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高寒高海拔多年冻土区拓宽路基差异沉降

穆柯 袁堃 金龙 董元宏

穆柯, 袁堃, 金龙, 董元宏. 高寒高海拔多年冻土区拓宽路基差异沉降[J]. 交通运输工程学报, 2016, 16(4): 68-77. doi: 10.19818/j.cnki.1671-1637.2016.04.007
引用本文: 穆柯, 袁堃, 金龙, 董元宏. 高寒高海拔多年冻土区拓宽路基差异沉降[J]. 交通运输工程学报, 2016, 16(4): 68-77. doi: 10.19818/j.cnki.1671-1637.2016.04.007
MU Ke, YUAN Kun, JIN Long, DONG Yuan-hong. Differential settlement of widened subgrade in cold and high-altitude permafrost regions[J]. Journal of Traffic and Transportation Engineering, 2016, 16(4): 68-77. doi: 10.19818/j.cnki.1671-1637.2016.04.007
Citation: MU Ke, YUAN Kun, JIN Long, DONG Yuan-hong. Differential settlement of widened subgrade in cold and high-altitude permafrost regions[J]. Journal of Traffic and Transportation Engineering, 2016, 16(4): 68-77. doi: 10.19818/j.cnki.1671-1637.2016.04.007

高寒高海拔多年冻土区拓宽路基差异沉降

doi: 10.19818/j.cnki.1671-1637.2016.04.007
基金项目: 

国家科技支撑计划项目 2014BAG05B01

国家科技支撑计划项目 2014BAG05B03

交通运输部建设科技项目 2013 318 490 010

交通运输部应用基础研究项目 2014 319 495 090

陕西省青年科技新星计划项目 2016KJXX-91

详细信息
    作者简介:

    穆柯(1983-), 男, 陕西西安人, 中交第一公路勘察设计研究院有限公司高级工程师, 工学博士, 从事冻土区道路工程研究

  • 中图分类号: U416.168

Differential settlement of widened subgrade in cold and high-altitude permafrost regions

More Information
  • 摘要: 为了研究高寒高海拔多年冻土区拓宽路基面层吸热对下伏多年冻土温度与沉降的影响, 建立了基于热力耦合理论的差异沉降计算的有限元模型, 并利用实体工程监测数据对模型进行了修正, 分析了不同季节、不同填高与阴阳坡工况下拓宽侧路基差异沉降分布规律, 确定了多年冻土区最优路基拓宽位置。研究结果表明: 多年冻土区拓宽路基最大融深与沉降均出现在秋季, 10月份的变形最不利, 病害特征最突出, 其中4m填高路基第10年最大差异沉降为16.9cm, 分别为7、1、4月份沉降的1.1、1.4、1.7倍; 差异沉降与路基填高存在正相关性, 当路基填高分别为2、4、6 m时, 10年内路基的差异沉降分别为13.2、16.9、18.1cm; 阴坡侧拓宽路基的温度与沉降变化小于阳坡侧, 在10年内, 阳坡侧拓宽路基底面最大升温为1.3℃, 阴坡侧为0.6℃, 阳坡侧拓宽路基最大差异沉降为16.9cm, 阴坡侧为12.3cm; 即使阴坡侧拓宽, 差异沉降仍使拓宽路基顶面形成一个斜率为2%~3%的斜坡, 进而使路面产生较大附加应力, 最终造成结构层病害。

     

  • 图  1  拓宽路基病害机理

    Figure  1.  Disease mechanism of widened subgrade

    图  2  几何模型

    Figure  2.  Geometric model

    图  3  有限元模型

    Figure  3.  Finite element model

    图  4  监测传感器分布

    Figure  4.  Distribution of monitoring sensors

    图  5  拓宽路段

    Figure  5.  Widened road section

    图  6  拓宽路基实测温度

    Figure  6.  Actual measuring temperatures of widened subgrade

    图  7  拓宽路基实测沉降

    Figure  7.  Actual measuring settlements of widened subgrade

    图  8  冻土上限实测值与计算值对比

    Figure  8.  Comparison between measured and calculated values of permafrost table

    图  9  沉降实测值与计算值对比

    Figure  9.  Comparison between measured and calculated values of settlement

    图  10  不同月份路基底面温度

    Figure  10.  Bottom temperatures of subgrade at different months

    图  11  不同月份拓宽路基沉降

    Figure  11.  Settlements of widened subgrade at different months

    图  12  不同填高拓宽路基温度分布

    Figure  12.  Temperature distributions of widened subgrades with different filling heights

    图  13  不同填高拓宽路基沉降分布

    Figure  13.  Settlement distributions of widened subgrades with different filling heights

    图  14  不同填高阴阳坡侧拓宽路基温度分布

    Figure  14.  Temperature distributions of widened subgrades with different filling heights at sunny and shade slopes sides

    图  15  拓宽路基沉降对比

    Figure  15.  Settlement comparison of widened subgrades

    表  1  热传导参数

    Table  1.   Parameters of heat conduction

    下载: 导出CSV

    表  2  沉降计算参数

    Table  2.   Calculating parameters of settlement

    下载: 导出CSV

    表  3  计算模型边界条件

    Table  3.   Boundary conditions of calculating model

    下载: 导出CSV
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出版历程
  • 收稿日期:  2016-06-10
  • 刊出日期:  2016-08-25

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