砂岩损伤演化过程的能量和红外辐射特征
Hai Sun1,2, Hong-Yan Zhu1,2, Jie Han1,2
1School of Civil Engineering, Liaoning Petrochemical University, Fushun 113001, China.
Materials (Basel, Switzerland)
|June 28, 2023
概括
红外热成像监测岩石破裂,揭示能量释放和微裂传播. 这项技术有助于了解岩石力学,以加强安全监测和预警系统.
科学领域:
- 岩石机械 岩石机械 岩石机械
- 地质物理学 地质物理学
- 材料科学是一种材料科学.
背景情况:
- 岩石裂变机制涉及复杂的能量动态 (度,储存,消散,释放).
- 监测技术对于研究岩石裂变和能量消散特征至关重要.
- 红外热成像为对岩石损伤的实验研究提供了优势.
研究的目的:
- 在砂岩中建立应变能量和红外辐射之间的理论关系.
- 调查砂岩中断裂能量消散和灾难机制.
- 利用红外热成像来研究能量释放和微裂变的演变.
主要方法:
- 使用MTS电动液压伺服压力机在砂岩上进行单轴加载实验.
- 红外热成像技术用于监测散射能量,弹性能量和红外辐射.
- 在岩石损伤期间分析能量转换和红外辐射计数 (IRC).
主要成果:
- 砂岩加载过渡涉及突然变化,同时释放弹性能量,消散能量激增和IRC激增.
- 砂岩样本的IRC激增显示了三个阶段:波动,稳定上升和快速上升,与弹性能量变化相关.
- 增加的IRC激增表明更大的局部损伤和更大的弹性/散射能量变化.
- 开发了一种使用红外热成像的微裂位置和传播模式识别的新方法.
结论:
- 红外热成像有效地捕捉了岩石损伤的演变和能量消耗.
- 开发的方法允许动态可视化和评估微裂纹传播.
- 这些发现为岩石稳定性,安全监测和预警系统提供了理论基础.
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