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岩石和岩石类材料之间的断裂特征的比较分析
Xinnan Cui1, Jianming Wang1, Bo Pan1
1Ansteel Beijing Research Institute, Beijing, 102211, China.
Heliyon
|August 3, 2023
概括
这项研究揭示了像石膏这样的脆性地质材料可以在最小的声辐射和小断裂过程区域 (FPZ) 时立即发生断裂. 更柔软的材料,如砂岩,呈现逐渐损坏和更大的FPZs.
科学领域:
- 地质技术工程 地质技术工程
- 材料科学 是一种材料科学.
- 岩石机械学 岩石机械学
背景情况:
- 了解地质材料的断裂行为对于工程应用至关重要.
- 岩石和类似岩石的材料在压力下表现出不同的机械反应.
研究的目的:
- 为了研究和比较各种岩石和岩石类材料的断裂特性.
- 分析断裂过程区域 (FPZ) 的形成机制.
主要方法:
- 在石膏,大理石,花岩,混凝土和细砂岩上进行了划痕半圆形曲 (SCB) 实验.
- 裂口开口位移被用尺测量. 裂口开口位移使用尺测量.
- 使用声波发射 (AE) 和数字图像相关性 (DIC) 来分析损坏,故障模式和FPZ.
主要成果:
- 地质材料根据脆性进行排名:石膏 <大理石 <花岩 <混凝土 <细砂岩.
- 易碎的材料 (石膏,大理石,花岩) 与柔性材料 (砂岩,混凝土) 相比显示出更高的裂开口速度.
- 随着脆弱性的增加,声辐射活动和FPZ大小下降.
结论:
- 断裂行为与材料特性有很大差异,从脆性材料的瞬间拉伸失效到柔性材料的损伤积累.
- FPZ形成受到材料的内部结构的影响,包括相互锁定和颗粒大小.
- AE和FPZ分析提供了对地质材料破裂机制的见解.
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