孔径大小:由水岩相互作用诱导的炭石的进化机制
Bo Wang1, Bin Gao2, Lilong Wang3
1Information Research Institute of the Ministry of Emergency Management, Beijing 100029, China.
ACS omega
|March 10, 2025
概括
水与岩石的相互作用显著改变了煤矿的孔隙结构,影响了煤床中甲的提取. 高矿化和流速将相互作用转移到较小的孔隙,增强甲回收潜力.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 能源科学 能源科学
背景情况:
- 水与岩石的相互作用通过改变地下孔状结构,对煤床甲 (CBM) 提取效率产生重大影响.
- 了解这些相互作用对于优化CBM回收和水库管理至关重要.
研究的目的:
- 为了研究水岩相互作用对煤层3号孔隙结构在Fanzhuang区块的影响.
- 分析不同矿化速率和流速如何影响煤炭孔状特征.
主要方法:
- 物理模拟交叉实验,旨在模拟水岩相互作用.
- 在不同的实验条件下 (矿化和流量) 对煤孔结构变化的比较分析.
主要成果:
- 水与岩石的相互作用地点主要在中孔和宏孔,在高矿化和流速下转移到微孔和小孔.
- 溶解的可溶性矿物质导致微孔合并为中孔;巨孔凝固减弱,导致转化为中孔.
- 高矿化和0.30毫升/分钟的流速对孔隙结构产生了显著影响,增加了离子度,pH和矿化.
结论:
- 水与岩石的相互作用动态地改变了煤矿的孔隙结构,对CBM提取有重大影响.
- 优化CBM生产系统可以通过在特定的水化学和流量条件下发现毛孔结构演变的发现来获取信息.
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