岩土力学 ›› 2025, Vol. 46 ›› Issue (9): 2661-2675.doi: 10.16285/j.rsm.2024.1378CSTR: 32223.14.j.rsm.2024.1378

• 基础理论与实验研究 •    下一篇

白云石对粉砂岩物理力学性质影响研究

张春瑞1, 2,纪洪广1, 2,付桢1, 2,张月征1, 2,宋宇1,田竹华1, 2,范文博3   

  1. 1. 北京科技大学 城市与地下空间北京市重点实验室,北京 100083;2. 矿山深井建设技术国家工程研究中心,北京 100013; 3. 中煤建设集团有限公司,北京 102218
  • 收稿日期:2024-11-16 接受日期:2025-02-10 出版日期:2025-09-10 发布日期:2025-09-03
  • 通讯作者: 纪洪广,男,1963年生,博士,教授,博士生导师,主要从事深部岩石力学、地下工程等领域的研究。E-mail: jihongguang@ces.ustb.edu.cn
  • 作者简介:张春瑞,女,1998年生,博士研究生,主要从事深部岩石力学的研究。E-mail: ustbzcr@163.com
  • 基金资助:
    地球深部探测与矿产资源勘探国家重大科技专项(No.2024ZD1004504);国家重点研发计划(No.2023YFC2907403)。

Influence of dolomite on the physical and mechanical properties of siltstone

ZHANG Chun-rui1, 2, JI Hong-guang1, 2, FU Zhen1, 2, ZHANG Yue-zheng1, 2, SONG Yu1, TIAN Zhu-hua1, 2, FAN Wen-bo3   

  1. 1. Beijing Key Laboratory of Urban Underground Space Engineering, University of Science and Technology Beijing, Beijing 100083, China; 2. National Engineering Research Center of Deep Shaft Construction, Beijing 100013, China; 3. China Coal Construction Group Limited Corporation, Beijing 102218, China
  • Received:2024-11-16 Accepted:2025-02-10 Online:2025-09-10 Published:2025-09-03
  • Supported by:
    This work was supported by the Deep Earth Probe and Mineral Resources Exploration-National Science and Technology Major Project (2024ZD1004504) and the National Key Research and Development Program of China (2023YFC2907403).

摘要: 白云石是通过白云石化作用形成,该过程使岩石孔隙率增加,以白云石为特征矿物,研究其对粉砂岩物理力学性能劣化的影响,对深部地下工程设计和稳定性预测具有重要意义。基于X射线荧光光谱仪(X-ray fluorescence spectrometer,简称XRF)、X射线衍射仪(X-ray diffractometer,简称XRD)、镜下鉴定、超声波波速、核磁共振测试,定量分析了白云石对粉砂岩物理参数的影响;通过巴西劈裂、单调加载、循环加卸载试验,获得了抗拉强度、抗压强度等力学参数的演化规律;建立了表观弹−黏−塑损伤模型,结合计算机断层扫描(computerized tomography,简称CT)和扫描电子显微镜(scanning electron microscope,简称SEM)扫描探究了白云石诱发粉砂岩劣化的机制。结果表明:(1)白云石的存在使颗粒磨圆度优,晶间咬合程度弱,与方解石交代边界孔隙明显,使孔隙连通性提升,孔隙率增大了2.77倍。(2)白云石的存在使抗拉最大应变减小,使抗压强度折减了14.5%,压密阶段延长了9%,裂纹稳定扩展阶段缩短了12%。(3)循环加卸载应力差值越大损伤值越高,不含白云石的岩石损伤变化较大,呈前期快速增加,后期缓慢增加的趋势,而含白云石的岩石损伤变化较为平稳,白云石使表观弹−黏−塑性损伤积累更剧烈。(4)不含白云石岩样裂纹弯折,耗散能较高,蓄能值低,含白云石岩样裂纹平直,耗散能较低,蓄能值高。白云石的存在使孔隙连通性增强,裂纹更易扩展,张拉裂纹占比升高。

关键词: 粉砂岩, 白云石, 力学性能, 损伤, 能量, CT扫描

Abstract: Dolomite is formed via dolomitization, a process that enhances porosity. Investigating the influence of dolomite as a characteristic mineral on the deterioration of the physical and mechanical properties of siltstone is significant for the design and stability prediction of deep underground engineering. This study employs X-ray fluorescence spectrometer (XRF), X-ray diffraction (XRD), microscopic analysis, ultrasonic wave velocity measurements, and nuclear magnetic resonance testing to quantify dolomite’s impact on siltstone’s physical parameters. Brazilian splitting tests, monotonic loading, and cyclic loading-unloading experiments reveal the evolution of mechanical parameters, including tensile and compressive strengths. An apparent elastic-viscous-plastic damage model is developed, and dolomite-induced deterioration mechanisms are investigated using computed tomography (CT) and scanning electron microscopy (SEM). The results indicate that: 1) Dolomite content enhances particle roundness, weakens intergranular interlocking, and creates distinct boundary pores with calcite, leading to enhanced pore connectivity and a 2.77-fold increase in porosity. 2) Dolomite presence reduces maximum tensile strain, decreases compressive strength by 14.5%, extends the compaction phase by 9%, and shortens the stable crack propagation phase by 12%. 3) A larger cyclic loading-unloading difference correlates with higher damage values. Dolomite-free rocks exhibit significant damage variation, with rapid early-stage increases followed by slower growth, whereas dolomite-containing rocks show more stable damage progression, with dolomite inducing more pronounced elastic-viscous-plastic damage accumulation. 4) Cracks in dolomite-free samples are bent, dissipating more energy with lower energy storage values, while those in dolomite-containing samples are straight, dissipating less energy with higher energy storage values. Dolomite enhances porosity, facilitating crack propagation and increasing the proportion of tensile cracks.

Key words: siltstone, dolomite, mechanical properties, damage, energy, CT scan

中图分类号: TU452
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