吐哈盆地侏罗纪煤中主要组分结构特征与生烃性分析

孙旭光; 陈建平; 王延斌

吐哈盆地侏罗纪煤中主要组分结构特征与生烃性分析

1 北京大学地球与空间科学学院,北京,100871;
2 石油勘探开发科学研究院,北京,100083;
3 中国矿业大学北京分校,北京,100083

基金项目: 国家自然科学基金项目（批准号：42102014）

详细信息

作者简介:
孙旭光男 1966年出生博士副教授有机地化

中图分类号: P618.11;P593

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文章访问数: 300
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Micro-FTIR Spectroscopy of Maceral from Jurassic Coals in Tu-ha Basin

1 School of Earth and Space Sciences, Peking University, Beijing 100871;
2 Institute of Petroleum Exploration and Development, CNPC, Beijing 10008;
3 Beijing Graduate School, China University of Mining and Technology, Beijing 100083

摘要

摘要: 在高纯度煤岩显微组分分离富集的基础上,应用透射式显微傅里叶红外光谱技术 (Micro FTIR),对吐哈盆地侏罗纪煤中的主要组分—镜质体、丝质体、角质体、藻类体的结构组成进行了测定。结果表明 :藻类体主要由长链脂族结构组成,芳香结构含量相对较少;角质体和基质镜质体中含有较丰富的芳香结构以及长链脂族结构;而丝质体则主要由芳香结构组成,脂族结构含量很少。显微组分的这种结构特征决定了藻类体具有很高的生烃潜力、角质体和镜质体的生烃潜力中等、而丝质体的生烃潜力则很低。对于吐哈盆地煤成油来说,由于藻类体主要由长链脂族结构组成,并且生烃潜力也高,因此其具有高的液态烃产率、丝质体的产油率最小、角质体和镜质体的液态烃产率中等。由于镜质体是本区煤中含量最高的组分。因此,对于吐哈盆地所形成的具有工业规模的油田来说,镜质体应该是主要的贡献组分之一。但对于富含藻类体的厚层状烛藻煤,由于它类型好,品质高、生烃潜力大、以中长链脂族结构为主,是煤成油最理想的源岩。
- 吐哈盆地 /
- 显微傅里叶红外光谱 /
- 显微组分 /
- 结构组成 /
- 生烃潜力 /
- 煤成油
Abstract: Fourier transformation infrared microspectroscopy ( Micro-FTIR)isone of effective waysfor identify-ing the chemical structure. Based on the high-purity coal macerals separating and concentrating,in this paper, Mi-cro-FT IR technique was used to investigate the chemical composition and structuresof alginite, sporinite, cutinite,desmocollinite and fusinite from Jurassic coalsin Tu -ha basin. The results show that the chemical structure of aligi-nite and sporinite are mainly composed of long aliphatic -side chain, and minor amounts of aromatic compounds. Cutinite and desmocollinite are mostly composed of aromatic compounds,in addition to large amount of aliphatic compounds. Whereas fusinite are dominant by aromatic structure. These indicate that aliginite and sporinite are one of the best oil source-rocks, with the highest hydrocarbon generation potential; cutinite and desmocollinite are also the better oil and gas source-rocks, and have higher hydrocarbon generating potential; fusinite has little hydro-carbon-generating potential. Desmocollinite is one of the most amount of macerals in Jurassic coals in Tu-ha basin,so it is one of the most important macerals for contribution to oil from coals in Tu-ha basin.
- Tu-ha basin /
- Micro-FTIR /
- macerals /
- chemical structure /
- hydrocarbon-generating potential /
- oil from coal

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参考文献(30)

