Wu Jian, Wu Dun, Gao Xia, Li Bo
Anhui Province Intelligent Underground Exploration and Environmental Geotechnical Engineering Research Center, College of Civil Engineering, Anhui Jianzhu University, Hefei 230601, China.
School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China.
ACS Omega. 2023 Oct 19;8(43):40547-40560. doi: 10.1021/acsomega.3c05367. eCollection 2023 Oct 31.
The metamorphic process of coal is often affected by magma intrusion and stratigraphic tectonic movement. It is of great significance to analyze the evolution characteristics of coal structure under different metamorphisms in the study of coalification. Nineteen coal samples collected from Huainan coalfield (Zhangji coal mine, Panji-4 coal mine, and Xinji-2 coal mine) were tested by electron paramagnetic resonance (EPR) to clarify the average evolution information on organic molecular structure during coal metamorphism. The results showed that compared with deep burial metamorphism, magma intrusion and stratigraphic tectonic stress could deepen the metamorphic degree of coal. For coal samples under three kinds of metamorphism, the relationship between three EPR parameters (free radical concentration , line width Δ, and Lande factor ) and vitrinite reflectance approximately satisfied a quartic polynomial distribution. At the same time, with the increase of , the changes of EPR parameters fluctuated, showing a phased and stepwise trend of change. Compared with related studies, the results showed that there were great differences in the and Δ distribution between high-rank and medium-rank coals during organic evolution. In this paper, the functional relationship between EPR parameters of coal and under different metamorphisms was constructed, and the internal relationship between them and its influencing factors was analyzed, which provides a reference for the study of molecular structure evolution characteristics of coal in Huainan coalfield.
煤的变质过程常受岩浆侵入和地层构造运动的影响。在煤化作用研究中,分析不同变质程度下煤结构的演化特征具有重要意义。采集了淮南煤田(张集煤矿、潘集四号煤矿和新集二号煤矿)的19个煤样,通过电子顺磁共振(EPR)测试,以阐明煤变质过程中有机分子结构的平均演化信息。结果表明,与深埋变质作用相比,岩浆侵入和地层构造应力会加深煤的变质程度。对于三种变质作用下的煤样,三个EPR参数(自由基浓度、线宽Δ和朗德因子)与镜质体反射率之间的关系大致满足四次多项式分布。同时,随着的增加,EPR参数的变化呈波动状,呈现出阶段性和阶梯式的变化趋势。与相关研究相比,结果表明在有机演化过程中,高阶煤和中阶煤的和Δ分布存在很大差异。本文构建了不同变质作用下煤的EPR参数与之间的函数关系,分析了它们之间的内在联系及其影响因素,为淮南煤田煤分子结构演化特征的研究提供了参考。