浅层滑坡诱发沟谷型泥石流的物源条件

陈文鸿; 余斌; 叶鹏; 柳侃; 叶龙珍; 杨治义

doi:10.3799/dqkx.2022.469

Volume 50 Issue 6

Jun. 2025

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Chen Wenhong, Yu Bin, Ye Peng, Liu Kan, Ye Longzhen, Yang Zhiyi, 2025. Research on Material Source Factors of Gully-Type Debris Flow Caused by Shallow Landslides. Earth Science, 50(6): 2356-2371. doi: 10.3799/dqkx.2022.469

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Chen Wenhong, Yu Bin, Ye Peng, Liu Kan, Ye Longzhen, Yang Zhiyi, 2025. Research on Material Source Factors of Gully-Type Debris Flow Caused by Shallow Landslides. Earth Science, 50(6): 2356-2371. doi: 10.3799/dqkx.2022.469

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Research on Material Source Factors of Gully-Type Debris Flow Caused by Shallow Landslides

doi: 10.3799/dqkx.2022.469

Chen Wenhong^{1, 2, 3
,},
Yu Bin¹,
Ye Peng¹,
Liu Kan⁴,
Ye Longzhen⁴,
Yang Zhiyi¹

1.
State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology, Chengdu 610059, China
2.
Chongqing Bureau of Geology and Mineral Exploration, Chongqing 401121, China
3.
Nanjiang Hydrogeological Engineering Geological Team, Chongqing Bureau of Geology and Mineral Resources Exploration and Development, Chongqing 401121, China
4.
Key Laboratory of Geohazard Prevention of Hill Mountain, Ministry of Natural Resources, Fuzhou 350002, China

Received Date: 2024-02-01
Available Online: 2025-07-11
Publish Date: 2025-06-25

Abstract

Abstract

Few studies pay attention to revealing the relationship between the amount of landslide material and the formation of gully debris flow, although a large number of shallow landslides in a watershed can lead to gully-type debris. Thus, the landslide source conditions required for the formation of this type of debris flow are evaluated based on the mechanism of debris flow formation. To analyze the relationship between the debris flow by shallow landslides in Baozhuang Village, Fujian, in 2010. And the material model of gully-type debris flow by shallow landslides was proposed. The result shows that the larger the landslides area in the catchment, the greater the possibility of gully-type debris flow. The landslide area (A₀), catchment area (A) and soil thickness (h) can be applied to classify the susceptibility class of gully-type debris flow by shallow landslides. For the gullies in the East China region: when the average soil thickness of the catchment is h (m), the total of area where landslides occur (A₀) is related to the area of the catchment (A) as: it is very high probabilities of debris flow formation when A₀/A≥0.045×(3/h). The probabilities of debris flow formation is medium when 0.02×(3/h)≤A₀/A≤0.045×(3/h). The probabilities of debris flow formation is very low when 0.02×(3/h)≥A₀/A. When the total area of landslides entering the channel (A_L) is related to the area of the catchment (A) as: it is very high probabilities of debris flow formation when A_L/A≥0.03×(3/h). The probabilities of debris flow formation is medium when 0.006 5×(3/h)≤A_L/A≤0.03×(3/h). The probabilities of debris flow formation is very low when 0.006 5×(3/h)≥A_L/A. The empirical models are simple, and the data needed necessary for the input are easily measurable catchment areas and landslides area. The approach may be applied to the analysis debris flow by shallow landslides in other areas due to simplicity, when adapting the threshold parameters according to new local conditions.
- shallow landslides,
- debris flow,
- statistical model,
- threshold,
- engineering geology

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References(50)

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Research on Material Source Factors of Gully-Type Debris Flow Caused by Shallow Landslides

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