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    Material Properties and Triaxial Thermal Damage Evolution Mechanism of Limestone under Different Temperature and Standing Time

    Source: Journal of Energy Engineering:;2025:;Volume ( 151 ):;issue: 004::page 04025029-1
    Author:
    Zhicheng Cao
    ,
    Weiqiang Zhang
    ,
    Jingyu Xie
    ,
    Zhoujian Shi
    DOI: 10.1061/JLEED9.EYENG-5875
    Publisher: American Society of Civil Engineers
    Abstract: The mechanisms of changes in rock properties over time following high-temperature exposure are critical for evaluating the long-term stability of thermally damaged surrounding rocks. This study focuses on limestone from coal-bearing sedimentary strata, conducting high-temperature experiments to analyze the changes in its physical and mechanical properties. The evolution equation of thermal damage in rock over time is derived, and the microscopic mechanisms behind the evolution of thermal damage characteristics are revealed. The results show that (1) after high-temperature treatment, the density of limestone exhibits the greatest rate of change after 60 days of placement, while the wave velocity, resistivity, and hardness show the greatest rate of change after 100 days. The mechanical properties of limestone generally change the most after 40 days of placement, with a slight rebound thereafter, stabilizing after 60 days. (2) At 20°C and 200°C, the physical and mechanical properties of limestone change insignificantly over time; however, at 400°C, the properties deteriorate over time, while, at 600°C, self-healing properties are observed. (3) At 400°C, the damage values of limestone increase over time, while, at 600°C, the damage values decrease. (4) At 20°C and 200°C, microscopic cracks do not develop over time, and the mineral composition remains largely unchanged; at 400°C, cracks begin to form and expand over time, while minerals undergo complete decomposition. At 600°C, larger cracks form, but, over time, these cracks heal, with minerals fully reacting to form new substances that fill the cracks, demonstrating clear self-healing characteristics. These findings provide an important theoretical foundation for assessing the long-term stability of rocks in high-temperature environments, particularly for geothermal energy extraction, deep mining, and other related fields. The understanding of thermal damage and self-healing properties is of significant practical relevance.
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      Material Properties and Triaxial Thermal Damage Evolution Mechanism of Limestone under Different Temperature and Standing Time

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4307578
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    contributor authorZhicheng Cao
    contributor authorWeiqiang Zhang
    contributor authorJingyu Xie
    contributor authorZhoujian Shi
    date accessioned2025-08-17T22:52:25Z
    date available2025-08-17T22:52:25Z
    date copyright8/1/2025 12:00:00 AM
    date issued2025
    identifier otherJLEED9.EYENG-5875.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4307578
    description abstractThe mechanisms of changes in rock properties over time following high-temperature exposure are critical for evaluating the long-term stability of thermally damaged surrounding rocks. This study focuses on limestone from coal-bearing sedimentary strata, conducting high-temperature experiments to analyze the changes in its physical and mechanical properties. The evolution equation of thermal damage in rock over time is derived, and the microscopic mechanisms behind the evolution of thermal damage characteristics are revealed. The results show that (1) after high-temperature treatment, the density of limestone exhibits the greatest rate of change after 60 days of placement, while the wave velocity, resistivity, and hardness show the greatest rate of change after 100 days. The mechanical properties of limestone generally change the most after 40 days of placement, with a slight rebound thereafter, stabilizing after 60 days. (2) At 20°C and 200°C, the physical and mechanical properties of limestone change insignificantly over time; however, at 400°C, the properties deteriorate over time, while, at 600°C, self-healing properties are observed. (3) At 400°C, the damage values of limestone increase over time, while, at 600°C, the damage values decrease. (4) At 20°C and 200°C, microscopic cracks do not develop over time, and the mineral composition remains largely unchanged; at 400°C, cracks begin to form and expand over time, while minerals undergo complete decomposition. At 600°C, larger cracks form, but, over time, these cracks heal, with minerals fully reacting to form new substances that fill the cracks, demonstrating clear self-healing characteristics. These findings provide an important theoretical foundation for assessing the long-term stability of rocks in high-temperature environments, particularly for geothermal energy extraction, deep mining, and other related fields. The understanding of thermal damage and self-healing properties is of significant practical relevance.
    publisherAmerican Society of Civil Engineers
    titleMaterial Properties and Triaxial Thermal Damage Evolution Mechanism of Limestone under Different Temperature and Standing Time
    typeJournal Article
    journal volume151
    journal issue4
    journal titleJournal of Energy Engineering
    identifier doi10.1061/JLEED9.EYENG-5875
    journal fristpage04025029-1
    journal lastpage04025029-13
    page13
    treeJournal of Energy Engineering:;2025:;Volume ( 151 ):;issue: 004
    contenttypeFulltext
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