冻融循环作用下寒区花岗岩细观损伤特征分析
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P642.3

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国家自然科学基金(No. 42477174);西藏自治区科技项目(XZ202402ZD0001,XZ202601YD0002 ,XZ202502YD0003)


Analysis of Micro-Damage Features in Cold-Region Granite Under Freeze-Thaw Cycles
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    摘要:

    由于高寒地区岩石长期受到冻融循环作用,岩石强度下降,影响工程长期稳定性。本文以川藏铁路沿线花岗岩为研究对象,开展了不同冻融循环次数后花岗岩的三轴卸荷试验,基于离散元数值模拟,建立了考虑水颗粒膨胀效应的冻胀数值模型。通过系统分析冻融岩样三轴卸荷过程中应力-应变曲线演变、微裂隙扩展、力链场演化、位移云图分布以及能量转化特征,揭示了其损伤演化规律。结果表明:(1)冻融作用导致岩样宏观力学参数同步下降,60次循环后试验测得黏聚力、峰值应力与弹性模量分别下降了62.08%、59.5%和60.2%;(2) 冻融损伤起源于微裂隙的萌生与扩展,破坏模式逐步由剪切主导演化为拉-剪复合型,颗粒位移由表及里加剧,最终引发宏观剥落;(3)受载试样微裂隙演化呈现“慢-陡-缓”三阶段特征,冻融次数增至20、40、60次,拉张裂纹起裂应力依次下降49.9%,97%,97.9%,剪切裂纹起裂应力相应下降48.8%,96.6%,97.3%,新裂纹萌生受到抑制,能量更集中于既有裂隙的贯通与扩展;(4) 弹性应变能占比由初始状态的92.8%降至60次冻融后的76.47%,表明冻融作用显著削弱了岩石的储能能力,从能量机制层面揭示了其强度丧失的本质原因。

    Abstract:

    Due to the long-term freeze-thaw cycle of rocks in high-altitude regions, their strength decreases, which affects the long-term stability of the project. Triaxial unloading tests on granite from the Sichuan Tibet Railway after different freeze-thaw cycles are conducted. Based on discrete element numerical simulation, a numerical model of frost heave considering the effect of water particle expansion is established. By systematically analyzing the evolution of stress-strain curves, micro-crack propagation, force chain evolution, displacement cloud distribution, and energy transformation characteristics during the triaxial unloading process of freeze-thawed rock samples, the damage evolution laws are revealed. The results indicate that: (1) Freeze-thaw action leads to a synchronous decline in the macroscopic mechanical parameters of the rock samples. After 60 cycles, the measured cohesion, peak stress, and elastic modulus decreased by 62.08%, 59.5%, and 60.2%, respectively. (2) Freeze-thaw damage originates from the initiation and propagation of micro-cracks. The failure mode gradually evolves from shear-dominated to[ ] tensile-shear composite, with particle displacement intensifying from the surface inward, ultimately leading to macroscopic spalling. (3) The micro-crack evolution in loaded specimens exhibits a three-stage characteristic of slow-steep-gentle. As the number of freeze-thaw cycles increases to 20, 40, and 60, the initiation stress of tensile cracks decreases by 49.9%, 97%, and 97.9%, respectively, while that of shear cracks decreases by 48.8%, 96.6%, and 97.3%, respectively. The initiation of new cracks is suppressed, and energy becomes more concentrated on the connection and propagation of existing cracks. (4) The proportion of elastic strain energy decreases from the initial 92.8% to 76.47% after 60 freeze-thaw cycles, indicating that freeze-thaw action significantly weakens the energy storage capacity of the rock, revealing the essential reason for its strength loss from the perspective of energy mechanism.

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唐群佳,温韬,张勃成,等. 冻融循环作用下寒区花岗岩细观损伤特征分析[J]. 科学技术与工程, 2026, 26(26): 11185-11199.
Tang Qunjia, Wen Tao, Zhang Bocheng, et al. Analysis of Micro-Damage Features in Cold-Region Granite Under Freeze-Thaw Cycles[J]. Science Technology and Engineering,2026,26(26):11185-11199.

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  • 收稿日期:2026-01-01
  • 最后修改日期:2026-07-07
  • 录用日期:2026-04-07
  • 在线发布日期: 2026-09-29
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