Evolution of molecular structure during coalification and graphitization: Evidence from multiple characterization methods

IF 7.5 1区 工程技术 Q2 ENERGY & FUELS
Fuel Pub Date : 2025-10-06 DOI:10.1016/j.fuel.2025.136990
Peng Qiao , Lei Xiao , Liru Tao , Jin Qian , Kun Yu , Mingna Ge
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引用次数: 0

Abstract

The molecular structure of coal plays a critical role in coalbed methane enrichment, carbon capture, utilization and storage (CCUS), as well as in the preparation of coal-based carbon materials. However, few studies have examined the continuous, overall evolution of coal molecular structure throughout coalification and graphitization. In this work, ultimate analysis, X-ray diffraction (XRD), Raman spectroscopy, high-resolution transmission electron microscopy (HRTEM) and Fourier transform infrared spectroscopy (FTIR) were employed to characterize the molecular structure of coals ranging from low-rank to coaly graphite. The results reveal distinct spectral features corresponding to different coal maturities. During the elimination of heteroatoms, deoxidation occurs primarily in the early stage of coalification, as evidenced by the disappearance of C=O structure from low-rank to medium-rank coals. Dehydrogenation proceeds throughout both coalification and graphitization, especially at high maturity stage, marked by the loss of aliphatic side chains and aromatic C–H bonds. The evolutionary trends of La, Lc and d002 parameters derived from XRD as a function of Ro, m indicate that aromatic layers begin forming in low-rank coals, with vertical stacking continuing through the medium-rank stage and accompanied by a decrease in d002. Re-stacking of aromatic layers and re-reduction of d002 occur during the early stage of graphitization. Polycondensation of naphthalene and 3 × 3, 4 × 4 aromatic rings proceed continuously during coalification and graphitization, increasing the lateral size of crystallites. The trends in G-FWHM from Raman data and alignment degree derived from HRTEM with increasing Ro, m suggest that the molecular structure become progressively more directionally aligned from graphitized coal to coaly graphite. The stepwise evolution of multiple parameters obtained from XRD, HRTEM and Raman indicates that coal graphitization is limited to Ro, m values between 4.0 % and 5.0 %. Overall, the results enhance the theoretical framework of coalification and graphitization, and have indicative significance for coal-to-oil, CCUS and preparation of coal-based carbon materials.
煤化和石墨化过程中分子结构的演化:来自多种表征方法的证据
煤的分子结构在煤层气富集、碳捕集利用与封存(CCUS)以及煤基碳材料制备中起着至关重要的作用。然而,很少有研究考察煤分子结构在煤化和石墨化过程中的连续、全面演变。本文采用极限分析、x射线衍射(XRD)、拉曼光谱(Raman spectroscopy)、高分辨率透射电子显微镜(HRTEM)和傅里叶变换红外光谱(FTIR)对低阶煤到煤石墨的分子结构进行了表征。结果表明,不同煤成熟度对应的光谱特征不同。在杂原子消除过程中,脱氧主要发生在煤化初期,从低阶煤到中阶煤的C=O结构消失就可以证明这一点。在煤化和石墨化过程中,脱氢过程都在进行,特别是在高成熟阶段,以脂肪侧链和芳香族C-H键的损失为标志。由XRD得到的La、Lc和d002参数随Ro、m的变化趋势表明,在低阶煤中开始形成芳香层,在中阶煤中继续垂直堆积,并伴随着d002的减少。芳层的重新堆积和d002的重新还原发生在石墨化的早期。在煤化和石墨化过程中,萘和3 × 3,4 × 4芳香环不断缩聚,增大了晶体的横向尺寸。Raman数据的G-FWHM和HRTEM的取向度随Ro、m的增加而变化趋势表明,石墨化煤到煤石墨的分子结构逐渐趋向定向排列。XRD、HRTEM和Raman等参数的逐步演化表明,煤的石墨化仅限于Ro、m值在4.0% ~ 5.0%之间。总体而言,研究结果增强了煤化和石墨化的理论框架,对煤制油、CCUS和煤基碳材料的制备具有指导意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Fuel
Fuel 工程技术-工程:化工
CiteScore
12.80
自引率
20.30%
发文量
3506
审稿时长
64 days
期刊介绍: The exploration of energy sources remains a critical matter of study. For the past nine decades, fuel has consistently held the forefront in primary research efforts within the field of energy science. This area of investigation encompasses a wide range of subjects, with a particular emphasis on emerging concerns like environmental factors and pollution.
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