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金属矿山 ›› 2026, Vol. 55 ›› Issue (6): 85-96.

• 采矿工程 • 上一篇    下一篇

实时高温下砂岩力学特性与损伤本构模型研究

李 皓1 吉东亮1 贾康杰1 袁 维1 冯怀平1 李晓斌2,3 龙沁雨1 王玉湘1   

  1. 1.省部共建交通工程结构力学行为与系统安全国家重点实验室,河北 石家庄 050043; 2.煤炭开采水资源保护与利用全国重点实验室,北京 102209;3.北京低碳清洁能源研究院,北京 102209
  • 出版日期:2026-07-15 发布日期:2026-07-08
  • 通讯作者: 吉东亮(1992—),男,讲师,博士,硕士研究生导师。
  • 作者简介:李 皓(2001—),男,硕士研究生。
  • 基金资助:
    中国国家铁路集团有限公司研发项目(编号:L2023G017);河北省教育厅青年基金项目(编号:50199990574);河北省燕赵黄金台聚才 计划项目(编号:A2025022);国铁重大项目(编号:K2020G034);国家自然科学基金项目(编号:U2568213);煤炭开采水资源保护与利 用国家重点实验室年开放基金项目(编号:NICE_RD_2025_111);河北省自然科学杰出青年基金项目(编号:E2024210019);河北省高 等学校基础研究重点培育专项(编号:JZX2024011)。

Study on Mechanical Properties and Damage Constitutive Model of Sandstone under Real-time High Temperature

LI Hao1 JI Dongliang1 JIA Kangjie1 YUAN Wei1 FENG Huaiping1 LI Xiaobin2,3 LONG Qinyu1 WANG Yuxiang1   

  1. 1.State Key Laboratory of Mechanical Behavior in Traffic Engineering Structure and System Safety,Shijiazhuang 050043,China; 2.State Key Laboratory of Water Resource Protection and Utilization in Coal Mining,Beijing 102209,China; 3.National Institute of Clean and Low Carbon Energy,Beijing 102209,China
  • Online:2026-07-15 Published:2026-07-08

摘要: 为研究高温作用下岩石的力学特性和损伤机制,通过颗粒流软件PFC3D开展了实时高温下砂岩的单轴 压缩模拟。明晰不同温度下砂岩应力—应变特性与裂纹发展过程,阐明砂岩峰值应力、峰值应变与裂纹发展随温度 的变化规律。基于力学特性厘清了砂岩热损伤机制,并建立了高温作用下砂岩的损伤统计本构模型。研究结果表明: 0~25 ℃温度范围内,砂岩的峰值应力和峰值应变随着温度升高而降低。25~150 ℃温度范围,峰值应力和峰值应变 具有相同的变化趋势,表现为先增大后减小。此外,通过引入韧性指数反映砂岩的抗破坏能力,其变化规律与峰值应 力演化趋势相同;随着温度升高热应力会促使原生裂纹扩展并产生新裂纹,内部颗粒膨胀会进一步加速裂纹发育最 终形成整体破坏。最后,构建了高温作用下砂岩的损伤统计本构模型,并结合模拟结果验证了模型的合理性。该研究 可为高温环境下砂岩力学特性的分析提供理论支持。

关键词: 高温 , 力学特性 , 韧性系数 , 本构模型 , Weibull分布

Abstract: In order to study the mechanical properties and damage mechanism of rock under high temperature,the uniaxi al compression simulation of sandstone under real-time high temperature was carried out by particle flow software PFC3D.The stress-strain characteristics and crack development process of sandstone at different temperatures are clarified,and the variation law of peak stress,peak strain and crack development of sandstone with temperature is clarified.Based on the mechanical prop erties,the thermal damage mechanism of sandstone is clarified,and the damage statistical constitutive model of sandstone under high temperature is established.The results show that the peak stress and peak strain of sandstone decrease with the increase of temperature in the temperature range of 0~25 ℃.In the temperature range of 25~150 ℃,the peak stress and peak strain have the same change trend,which increases first and then decreases.In addition,the toughness index is introduced to reflect the an ti-failure ability of sandstone,and its change rule is the same as the evolution trend of peak stress.As the temperature increa ses,the thermal stress will promote the propagation of the original crack and generate new cracks,and the expansion of the in ternal particles will further accelerate the crack development and eventually form the overall damage.Finally,the damage statis tical constitutive model of sandstone under high temperature is constructed,and the rationality of the model is verified by the simulation results.This study can provide theoretical support for the analysis of mechanical properties of sandstone under high temperature environment.

Key words: hightemperature,mechanicalproperties,toughnesscoefficient,constitutivemodel,Weibulldistribution

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