[1]	Murchison D G, Jones J M. Infrared spectra of resinite and their carbonized and oxidized products[J]. Fuel, 1966, 27: 141～158
[2]	Millais R and Murchison D G. Properties of the coal macerals: infrared spectra of alginites[J]. Fuel, 1969, 48 (2): 247～258
[3]	Dyrkacz R, Bloomquist C A, Solomon P R. Fourier transform infrared study of high-purity macerals types[J]. Fuel, 1984, 63: 536～542
[4]	Kister J.Characterization of chemical structure, degree of maturation and oil potential of torbanites by quantitative FTIR spectroscopy[J]. Fuel, 1900, 69 (11): 1 356～1 361
[5]	Michaelian K H, Friesen W I. Photoacoustic FTIR spectra of separated western Canadian coal macerals[J]. Fuel, 1990, 69: 1 271～1 275
[6]	Rochid A, Landais P. Transmission micro-infrared spectroscopy, an efficient tool for microscale characterization of coal[J]. Fuel, 1991, 70: 364～371
[7]	Pradier B, Landais P, Rochdi A, Davis A. Chemical basis of fluorescence alteration of crude oils and kerogens-II, Fluorescence and infrared micro-spectrometric analysis of vitrinite and liptinite[J]. Org.,Geochem, 1992, 18: 241～248
[8]	Lin R, Ritz P. Studying individual macerals using IR microspectroscopy, and implication on oil versus gas/condense proneness and ‘low-rank' generation[J]. Org. Geochem., 1993, 20: 695～706
[9]	Mastalerz M, Bustin R M. Electron microprobe and micro-FTIR analyses applied to maceral chemistry[J]. Inter. J. Coal Geol., 1993, 24: 333～345
[10]	Mastalerz M, Bustin R M. Application of reflectance microFourier transform infrared spectrometry in studying coal macerals: Comparison with other Fourier transform infrared techniques[J]. Fuel, 1995, 74: 536～542
[11]	Ibarra J V, Moliner R, Bonet A J. FT-IR investigation on char formation during the early stages of coal pyrolysis[J]. Fuel, 1994, 73: 918～924
[12]	Ibarra J V, Munoz E, Moliner R. FT-IR study of the evolution of coal structure during the coalification process[J].Org. Geochem., 1996, 24: 725～735
[13]	Guo Y T, Bustin R M. Micro-FTIR spectroscopy of liptinite macerals in coal[J]. Inter. J. Coal Geol., 1998, 36: 259～275
[14]	Ganz H, Kalkreuth W. Application of infrared spectroscopy to the classification of kerogen-types and the evolution of source rock and oil-shale potentials[J]. Fuel, 1987, 66: 708～711
[15]	Christy A A. Multi-variate calibration of diffuse reflectance infrared spectra of coals as an alternative to rank determination by vitrinite reflectance[J]. Chemometrics Intell. Lab. Systems, 1987, 2 (2): 199～207
[16]	Thomas B M. Land-plant source rocks for oil and their significance in Australian basin[J]. APEA J, 1982, 22 (1): 164～178
[17]	Smith G C, Cook A C. Petroleum occurrence in Gippsland basin and its relationship to rank and organic matter type[J]. APEA J, 1984, 24 (1): 196～216
[18]	Cook A C, Struckmeyer H. The role of coal as a source rock for oil[A]. In: Glennie R C, ed. Second South-Eastern Australia Oil Exploration Symposium[C]. Melbourne: Petroleum Exploration Society of Australia, 1986. 410～432
[19]	Snowdon L R, Powell T G. Immature oil and condensate-Modification of hydrocarbon generation model for terrestrial organic matter[J]. AAPG Bull, 1982, 66: 775～788
[20]	Snowdon L R. Oil from type Ⅲ organic matter: Resinite revisited[J]. Org. Geochem., 1991, 17 (6): 743～747
[21]	赵师庆,吴观茂. 论富氢镜质组型腐殖煤--生油煤的一种新类型[J]. 中国煤田地质,1995.77～81[Zhao Shiqing,Wu Guanmao.On the humic coal of hydrogen-rich vitrinite type--a new type of oil prone coals[J].Coal Geology of China,1995,7(1),77～81]
[22]	赵长毅,程克明,向忠华等. 吐哈盆地煤中基质镜质体生烃潜力与特征[J]. 科学通报,1994,39(21):1 989～1 991[Zhao Changyi,Cheng Keming,Xiang Zhonghua.The hydrocarbon generation of desmocollinite from Jurassic coal in the Turpan-Hami basin[J]. Chinese Science Bulletin,1994,39(21):1 989～1 991]
[23]	赵长毅,程克明. 吐哈盆地煤显微组分生烃模式[J]. 科学通报,1994,42(19):2 102～2 105[Zhao Changyi,Cheng Keming.The Hydrocarbon-generating Mode of Macerals from Jurassic coal in the Turpan-Hami basin,Northwest China[J].Chinese Science Bulletin,1994,42(19):2 102～2 105]
[24]	赵长毅, 程克明, 王飞宇. 吐哈盆地煤成烃主要贡献组分剖析[J]. 沉积学报, 1997, 15(2): 95～99[Zhao Changyi,Cheng Keming,Wang Feiyu.Analyses on the macerals contributing mainly to hydrocarbons derived form coals of the Turpan-Hami basin[J].Acta Sedimentologica Sinica,1997,15(2):95～99]
[25]	陈建平, 黄第藩, 李晋超, 秦勇. 吐哈盆地侏罗纪煤系油气主力源岩探讨[J]. 地质学报, 1999, 73(2): 140～152[Chen Jianping,Huang Difan,Li Jinchao,Qin Yong.Main Source Rocks of Petroleum from Jurassic Coal-bearing Strata in the Turpan-Hami,Northwest China[J].Acta Geologica Sinica,1999,73(2):140～152]
[26]	柳益群, 袁明生, 周立发, 张世焕. 新疆吐-哈盆地前侏罗系烛藻煤的发现及其地质意义[J]. 沉积学报, 2000, 4:595～599[Liu Yiqun,Yuan Mingaheng,Zhou Lifa,Zhang Shihuan.Discovery of Pre-Jurassic Cannel-Boghead with its geological Significance in Turpan-Hami basin,Xinjiang[J].Acta Sedimentologica Sinica,2000,4:595～599]
[27]	孙旭光, 李荣西, 杜美利. 煤岩显微组分分离富集[J]. 中国煤田地质, 1997, 9(3): 26～27[Sun Xuguang,Li Rongxi.Discussion on the Method of Coal Maceral Separation[J].Coal Geology of China,1997,9(3):26～27]
[28]	Marchessault R H. Application of infrared spectroscopy to cellulose and wood polysaccharides[A]. In: Wood Chemistry, Proceedings of the Wood Chemistry Symposium[C]. London: Butterworth, 1962. 107～129
[29]	Hergert L H. Infrared spectra[A]. In: Sarkanen K V, Ludwin C H eds.Lignins. New York:Wiley-Interscience, 1974. 267～297
[30]	Painter P C, Starsinic M, Coleman M M. Determination of functional groups in coal by Fourier transform interferometry[A]. In: Ferraro J R, Basile L J eds. Fourier Transform Infrared Spectroscopy[C]. Vol. 4.New York:Academic Press, 1985. 169～240

