岩在周期性水分浸泡和湿下的孔裂结构的进化特征
Yankun Ma1,2, Jing Cheng1,2, Xiaoqi Wang3
1Anhui University of Science and Technology, School of Safety Science and Engineering, Huainan, Anhui 232001, China.
ACS omega
|February 16, 2026
概括
循环潮湿浸泡和湿 (CMIW) 改变了煤的孔裂纹结构 (PFS),增加了透性和改善了水分分布. 这项研究提供了优化煤层注入水以抑制灰尘的见解.
科学领域:
- 地质地质地质地质地质地
- 材料科学 材料科学 材料科学
- 采矿工程 采矿工程 采矿工程
背景情况:
- 煤层水注入对于抑制灰尘至关重要.
- 了解水与煤的相互作用是优化这一过程的关键.
- 孔隙裂结构 (PFS) 显著影响煤炭中的流体流动和水分分布.
研究的目的:
- 为了研究在循环潮湿浸泡和湿 (CMIW) 下,煤的PFS的演变.
- 分析CMIW对矿物质含量,孔隙特性和透性的影响.
- 探索PFS演变和湿度分布之间的关系,以改善除尘策略.
主要方法:
- 在煤样本上进行循环潮湿浸泡和湿 (CMIW) 实验.
- 低场核磁共振 (NMR) 测试T2频谱和MRI成像.
- 用X射线衍射 (XRD) 分析矿物质含量变化.
- 透度测量以量化流量特征.
主要成果:
- CMIW显著降低了高酸盐,酸盐和石英含量.
- PFS的演变导致中等毛孔的增加和毛孔连接的改变.
- 透率大幅增加 (高达1665%),水分分布变得更加均.
- 漏孔的碎形尺寸下降,水分布异构性随着反复湿而减弱.
结论:
- CMIW从根本上改变了煤的PFS和矿物成分.
- 通过可控湿来优化PFS可以提高煤炭的透性和水分分布.
- 这些发现为通过通过管理PFS和湿度均性来改善煤层注入水的粉尘抑制提供了科学依据.
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