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干湿循环作用下泥质粉砂岩力学劣化规律与损伤本构模型

李智,  韩磊,  何晓芸,  侯召旭

李智, 韩磊, 何晓芸, 侯召旭. 干湿循环作用下泥质粉砂岩力学劣化规律与损伤本构模型[J]. 岩土工程技术, 2026, 40(5): 727-737. doi: 10.20265/j.cnki.issn.1007-2993.2025-0159
引用本文: 李智, 韩磊, 何晓芸, 侯召旭. 干湿循环作用下泥质粉砂岩力学劣化规律与损伤本构模型[J]. 岩土工程技术, 2026, 40(5): 727-737. doi: 10.20265/j.cnki.issn.1007-2993.2025-0159
LI Zhi, HAN Lei, HE Xiaoyun, HOU Zhaoxu. Mechanical degradation behavior and damage constitutive model of muddy siltstone under cyclic wetting and drying conditions[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(5): 727-737. doi: 10.20265/j.cnki.issn.1007-2993.2025-0159
Citation: LI Zhi, HAN Lei, HE Xiaoyun, HOU Zhaoxu. Mechanical degradation behavior and damage constitutive model of muddy siltstone under cyclic wetting and drying conditions[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2026, 40(5): 727-737. doi: 10.20265/j.cnki.issn.1007-2993.2025-0159

干湿循环作用下泥质粉砂岩力学劣化规律与损伤本构模型

doi: 10.20265/j.cnki.issn.1007-2993.2025-0159
基金项目: 中交路桥华南工程有限公司资助项目(R110124H01094)
详细信息
    作者简介:

    李 智,男,1983年生,硕士,高级工程师,主要从事公路工程的建设管理工作。E-mail:185965302@qq.com

    通讯作者:

    韩 磊,男,1995年生,工程师,主要从事公路工程的建设管理工作。E-mail:2313144534@qq.com

  • 中图分类号: TU452

Mechanical degradation behavior and damage constitutive model of muddy siltstone under cyclic wetting and drying conditions

  • 摘要: 针对桂北地区泥质粉砂岩在干湿循环作用下的力学性能劣化问题,开展不同干湿循环次数的单轴抗压强度试验与SEM试验,并基于能量演化规律确定了泥质粉砂岩的完全压密点,构建了泥质粉砂岩分段损伤本构模型。研究结果表明:(1)在经历5次干湿循环后,泥质粉砂岩单轴抗压强度和弹性模量分别下降了90.7%和81.5%,破坏模式由剪切破坏转变为拉−剪复合破坏。(2)确定耗散能等于弹性应变能的点为完全压密点,压密应变随干湿循环次数增加呈线性增大。(3)分段损伤本构模型拟合结果与试验数据的匹配度较好,可更准确地描述干湿循环作用下泥质粉砂岩的变形破坏特性。研究结果为桂北地区历经降雨−曝晒循环的边坡稳定性提供了数据支持和理论参考。

     

  • 图  1  X-射线衍射图像与矿物成分相对含量

    Figure  1.  X-ray diffraction pattern and relative mineral content

    图  2  泥质粉砂岩试样无损浸水试验结果

    Figure  2.  Results of free soaking test on argillaceous siltstone sample

    图  3  干湿循环路径图

    Figure  3.  Path diagram of wet-dry cycles

    图  4  不同干湿循环次数下泥质粉砂岩质量损失率和纵波波速变化

    Figure  4.  Variation in mass loss rate and P-wave velocity of argillaceous siltstone with number of wet-dry cycles

    图  5  不同干湿循环次数下泥质粉砂岩单轴压缩试验结果

    Figure  5.  Results of uniaxial compression tests on argillaceous siltstone under different numbers of wet-dry cycles

    图  6  试样加载过程能量演化示意图

    Figure  6.  Schematic diagram of energy evolution during sample loading

    图  7  单轴压缩试验过程泥质粉砂岩试样的能量演化曲线

    Figure  7.  Energy evolution curves of argillaceous siltstone sample during uniaxial compression test

    图  8  不同干湿循环次数下压密应变变化曲线

    Figure  8.  Variation curves of compaction strain with number of wet-dry cycles

    图  9  不同干湿循环次数下单轴压缩试验泥质粉砂岩破坏模式

    Figure  9.  Failure modes of argillaceous siltstone in uniaxial compression tests under different numbers of wet-dry cycles

    图  10  不同干湿循环次数下泥质粉砂岩破坏断面的微观形貌(500倍)

    Figure  10.  Micromorphology of fracture surface of argillaceous siltstone under different numbers of wet-dry cycles (×500)

    图  11  不同干湿循环次数下泥质粉砂岩的干湿循环损伤变量

    Figure  11.  Damage variable induced by wet-dry cycles in argillaceous siltstone

    图  12  泥质粉砂岩分段式损伤本构模型验证结果(图中蓝色背景为压密段)

    Figure  12.  Validation results of the piecewise damage constitutive model for argillaceous siltstone (the blue background in the Fig. indicates the compaction stage)

    表  1  不同干湿循环次数条件下泥质粉砂岩分段损伤本构模型参数

    Table  1.   Parameters of the piecewise damage constitutive model for argillaceous siltstone under different numbers of wet-dry cycles

    干湿循环次数n$ {D}_{12} $$ {\varepsilon }_{\text{A}n} $/10−2$ {\sigma }_{\text{A}n} $/MPa压密段非压密段
    $ {m}_{1n} $$ {F}_{1n} $R2$ {m}_{2n} $$ {F}_{2n} $R2
    00.0000.6222.1532.04191.04500.994334.43000.56350.9983
    10.0880.6722.0172.03901.17160.994314.00670.55810.9936
    20.3420.7719.8621.83001.39750.998013.95000.40610.9546
    30.4510.7717.8471.74691.29320.99678.59850.44020.9770
    40.5400.8214.6801.73921.45330.99335.55900.67910.9692
    下载: 导出CSV
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  • 收稿日期:  2025-04-08
  • 修回日期:  2025-06-30
  • 录用日期:  2025-08-25
  • 网络出版日期:  2026-10-08
  • 刊出日期:  2026-10-08

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