煤层气
钻孔
潜热
煤
磁导率
冻胀
液氮
岩土工程
霜冻(温度)
材料科学
地质学
煤矿开采
复合材料
化学
热力学
膜
物理
生物化学
有机化学
作者
Haifei Lin,Botao Li,Shugang Li,Lei Qin,Zongyong Wei,Pei Wang,Rongwei Luo
出处
期刊:Energy
[Elsevier]
日期:2024-01-25
卷期号:291: 130445-130445
被引量:8
标识
DOI:10.1016/j.energy.2024.130445
摘要
In this study, a fully coupled thermal-hydro-mechanical (THM) model was developed considering the latent heat of phase transition and expansion strain, to investigate the water-ice phase transition and heat and mass transfer laws. The response surface methodology was adopted to examine the sensitivity of input parameters on the LN2 effective freezing radius response. The results showed that the temperature of the coal surrounding the borehole dropped rapidly and generated a low-temperature region and frozen surface during the initial stage of LN2 injection (1 h). From the water-ice interface, reservoir’s frost heaving strain and permeability can be divided into three zones: the frozen zone, the transition zone, and the unfrozen zone. As the LN2 freezing time increased, the extent of the frozen zone increases, and the corresponding low permeability range of the reservoir also gradually expands. The LN2 effective freezing radius increases exponentially, and the effective solidification radius is 1.45 m after 1000 h. Sensitivity analysis demonstrates that the significant variables affecting the LN2 effective freezing radius are the water content (0.547) and initial permeability (0.268) from the main effects.
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