融雪-降雨型滑坡失稳机理
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P642. 22

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陕西省自然科学基础研究计划面上项目(2021JM-180);中交第二公路工程局有限公司重点科技项目,项目编号2020X-1-20;


Study on the destabilization mechanism of snowmelt-rainfall type landslide
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    摘要:

    冻区融雪降雨导致的滑坡对公路交通基础设施的建养造成了巨大威胁,本研究以新疆伊犁地区某公路工程为依托,为此进行现场勘察,建立了新疆某公路6#滑坡监测站,通过建立监测站,对该边坡的位移、水分、温度等信息开展监测,利用该监测站2019年11月至2020年8月整个冻结融化期的监测数据,同时基于geostudio软件的非饱和土分析,将数值模拟土壤含水率变化与现场监测数据进行拟合,建立了有效的数值方法,并对融雪期该边坡在季节性冻土冻融影响下边坡的稳定性进行了分析,研究了融雪期表层边坡土的含水率变化与边坡稳定性的关系,并根据建立模型分析了该滑坡的初始滑动。结果表明:融雪水对土壤含水率的变化起主导作用—融雪水及冻结滞水沿着裂缝优势入渗,在融雪期初期增大土体含水率,增大土体自重;在融雪期维持土体较高含水率,随着连续降雨发生,湿润锋下移,土体孔压增大,形成暂态饱和区,边坡失稳。融雪期长时降雨是该滑坡发生的重要原因。将数值模拟土壤含水率变化与现场监测数据进行拟合,在此基础上进行边坡稳定性分析的方法具有较高可信度,可为该地区之后滑坡预警提供参考。

    Abstract:

    Landslides caused by snow melt and rainfall in the seasonal freezing area pose a great threat to the construction and maintenance of highway transportation infrastructure, this study is based on a highway project in the Yili region of Xinjiang, for which a site survey was conducted and a monitoring station for 6# landslide of a highway in Xinjiang was established, by establishing a monitoring station, information such as displacement, moisture and temperature of this slope was monitored, using this monitoring station from November 2019 to August 2020 for the whole freeze-thaw period, and also based on the unsaturated soil analysis of geostudio software, the numerical simulation of soil moisture content change was fitted with the field monitoring data, and an effective numerical method was established, and the stability of this slope under the influence of seasonal permafrost freeze-thaw during the snowmelt period was analyzed, and the relationship between the moisture content change of the surface slope soil and the stability of the slope during the snowmelt period was studied, and according to the The initial sliding of the landslide was analyzed according to the model established. The results show that: snowmelt water plays a dominant role in the change of soil water content - snowmelt water and frozen stagnant water infiltrate along the fracture advantage, increasing the soil water content at the beginning of the snowmelt period and increasing the self-weight of the soil; maintaining a higher soil water content during the snowmelt period, and with the occurrence of continuous rainfall, the wetting front moves down, the soil pore pressure increases, forming a transient saturation zone and Slope destabilization. The long-time rainfall during the snowmelt period is an important reason for the occurrence of this landslide. The method of fitting the numerical simulation of soil water content changes with the field monitoring data and performing slope stability analysis on this basis has high credibility and can provide reference for landslide warning after this area.

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引用本文

凌松耀,蹇永明,张智勇,等. 融雪-降雨型滑坡失稳机理[J]. 科学技术与工程, 2023, 23(21): 8980-8987.
Ling Songyao, Jian Yongming, Zhang Zhiyong, et al. Study on the destabilization mechanism of snowmelt-rainfall type landslide[J]. Science Technology and Engineering,2023,23(21):8980-8987.

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  • 收稿日期:2022-10-13
  • 最后修改日期:2023-05-12
  • 录用日期:2023-02-02
  • 在线发布日期: 2023-07-25
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