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基于微观机理的高温后大理岩动态力学特性分析

Analysis of the dynamic mechanical properties of marble after high-temperature exposure based on microscopic mechanisms

  • 摘要: 为研究温度对大理岩动态力学特性的影响,对常温(25 ℃)及高温(200 ℃、400 ℃、600 ℃和800 ℃)后的大理岩试样开展SHPB试验、XRD和SEM微观试验,探究了高温后大理岩动态力学特性与温度的关系及微观损伤机理。结果表明:高温后大理岩的动态压缩应力-应变曲线分为弹性、屈服、破坏3个阶段;大理岩的峰值应力及破坏特征均存在明显的温度效应,即随温度的升高,大理岩的峰值应力逐渐下降,破碎程度加剧;大理岩的动态力学特性与其矿物组分及晶体结构密切相关,200 ℃~600 ℃时,微缺陷增多,且白云石发生了热分解转化,在800 ℃时,矿物分解生成CO2气体和氢氧化钙,且晶体结构发生熔融破坏,内部损伤严重,塑性增强,从而导致宏观力学特性的大幅下降。

     

    Abstract: To study the effect of temperature on the dynamic mechanical properties of marble,dynamic compression tests,XRD,and SEM microscopic tests were conducted on marble samples at room temperature (25 ℃) and after exposure to high temperatures (200 ℃,400 ℃,600 ℃,and 800 ℃).The relationship between the dynamic mechanical properties of marble and temperature,as well as the microscopic damage mechanisms,were explored.The results show that the dynamic compressive stress-strain curves of marble after high-temperature exposure can be divided into 3 stages:elastic,yield,and failure.The peak stress and failure characteristics of marble exhibit a significant temperature effect:as the temperature increases,the peak stress of marble gradually decreases,and the degree of fragmentation intensifies.The dynamic mechanical properties of marble are closely related to its mineral composition and crystal structure.Between 200 ℃ and 600 ℃,micro-defects increase,and dolomite undergoes thermal decomposition and transformation.At 800 ℃,mineral decomposition produces CO2 gas and calcium hydroxide,and the crystal structure undergoes melting damage,leading to severe internal damage and increased plasticity,resulting in a substantial decline in macroscopic mechanical properties.

     

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