易碎岩石的宏微裂变机制和声学发射特征由加载率效应诱导
Yun Cheng1,2,3, Changwei Li4,5, Yinhao Sun4,5
1School of Civil Engineering, Yancheng Institute of Technology, Yancheng, 224051, Jiangsu, China. chengyun_ifu@163.com.
Scientific reports
|October 10, 2024
概括
负载率显著影响脆性岩石.
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:
- 脆弱岩石的恶化和变形是深铁路道中的关键问题.
- 了解宏微断裂和声辐射 (AE) 演变对于道的稳定性至关重要.
研究的目的:
- 为了研究加载率对脆性岩石断裂和AE特征的影响.
- 分析机械参数,断裂模式和AE信号之间的关系.
主要方法:
- 在脆性岩石样本上进行单轴压缩试验.
- 扫描电子显微镜 (SEM) 用于微碎裂分析.
- 在不同负载率下监控声辐射 (AE) 信号.
主要成果:
- 增加的负载率提高了机械参数 (强度,模量) 并扩展了弹性变形.
- 断裂模式从斜切切转向具有更高负载率的复合和拉伸断裂.
- 显微镜分析显示,在更高的速度下抑制剪切骨折和促进拉伸骨折.
- AE参数 (振幅,密度) 随着负载率的增加而增加,拉力断裂显示出更高的AE活动.
- 累积的AE事件和能量提供比AEb值更早的警告.
结论:
- 负载率是影响脆性岩石破裂机制和AE演变的关键因素.
- 由较高的负载率促进的拉伸断裂,表现出明显的微观结构和AE特征.
- AE监测,特别是累积事件和能量,为深道中的岩石爆炸提供了有效的早期预警能力.
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