在结解周期下,砂岩的损害演变和声辐射特性
Chuangye Wang1, Ru You1,2, Wenyu Lv2
1School of Mining and Coal, Inner Mongolia University of Science & Technology, Baotou 014010, China.
ACS omega
|February 5, 2024
概括
结解周期会降解砂岩,降低强度并增加应变. 声辐射分析揭示了内部裂的发展,高峰频率预测了故障,并表明向拉伸裂纹转移.
科学领域:
- 地质技术工程 地质技术工程
- 岩石机械学 岩石机械学
- 材料科学 材料科学 材料科学
背景情况:
- 由于冰解周期导致的岩石退化是寒冷地区基础设施的关键问题.
- 了解周期性结和解下岩石损伤的微机制,对于预测材料的行为和确保结构完整性至关重要.
研究的目的:
- 为了研究经过冷解周期的砂岩的变形和断裂特性.
- 分析融周期对岩石机械性能和内部损伤演变的影响.
- 为了确定监测和预测岩石破裂的关键声学排放参数.
主要方法:
- 在砂岩样本上进行了单轴压缩测试.
- 使用声波排放 (AE) 监测来捕捉微裂变事件.
- 分析包括峰值应力,弹性模量,应变,AE能量,事件速率,振幅和频率.
- 计算了结解损害因子 (De 和 D).
主要成果:
- 砂岩峰应力和弹性模量下降,而随着更多的结解周期,应力增加.
- 能源和事件率的AE有效地表明了内部裂的发展.
- 峰值频率成为预测最终失败的敏感指标.
- 裂纹特征从混合拉力切割转变为主要的拉力破裂,经过广泛的冷解暴露.
结论:
- 冷解周期显著削弱了砂岩,并促进了内部裂的生长.
- 声波发射参数,特别是峰值频率,为岩石损伤进展和故障预测提供了宝贵的见解.
- 这些发现有助于更好地了解环境压力因素下的岩石力学,并为寒冷气候中的工程实践提供信息.
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