泥石流
地表径流
碎片
水文学(农业)
地质学
渗透(HVAC)
拦截
沉积(地质)
流域
环境科学
腐蚀
大洪水
夹带(生物音乐学)
洪水(心理学)
地貌学
岩土工程
构造盆地
气象学
地理
生态学
地图学
心理治疗师
考古
哲学
节奏
生物
美学
心理学
海洋学
作者
Huicong An,Canbin Ouyang,Fulei Wang,Qingsong Xu,Dongpo Wang,Weihong Yang,Tianzhen Fan
标识
DOI:10.1016/j.enggeo.2022.106546
摘要
On June 17, 2020, a large debris flow occurred in the Meilong catchment following a short-duration, high-intensity rainstorm. The debris flow was initiated by two shallow landsides upstream of the catchment and had a volume of approximately 7.7 × 105 m3. It blocked the river and then induced flooding, causing significant losses to the local residents. In this study, through a combination of field observation, image interpretation, and laboratory experiments, the initiation mechanism, erosion depth along the main channel, and deposition area of this debris flow were comprehensively analyzed. A sequentially integrated numerical model considering the rainfall interception by vegetation, infiltration, and runoff process was developed. Considering the spatial variations in the climatic, hydrological, and geotechnical parameters, the entire process of debris flow initiation, motion, entrainment, and deposition was simulated. The computational outcomes matched well with the field observation results. A combination of the proposed integrated model and spatially varying parameters can be used to effectively describe the debris flow characteristics in the initiation and propagation stages and provide significant insights into the physical processes involved in such hazards.
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