煤炭的冷裂变动力学:由液态CO2诱导的裂变启动和传播机制2 阶段过渡
Feiyang Jin1,2, Hu Wen1,2,3, Shixing Fan1,2
1College of Safety Science and Engineering, Xi'an University of Science and Technology, Xi'an 710054, China.
ACS omega
|January 1, 2026
概括
降低液态二氧化碳 (CO2) 注入温度显著提高了煤炭裂纹网络的形成. 这种低温影响降低了断裂压力,增加了裂的分支,改善了煤床储层的修改.
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
- 能源资源 能源资源
背景情况:
- 液体二氧化碳裂变是煤层的一个有前途的无水技术.
- 在低温冲击下断裂网络形成的强化机制仍未得到充分探索.
研究的目的:
- 为了研究液体二氧化碳裂变对煤层裂变传播的低温冲击效应.
- 为了构建一个断裂传播标准,考虑液态CO2的低温影响.
- 分析煤炭破碎过程中的能量释放和断裂网络演变.
主要方法:
- 开发了一个真正的三轴液体二氧化碳裂变平台,用于低温冲击测试.
- 利用声辐射监测来研究断裂传播.
- 应用了拉伸应力标准和有效应力原理来模拟断裂传播.
主要成果:
- 液态CO2温度从10°C降低到-10°C增加了温度差异,并诱导了拉伸应力度.
- 峰值裂变压力下降了10.5%,温度应力比例从10.46%上升到23.13%.
- 每下降5°C,分支裂平均增加45%,增强了网络密度和范围.
结论:
- 液态二氧化碳的低温影响显著加剧了煤炭中断裂网络的演变.
- 这种现象降低了断裂压力,并促进了更复杂的断裂网络.
- 这些发现为优化煤床储应用中的液态二氧化碳裂变提供了理论支持.
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