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金属矿山 ›› 2026, Vol. 55 ›› Issue (4): 68-80.

• 采矿工程 • 上一篇    下一篇

冻融循环下含胶结节理花岗岩的物理力学特性演化及拉伸破坏规律研究#br#

周 韬1,2 李 睿1,2 崔晓航1,2 李俊言1,2 范 庆3   

  1. 1. 深地工程智能建造与健康运维全国重点实验室,广东 深圳 518060;2. 深圳大学深地科学与绿色能源研究院,
    广东 深圳 518060;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
  • 出版日期:2026-04-15 发布日期:2026-05-08
  • 作者简介:周 韬(1986—),男,教授,博士。
  • 基金资助:
    国家自然科学基金资助项目(编号:52274090);深圳市自然科学基金资助项目(编号:KQTD20221101093555006)。

Study on the Evolution of Physical and Mechanical Properties and Tensile Failure Law of Cemented Jointed Granite under Freeze-thaw Cycles#br#

ZHOU Tao1,2 LI Rui1,2 CUI Xiaohang1,2 LI Junyan1,2 FAN Qing3   

  1. 1. State Key Laboratory of Intelligent Construction and Health Operation and Maintenance of Deep Earth Engineering,
    Shenzhen 518060,China;2. Institute of Deep Earth Science and Green Energy,Shenzhen University,Shenzhen 518060,China;
    3. Sinosteel Maanshan General Institute of Mining Research Co. ,Ltd. ,Maanshan 243000,China
  • Online:2026-04-15 Published:2026-05-08

摘要: 针对寒区工程岩体常遭受冻融侵蚀作用等问题,通过对含天然胶结节理花岗岩进行冻融循环试验和巴
西劈裂试验,结合光学显微镜、数字散斑(DIC)、三维表面形貌扫描、SEM 等技术,探究其在冻融循环后的物理特性、拉
伸力学特征及破坏模式的演化规律。试验结果表明:含天然胶结节理花岗岩经60 次冻融后,孔隙率增长17. 91%、波
速衰减8. 28%、裂隙平均增长宽度达3~8 μm;随着冻融次数的增加,试样微裂纹逐渐增多并随孔径增大而形成孔洞;
胶结节理经60 次冻融后其拉伸强度降低32. 23%,峰值应变上升18. 41%;通过DIC 技术、三维形貌扫描及SEM 分析
发现,胶结节理在巴西劈裂试验中呈现出从节理中心起裂后向两端扩展破坏的模式,胶结节理破坏面的尖锐程度随
冻融次数增加而显著下降,整体形貌特征趋于均质化和平滑,体现出明显的冻融循环效应。

关键词: 冻融循环 , 胶结节理 , 物理力学性能 , 破坏模式 , 巴西劈裂试验

Abstract: In view of the problems that the engineering rock mass in cold regions is often subjected to freeze-thaw erosion,
the freeze-thaw cycle test and Brazilian splitting test were carried out on the granite with natural cemented joints. Combined
with optical microscopy,digital speckle (DIC),three-dimensional surface topography scanning,SEM and other technologies,
the physical characteristics,tensile mechanical characteristics and failure mode evolution after freeze-thaw cycles were explored.
The test results show that after 60 freeze-thaw cycles,the porosity of granite with natural cemented joints increases by
17. 91%,the wave velocity decreases by 8. 28%,and the average growth width of cracks reaches 3~8 μm. With the increase of
the number of freeze-thaw cycles,the micro-cracks of the sample gradually increase and form holes with the increase of the pore
size. After 60 freeze-thaw cycles,the tensile strength of the cemented joint decreases by 32. 23%,and the peak strain increases
by 18. 41% . Through DIC technology,three-dimensional morphology scanning and SEM analysis,it is found that the cemented
joint shows a mode of expanding from the center of the joint to both ends in the Brazilian splitting test. The sharpness of the cemented
joint failure surface decreases significantly with the increase of the number of freeze-thaw cycles,and the overall morphology
tends to be homogeneous and smooth,reflecting the obvious freeze-thaw cycle effect.

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