Tests on the mitigation of dry granular flows induced by mountain landslides using ring-net technologies
文献类型:期刊论文
作者 | Wang, Bin3,4; Tian, Hongyan3,4; Su, Lijun2,3,4![]() |
刊名 | EARTH SURFACE PROCESSES AND LANDFORMS
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出版日期 | 2025-02-01 |
卷号 | 50期号:2页码:20 |
关键词 | analytical model dry granular flow granular jump impact force ring-net flexible barrier |
ISSN号 | 0197-9337 |
DOI | 10.1002/esp.70003 |
英文摘要 | ROCCO ring-net flexible barriers play a crucial role in mitigating granular flows induced by landslides in steep mountainous regions. In geotechnical engineering practice, the design of these barriers critically depends on two key factors: the maximum jump height of the granular flow and its peak impact force. While ring-net flexible barriers are known for their deformability and permeability, these characteristics remain poorly understood from a quantitative perspective. To further reveal the impact-jump mechanisms of granular flows against ROCCO ring-net flexible barriers, an array of small-scale laboratory flume experiments were conducted. To modify the permeability of the barrier, three groups of particles with different median diameters were configured to control the relative diameter ratios between the ring-net mesh size and the grains from 2.0 to 3.6. The flow depth and velocity of the incoming granular flow were adjusted by altering the channel inclination to ensure the Froude number between 3 and 10 for dynamic similarity. Specifically accounting for barrier deformation and material outflow, the semi-empirical analytical models, grounded in the principles of momentum and mass conservation, were established. Futhermore, the proposed models were validated by comparing the normalized jump height, and the impact force coefficient at the moment of peak impact force between the prediction value and the experiment data. The experimental results show that both the incoming flow characteristics and the relative diameter ratio lambda jointly determine the impact-jump mechanisms: pile-up or run-up. A larger lambda tends to transition the impact-jump mechanism from pile-up to run-up under the flow conditions with a high Froude number Fr, while the corresponding maximum granular jump height and peak impact force decrease as expected. Comparison between the proposed models and experimental results indicates that barrier deflection determines the upper limit of the jump height, while the lower limit is further controlled by the outflow mass flux. The improved hydro-dynamic impact force model can adequately address most run-up scenarios, whereas, for pile-up cases, the contribution of the hydro-static force should also be considered. |
WOS关键词 | DEBRIS-FLOW ; QUANTITATIVE-ANALYSIS ; RIGID BARRIER ; RUN-UP ; IMPACT ; SIZE ; MASS |
资助项目 | National Key Research and Development Program of China |
WOS研究方向 | Physical Geography ; Geology |
语种 | 英语 |
WOS记录号 | WOS:001417698900001 |
出版者 | WILEY |
资助机构 | National Key Research and Development Program of China |
源URL | [http://ir.imde.ac.cn/handle/131551/58757] ![]() |
专题 | 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
通讯作者 | Su, Lijun |
作者单位 | 1.Liupanshui Normal Univ, Sch Civil Engn & Urban Planing, Liupanshui, Peoples R China 2.China Pakistan Joint Res Ctr Earth Sci, Islamabad, Pakistan 3.Univ Chinese Acad Sci, Beijing, Peoples R China 4.Chinese Acad Sci, Inst Mt Hazards & Environm, State Key Lab Mt Hazards & Engn Resilience, Chengdu, Peoples R China |
推荐引用方式 GB/T 7714 | Wang, Bin,Tian, Hongyan,Su, Lijun,et al. Tests on the mitigation of dry granular flows induced by mountain landslides using ring-net technologies[J]. EARTH SURFACE PROCESSES AND LANDFORMS,2025,50(2):20. |
APA | Wang, Bin,Tian, Hongyan,Su, Lijun,Xiao, Siyou,Liu, Zhenyu,&Miao, Shuaisheng.(2025).Tests on the mitigation of dry granular flows induced by mountain landslides using ring-net technologies.EARTH SURFACE PROCESSES AND LANDFORMS,50(2),20. |
MLA | Wang, Bin,et al."Tests on the mitigation of dry granular flows induced by mountain landslides using ring-net technologies".EARTH SURFACE PROCESSES AND LANDFORMS 50.2(2025):20. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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