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吐哈盆地侏罗纪煤中主要组分结构特征与生烃性分析

作者简介:
孙旭光男 1966年出生博士副教授有机地化

计量

Micro-FTIR Spectroscopy of Maceral from Jurassic Coals in Tu-ha Basin

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目录

吐哈盆地侏罗纪煤中主要组分结构特征与生烃性分析

1 北京大学地球与空间科学学院,北京,100871;

2 石油勘探开发科学研究院,北京,100083;

3 中国矿业大学北京分校,北京,100083

作者简介:
孙旭光男 1966年出生博士副教授有机地化

English Abstract

Micro-FTIR Spectroscopy of Maceral from Jurassic Coals in Tu-ha Basin

1 School of Earth and Space Sciences, Peking University, Beijing 100871;

2 Institute of Petroleum Exploration and Development, CNPC, Beijing 10008;

3 Beijing Graduate School, China University of Mining and Technology, Beijing 100083

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吐哈盆地侏罗纪煤中主要组分结构特征与生烃性分析

作者简介: 孙旭光 男 1966年出生 博士 副教授 有机地化

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出版历程

Micro-FTIR Spectroscopy of Maceral from Jurassic Coals in Tu-ha Basin

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目录

吐哈盆地侏罗纪煤中主要组分结构特征与生烃性分析

1 北京大学地球与空间科学学院,北京,100871; 2 石油勘探开发科学研究院,北京,100083; 3 中国矿业大学北京分校,北京,100083

作者简介: 孙旭光 男 1966年出生 博士 副教授 有机地化

English Abstract

Micro-FTIR Spectroscopy of Maceral from Jurassic Coals in Tu-ha Basin

1 School of Earth and Space Sciences, Peking University, Beijing 100871; 2 Institute of Petroleum Exploration and Development, CNPC, Beijing 10008; 3 Beijing Graduate School, China University of Mining and Technology, Beijing 100083

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期刊在线

联系我们

作者简介:
孙旭光男 1966年出生博士副教授有机地化

1 北京大学地球与空间科学学院,北京,100871;

2 石油勘探开发科学研究院,北京,100083;

3 中国矿业大学北京分校,北京,100083

作者简介:
孙旭光男 1966年出生博士副教授有机地化

1 School of Earth and Space Sciences, Peking University, Beijing 100871;

2 Institute of Petroleum Exploration and Development, CNPC, Beijing 10008;

3 Beijing Graduate School, China University of Mining and Technology, Beijing 100083