WANG Chenghua. System of operated by mass people and warning of sudden outbrust hazards in geological hazards mountainous area[J]. Science of Soil and Water Conservation, 2008, 6(Sup 1): 12 − 15. (in Chinese with English abstract)

    Google Scholar

    [10] 游勇. 泥石流排导槽水力最佳断面[J]. 山地学报,1999,17(3):255 − 258. [YOU Yong. Optimal hydraulic condition of debris flow drainage canal[J]. Journal of Mountain Research,1999,17(3):255 − 258. (in Chinese with English abstract) doi: 10.3969/j.issn.1008-2786.1999.03.012

    CrossRef Google Scholar

    [11] 游勇, 柳金峰, 欧国强. 泥石流常用排导槽水力条件的比较[J]. 岩石力学与工程学报, 2006, 25(增刊1): 2820 − 2825

    Google Scholar

    YOU Yong, LIU Jinfeng, OU Guoqiang. Comparison of hydraulic conditions among usual debris flow drainage canal[J]. Chinese Journal of Rock Mechanics and Engineering, 2006, 25(Sup 1): 2820 − 2825. (in Chinese with English abstract)

    Google Scholar

    [12] YOU Yong,LIU Jinfeng,CHEN Xingzhang,et al. Debris flow formation conditions and optimal characteristics of drainage canal following Wenchuan earthquake[J]. Environmental Earth Sciences,2012,65(4):1005 − 1012. doi: 10.1007/s12665-011-1024-x

    CrossRef Google Scholar

    [13] 邸雪颖,陶玉柱. 火后泥石流研究进展[J]. 应用生态学报,2013,24(8):2383 − 2392. [DI Xueying,TAO Yuzhu. Research progress in post-fire debris flow[J]. Chinese Journal of Applied Ecology,2013,24(8):2383 − 2392. (in Chinese with English abstract) doi: 10.13287/j.1001-9332.2013.0396

    CrossRef Google Scholar

    [14] 庞伟军,常刚,苟海瑞,等. 甘肃肃南县长达坂沟泥石流成灾机理和防治措施建议[J]. 中国地质灾害与防治学报,2018,29(2):29 − 34. [PANG Weijun,CHANG Gang,GOU Hairui,et al. Disaster mechanism of debris flow of Changdaban gully in Sunan County of Gansu Province and suggstions for its prevention[J]. The Chinese Journal of Geological Hazard and Control,2018,29(2):29 − 34. (in Chinese with English abstract) doi: 10.16031/j.cnki.issn.1003-8035.2018.02.05

    CrossRef Google Scholar

    [15] 文强,胡卸文,刘波,等. 四川丹巴梅龙沟“6·17”泥石流成灾机理分析[J]. 中国地质灾害与防治学报,2022,33(3):23 − 30. [WEN Qiang,HU Xiewen,LIU Bo,et al. Analysis on the mechanism of debris flow in Meilong valley in Danba County on June 17,2020[J]. The Chinese Journal of Geological Hazard and Control,2022,33(3):23 − 30. (in Chinese with English abstract) doi: 10.16031/j.cnki.issn.1003-8035.2022.03-03

    CrossRef Google Scholar

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