中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Field observation of debris-flow activities in the initiation area of the Jiangjia Gully, Yunnan Province, China

文献类型:期刊论文

作者YANG Hong-juan1; ZHANG Shao-jie1; HU Kai-heng1; WEI Fang-qiang2; WANG Kai1; LIU Shuang1
刊名JOURNAL OF MOUNTAIN SCIENCE
出版日期2022-06-01
卷号19期号:6页码:1602-1617
ISSN号1672-6316
关键词Debris flow Field observation Initiation mechanism Rainfall threshold Jiangjia gully
DOI10.1007/s11629-021-7292-3
通讯作者ZHANG Shao-jie(sj-zhang@imde.ac.cn)
英文摘要The Jiangjia Gully, which is located in Dongchuan District, Yunnan Province, China, is a watershed prone to debris flows and has long-term recorded data of debris-flow occurrence. However, the initiation mechanism has mainly been studied by experiments in this watershed. To further reveal debris-flow formation mechanism in the Jiangjia Gully, debris-flow activities in the initiation zone were observed with hand-held video cameras in the summer of 2016 and 2017. In these two years, six debris-flow events were triggered in Menqian Gully, a major tributary of the Jiangjia Gully, while debris-flow activities in some sub-watersheds of Menqian Gully were recorded with video cameras in four events. The video recording shows that landslides constituted an important source for sediment supply in debris flow. Some landslides directly evolved into debris flows, while the others released sediment into rills and channels, where debris flows were generated for sediment entrainment by water flow. Therefore, debris-flow occurrence in the Jiangjia Gully is influenced both by infiltration-dominated processes and by runoff-dominated processes. In addition, rainfall data from four gauges installed in Menqian Gully were analyzed using mean intensity (I), duration (D), peak 10-minute rainfall (R-10min) and antecedent rainfall (AR) up to 15 days prior to peak 10-minute rainfall. It reveals that debris-flow triggering events can be discriminated from non-triggering events either by an I-D threshold or by an R-10min-AR threshold. However, false alarms can be greatly reduced if these two kinds of thresholds are used together. Moreover, behaviors including intermittency of debris flow, variance in moisture content and volume among surges, and coalescence of multiple surges by temporary damming were observed, indicating the complexity of debris-flow initiation processes. These findings are expected to enhance our knowledge on debris-flow formation mechanism in regions with similar environmental settings.
资助项目National Key Research and Development Program of China[2020YFD1100701] ; Science and Technology Research and Development Program of China Railway[K2019G006] ; Chongqing Municipal Bureau of Land, Resources and Housing Administration[KJ-2021016]
WOS研究方向Environmental Sciences & Ecology
语种英语
出版者SCIENCE PRESS
WOS记录号WOS:000819035700009
源URL[http://119.78.100.138/handle/2HOD01W0/15967]  
专题中国科学院重庆绿色智能技术研究院
通讯作者ZHANG Shao-jie
作者单位1.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Earth Surface Proc, Chengdu 610041, Peoples R China
2.Chinese Acad Sci, Chongqing Inst Green & Intelligent Technol, Chongqing 400714, Peoples R China
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YANG Hong-juan,ZHANG Shao-jie,HU Kai-heng,et al. Field observation of debris-flow activities in the initiation area of the Jiangjia Gully, Yunnan Province, China[J]. JOURNAL OF MOUNTAIN SCIENCE,2022,19(6):1602-1617.
APA YANG Hong-juan,ZHANG Shao-jie,HU Kai-heng,WEI Fang-qiang,WANG Kai,&LIU Shuang.(2022).Field observation of debris-flow activities in the initiation area of the Jiangjia Gully, Yunnan Province, China.JOURNAL OF MOUNTAIN SCIENCE,19(6),1602-1617.
MLA YANG Hong-juan,et al."Field observation of debris-flow activities in the initiation area of the Jiangjia Gully, Yunnan Province, China".JOURNAL OF MOUNTAIN SCIENCE 19.6(2022):1602-1617.

入库方式: OAI收割

来源:重庆绿色智能技术研究院

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