等变质煤中镜质组有机地球化学研究——核磁共振特征

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ORGANIC GEOCHEMISTRY OF ISOMETAMORPHIC COAL-CHARACTERISTICS OF NUCLEAR MAGNETIC RESONANCE (NMR)

摘要: 本文应用核磁共振法CP/MAS-¹³C-NMR和¹H-NMR技术,研究高挥发份烟煤阶段(R°_max≈0.64～0.74%)两种煤相的镜质组和镜质组氯仿可溶物的核磁共振特征,并结合元素分析、抽提物分离分析以及煤岩学特征等,对这两种煤相镜质组的结构进行研究。
- 镜质组 /
- 类型 /
- 结构模型 /
- 核磁共振
Abstract: In the paper, the NMR characteristics of vitrinites and their chloroform soluble matters from the two coal facies during the high volatile stage of bituminious coal (R_max^o≈0.64～0.74%)are approached by the techniques of CP/MAS-¹³C-NMR and 1^H-NMR. Moreover, with the basis of element analysis,separation of extracts and coal petrological characteristics,the authors have studied the vitrinite textures of the two coal facies.

[1]	Vandcr Hardt D T,et al.Fuel 1976;55:202-209
[2]	Rugmirc R J,et al. New Approneles conl Clrnriairy,ACS 1981;169;23-92
[3]	Painter P C,et al. Fuel 1983; 62;103-111
[4]	Rctcufsky H L. con.Science 1982;1:93-82
[5]	赵师庆等.中国石炭二叠纪含煤地层及地质学术会议论文集,1987;366-379
[6]	赵师庆等.中国科学院有侧也球化学开放实验室年报,1987;23-99
[7]	赵师庆等.石油实验地质,1988;10(2):159-168
[8]	Gcrstcin B C,et al. conl Structure. 1982;87-129
[9]	Rctcofsky H L,et al. Fuel 1978;57;921
[10]	Brown J K,et al. Fuel 1960; 39:87
[11]	Gerstein B C,et al. conl Structure,ACS 1981;191:23-92
[12]	陈鹏等.煤焦化学,1989;33:285-289
[13]	Larsen J W,et al. Orgttic chemistry of conl,ACS 1978;73:36-99
[14]	Green T,et al. Conl Structure 1982;199-282
[15]	Giwen P H. Conl Science 1984;3:63-251
[16]	朱之培等.煤化学,1984