利用环网技术减缓山体滑坡引起的干粒状流试验

IF 2.8 3区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Bin Wang, Hongyan Tian, Lijun Su, Siyou Xiao, Zhenyu Liu, Shuaisheng Miao
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引用次数: 0

摘要

ROCCO环网柔性屏障在缓解陡坡山区滑坡引发的颗粒流中发挥着至关重要的作用。在岩土工程实践中,这些屏障的设计主要取决于两个关键因素:颗粒流的最大跳跃高度和峰值冲击力。虽然环网柔性屏障以其可变形性和渗透性而闻名,但从定量的角度来看,这些特性仍然知之甚少。为了进一步揭示颗粒流对ROCCO环网柔性屏障的冲击-跳跃机制,进行了一系列小型室内水槽试验。为了改善屏障的渗透性,我们配置了三组中值直径不同的颗粒,将环网孔径与颗粒的相对直径比控制在2.0到3.6之间。通过改变通道倾斜度来调节来流颗粒流的流动深度和流速,保证动态相似的弗劳德数在3 ~ 10之间。建立了基于动量和质量守恒原理的半经验分析模型,具体考虑了屏障变形和物质流出。通过将预测值与实验数据进行比较,验证了模型的归一化跳跃高度和冲击力峰值时刻的冲击力系数。实验结果表明,来流特性和相对直径比λ共同决定了冲击跳跃机制:堆积或助跑。在高弗鲁德数Fr的流动条件下,较大的λ倾向于将冲击跳跃机制从堆积过渡到助跑,而相应的最大颗粒跳跃高度和峰值冲击力则如预期的那样降低。模型与实验结果的对比表明,障壁偏转决定了跳跃高度的上限,而下限则进一步受到流出质量通量的控制。改进的水动力冲击力模型可以很好地处理大多数的助跑情况,而对于堆积情况,还需要考虑水静力的贡献。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Tests on the mitigation of dry granular flows induced by mountain landslides using ring-net technologies

Tests on the mitigation of dry granular flows induced by mountain landslides using ring-net technologies

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 λ jointly determine the impact-jump mechanisms: pile-up or run-up. A larger λ 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.

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来源期刊
Earth Surface Processes and Landforms
Earth Surface Processes and Landforms 地学-地球科学综合
CiteScore
6.40
自引率
12.10%
发文量
215
审稿时长
4 months
期刊介绍: Earth Surface Processes and Landforms is an interdisciplinary international journal concerned with: the interactions between surface processes and landforms and landscapes; that lead to physical, chemical and biological changes; and which in turn create; current landscapes and the geological record of past landscapes. Its focus is core to both physical geographical and geological communities, and also the wider geosciences
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