理论与试验研究

干湿与循环载荷耦合下白云岩力学特性演化

  • 成功 ,
  • 周长冰 ,
  • 王运敏 ,
  • 李小双
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  • 1.绍兴文理学院 土木工程学院,浙江 绍兴 312000;
    2.金属矿山安全与健康国家重点实验室,安徽 马鞍山 243000;
    3.中钢集团马鞍山矿山研究总院股份有限公司,安徽 马鞍山 243000;
    4.齐鲁理工学院 土木工程学院,济南 250200;
    5.常州大学 城市建设学院,江苏 常州 213164
成功(1999—),男,江苏南通人,硕士生,从事矿山岩体力学研究工作。E-mail:1569652410@qq.com
李小双(1983—),男,湖北随州人,教授,从事矿山岩体力学研究工作。E-mail:xsli2011@cczu.edu.cn

收稿日期: 2025-07-15

  网络出版日期: 2026-06-23

基金资助

国家自然科学基金(42477142,42277154);江苏省中青年学术带头人项目(SCZ2509200010)

Evolution of Mechanical Properties of Dolomite under Coupled Dry-Wet and Cyclic Loads

  • Cheng Gong ,
  • Zhou Changbing ,
  • Wang Yunmin ,
  • Li Xiaoshuang
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  • 1. School of Civil Engineering, Shaoxing University of Arts and Sciences, Shaoxing, Zhejiang 312000, P. R. China;
    2. State Key Laboratory of Safety and Health in Metal Mines, Maanshan, Anhui 243000, P. R. China;
    3. Sinosteel Maanshan Mining Research Institute Co., Ltd., Maanshan, Anhui 243000, P. R. China;
    4. School of Civil Engineering, Qilu University of Technology, Jinan 250200, P. R. China;
    5. School of Urban Construction, Changzhou University, Changzhou, Jiangsu 213164, P. R. China

Received date: 2025-07-15

  Online published: 2026-06-23

摘要

针对循环载荷与干湿循环耦合作用对白云岩力学特性演化规律的影响,进行了不同干湿循环次数和循环载荷上限条件下的三轴压缩试验,并结合宏细观结构分析,系统研究了白云岩的强度衰减、变形特性及损伤演化机制。结果表明:随着干湿循环次数的增加,白云岩质量降低、含水率呈对数增加趋势;随干湿循环次数增加,白云岩峰值抗压强度、弹性模量逐渐降低,损伤因子呈对数增加,不同上限循环荷载对于干湿劣化效应具有一定促进作用;试样弹性模量随循环荷载上限增加呈不同变化趋势;干湿循环对白云岩破坏模式无明显影响,即剪切破坏或剪切拉伸混合破坏;干湿循环作用会造成白云岩内部可溶盐和胶体的溶解以及裂隙的开裂扩展,而不同上限循环加卸载加速了裂隙扩展及颗粒间胶结物的破坏,两者共同作用时,岩石物理性质的衰减速度比单一因素更为迅速。

本文引用格式

成功 , 周长冰 , 王运敏 , 李小双 . 干湿与循环载荷耦合下白云岩力学特性演化[J]. 地下空间与工程学报, 2026 , 22(3) : 860 -869 . DOI: 10.20174/j.JUSE.2026.03.11

Abstract

Regarding the influence of cyclic loading and dry-wet cycling coupling effects on the evolution of mechanical properties of dolomite, triaxial compression tests are conducted under different dry-wet cycle counts and cyclic loading upper limits. Combined with macro- and microstructural analysis, the strength degradation, deformation characteristics, and damage evolution mechanisms of dolomite are systematically investigated. The results indicate that: As the number of dry-wet cycles increases, the mass of dolomite decreases, while the water content shows a logarithmic increasing trend. With the increase in dry-wet cycles, the peak compressive strength and elastic modulus of dolomite gradually decrease, and the damage factor exhibits a logarithmic increase. Different upper-limit cyclic loadings have a certain promoting effect on the dry-wet degradation. The elastic modulus of the specimens shows varying trends with the increase in the upper limit of cyclic loading. Dry-wet cycling has no significant impact on the failure mode of dolomite, which remains shear failure or mixed shear-tensile failure. Dry-wet cycling leads to the dissolution of internal soluble salts and colloids in dolomite, as well as the initiation and propagation of cracks, while cyclic loading and unloading at different upper limits accelerate crack propagation and the destruction of cementing materials between particles. When these two factors act together, the deterioration rate of the rock's physical properties is faster than under either factor alone.

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