地下气化过程中煤体孔隙结构演化的核磁共振研究

NMR-based investigation of pore structure evolution in coal during underground gasification

  • 摘要: 在全球能源结构转型与“双碳”目标背景下,煤炭地下气化(UCG)被广泛视为深部难采煤资源实现原位高效转化与清洁利用的战略路径。UCG过程中,煤体结构在高温及多阶段化学反应(如干燥、热解、气化、氧化)作用下持续演变,孔隙结构的变化对气化剂渗流行为与合成气产率具有重要影响。为揭示热作用条件下煤体孔隙结构的响应机制,基于低场核磁共振(NMR)技术,系统研究了不同气氛(氮气与空气)及加热温度(200、300、400 ℃)对煤样孔隙度、孔径分布与孔隙连通性的影响规律。结果表明,热作用促进孔隙的扩展和连通,表现为横向弛豫时间谱峰值整体增强,尤以中孔与大孔增幅最为明显。相同温度下,空气气氛下热作用效果优于氮气气氛。空气气氛下热作用提高了煤样的孔隙度,其增长率高于氮气气氛,在400 ℃时,空气气氛下孔隙度增长率达到90.04%,远高于氮气气氛下的65.24%。同时,随着热作用温度的升高,煤样的孔隙结构发生了显著变化,微孔的占比下降,中孔和大孔的占比增加。热作用促进了孔隙连通性的增强,有利于提升煤体渗透能力。在空气气氛下,400 ℃时煤样的有效孔隙度达到19.17%,占总孔隙度的75.56%,高于氮气气氛下的15.56%,占比70.53%。此外,随着热作用温度的升高,大孔和中孔的分形维数呈下降趋势,表明热作用处理使煤样的孔隙结构更加规则,连通性与渗透性同步增强。在空气气氛下的热作用处理过程中,煤样经历了干燥、气化和燃烧等多个阶段,导致其内部结构破坏更为严重。

     

    Abstract: Against the backdrop of the global energy transition and the “dual carbon” goals, underground coal gasification (UCG) is widely regarded as a strategic pathway for the in-situ, efficient conversion and clean utilization of deep, hard-to-mine coal resources. During the UCG process, the coal structure continuously evolves under high temperatures and multi-stage chemical reactions, such as drying, pyrolysis, gasification, and oxidation. These structural changes, particularly in pore morphology, exert a significant influence on gasifying agent flow behavior and syngas production rates. To elucidate the response mechanism of coal pore structures under thermal conditions, the effects of different atmospheres (nitrogen and air) and heating temperatures (200 ℃, 300 ℃, and 400 ℃) on porosity, pore size distribution, and pore connectivity were systematically investigated using low-field nuclear magnetic resonance (NMR) technology. The results indicate that thermal treatment promotes pore expansion and improved connectivity, as evidenced by the overall enhancement of transverse relaxation time spectra, with medium and large pores exhibiting the most pronounced increases. At the same temperature, the effect of thermal treatment in an air atmosphere is more significant than that in a nitrogen atmosphere. Thermal treatment under air notably increases the coal sample’s porosity, with the growth rate surpassing that under nitrogen; at 400 ℃, porosity increased by 90.04% in air compared to 65.24% in nitrogen. Moreover, as the temperature rises, the pore structure undergoes marked transformation: the proportion of micropores decreases, while that of mesopores and macropores increases. Thermal effects also enhance pore connectivity, thereby improving the permeability of the coal matrix. At 400 ℃ in air, the effective porosity reaches 19.17%, accounting for 75.56% of the total porosity, which is higher than the 15.56% and 70.53% observed under nitrogen, respectively. Furthermore, the fractal dimensions of medium and large pores show a decreasing trend with increasing temperature, indicating that thermal treatment renders the pore structure more regular, with simultaneous improvements in connectivity and permeability. During thermal treatment in an air atmosphere, the coal samples experience multiple stages including drying, gasification, and combustion, resulting in more severe internal structural damage.

     

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