微裂纹类型对结解侵蚀下的砂岩宏观裂纹的影响
Yanan Sun1, Bing Liang1, Junzu Ma1
1School of Mechanics and Engineering, Liaoning Technical University, Fuxin, China.
PloS one
|August 18, 2025
概括
冷解侵蚀通过产生微裂损坏了砂岩,削弱了它的强度并改变了裂纹模式. 这项研究揭示了微裂纹如何在重复的冷解周期下影响宏观骨折行为.
科学领域:
- 地质技术工程 地质技术工程
- 材料科学 材料科学 材料科学
- 寒冷地区工程 寒冷地区工程
背景情况:
- 结冰解侵蚀在寒冷地区是一个重要的危险,导致岩石质量中的微裂.
- 不同的微裂变形式在融条件下对砂岩宏裂变的影响尚不清楚.
研究的目的:
- 分析微裂变对经过冷解循环的砂岩的宏裂变特征的影响.
- 阐明微裂变影响宏观骨折的机制.
主要方法:
- 采用了组合的声辐射 (AE) 测试和数值模拟.
- 分析包括峰值强度,弹性模量,纵向波速,AE声计数,b值,RA (道能量/总能量) 和AF (上升时间/频率含量).
- 一个数值模型的砂岩后融侵蚀被开发.
主要成果:
- 砂岩的峰值强度,弹性模量和波速随着结解周期的增加而减少.
- 在80个循环后,AE响声计数显示持续积累,表明渐进的微裂纹.
- b值趋势表明微裂变的持续积累.
- RA和AF值表明从剪切转向拉伸性故障模式,并增加结解周期.
- 数字模拟揭示了不均的移位和力链场,导致不同的断裂延伸模式.
结论:
- 融侵蚀逐渐削弱了砂岩,改变了其故障机制.
- 微裂纹,无论是沿晶体还是通过晶体,都显著影响了砂岩中的宏观裂纹模式.
- 了解这些微机制对于冷区工程和岩石质量的稳定性评估至关重要.
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