砂岩在中速冲击下具有不同水分含量的动态机械行为背后的潜在机制
Fanjie Kong1,2, Xiaobin Li1, Xian'e Peng3
1State Key Laboratory of Water Resource Protection and Utilization in Coal Mining, National Institute of Low Carbon and Clean Energy, Beijing, 102209, China.
水含量显著削弱了砂岩的动态压力强度,增加了应变,影响了地下水库的稳定性. 较高的和导致强度较低,而断裂程度影响了这种软化效应.
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:
- 地下煤矿水库的稳定性受到由于水侵蚀和压力而改变的岩石特性的威胁.
- 在不同的含水量和冲击负荷下,岩石的机械性能对于周围岩石的稳定性至关重要.
研究的目的:
- 为了研究水含量,动态压力强度,应变和冲击下的砂岩碎形尺寸之间的关系.
- 量化水在动态负载下对砂岩的削弱和软化作用.
主要方法:
- 在粗砂岩和细砂岩样本上进行掉落重量冲击测试.
- 砂岩样本受到不同的水含量水平的影响.
- 用碎形维度计算分析了断裂表面.
主要成果:
- 砂岩的动态压力强度随着含水量的增加而下降.
- 随着和水平的提高,砂岩的压力会增加,这表明水引起的削弱和软化效应.
- 断裂碎片尺寸最初增加,然后随着水和而减少,这表明在动态负载下存在复杂的相互作用.
结论:
- 水显著降低了砂岩的动态压力强度,并增加了它的应变,损害了水库的稳定性.
- 观察到的水的削弱效应在压力强度上的断裂程度的影响上占主导地位.
- 这些发现为评估围绕岩石的地下煤矿水库的稳定性提供了理论指导.
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