地球科学进展 ›› 1996, Vol. 11 ›› Issue (5): 453 -459. doi: 10.11867/j.issn.1001-8166.1996.05.0453

学术研究动态 上一篇    下一篇

油气生成热模拟实验研究进展
姜峰 1,张友联 2,杜建国 3   
  1. 1.中国科学院兰州地质研究所 兰州 730000;2.地震出版社 北京 100081;3.国家地震局分析预报中心 北京 100036
  • 收稿日期:1996-01-17 修回日期:1996-03-07 出版日期:1996-10-01
  • 通讯作者: 姜峰,男,1970年1月出生,硕士研究生,研究方向为同位素地球化学。
  • 基金资助:

    中国科学院资助项目(Z106-07)

ADVANCE OF PYROLYSIS EXPERIMENTATION ON HYDROCARBON GENESIS

Jiang Feng 1,Zhang Youlian 2,Du Jianguo 3   

  1. 1.Lanzhou Institute of Geology,Chinese Academy of Sciences,Lanzhou 720000;2.Seismology Press,Beijing 100081;3.Seismological Analysis and Prediction Centre,State Seismologic Bureau,Beijing 100036
  • Received:1996-01-17 Revised:1996-03-07 Online:1996-10-01 Published:1997-09-01

作为研究油气地球化学的一种重要手段──热模拟被愈来愈广泛地应用。介绍了不同时期油气生成模拟实验研究的状况,阐述了模拟实验已解决的和尚存在的问题,进而指出了其发展趋势和应开展的工作。

As an important geochemical technique for studying oil and gas generation,pyrolysis experiment is more and more widely applied.More than 100 publications about pyrolysis experiment are reveiwed,and the developments and new research fields are mentioned in this paper.New experiment techniques would be developed.More attention would be drawn to catalytic mechanism of minerals,the thermal-fluids effects on hydrocarbon formation,the effect of stress on Ro,distribution of humic acid to oil and gas formation,and the effects of super-critical fluids on oil and gas generation.

[1]Shimoyarna A and Johns W D. Formation of alkanes from fally acids in the precence of CaCOa. Geochim Cosmochim Acta,1972,36:87-91.
[2]Schouten S.   Laboratory simulation of natural sulphurization:ⅡReaction o! mulli-luncrionalized lipids with inorganic polysulphides at low temperatures. Org Geochem,1994,22(3-5):825-834.
[3]Dembicki H Jr. The effects of the mineral on the determination of kinetic parameters using modified Rock Eval pyrolysis. Qrg Geochem,1992, (18):531-539.
[4]黄第藩,秦匡宗,王铁冠,等.煤成油的形成和成烃机理.北京:石油工业出版社,1995.
[5]徐永昌,沈平,申歧样,等.煤系有机质热模拟产物的化学特征及地质意义.中科院兰州地质研究所生物气体地球化学开放研究实验室研究年报.兰州:甘肃科学技术出版社,1986.
[6]徐振泰,王顺林.干酪根向油气演化的热变模拟实验.石油学报,1981. 2(4): 25-31.
[7]李忠.试论油气形成过程中粘土矿物催化作用.石油实验地质,1992, 4(1): 59-63.
[8]陈建平,程克明,张大江,等.热模拟实验过程中生物标记物的演化.石油勘探与开发,1993. 20(2) : 30-36.
[9]杨天宇,王涵云.岩石中有机质高温高压模拟实验.石油与夭然气地质,1987, 8(4) : 380-390.
[10]张文正,裴戈,关德师.烃源岩轻烃生成与演化的热压模拟实验研究.石油勘探与开发,1991, 18(3): 1-15.
[11]李丽,王新洲.烃煤煤化作用的模拟试验.石油与天然气地质,1985, 6(2): 121-126.
[12]Mastalerz M.  The effect of temperature,pressure and strain on carbonization in high-volatile bituminous and anthracitic coals. Org Geochem,1993,21(2):315-325.
[13]Hoering T C.  Thermal realtions of kerogen with added water,  heavy water and pure organic substances.  Org Geochem,1984,(5):267-278.
[14]Rontani J F, Grossiv .Abiotic degradation of intact and photooxidized chlorophyll phytyl chain under simulated geological conditions. Org Geochem, 1995,23(4):355-366.
[15]Tissot B P and Welte D H. Petroleum Formation and occurence. Springer-Verlag Berlin Heidelberg New York,1984.
[16]卢书锷.泥质沉积物排烃模拟.石油实验地质,1987, 9(1): 22-33.
[17]Saxby J D, Riley K W. Petroleum generation by laboratory scale pyrolysis over six years simulating conditions in a subsiding basin.  Nature, 1984,308:177-179..
[18]Saxby J D, Bemett A J R,Corran J F.  Petroleum generation:Simulation over six years of hydrocarbon formation from torbanite and brown coal in a subsiding basin. Org Geochem,1986,9:69-81.
[19]Lewan M D,Winters J C, Donald J H. Generation of oil-like pyrolyzates from organic-rich shales. Science. 1979,203:897-899.
[20]Lewan M D.  Evaluation of petroleum generation by hydrous pyrolysis experimentation.  Phil Tras R Soc Lond A,1985,315:123-134.
[21]Lewan M D and Williams J A. Evaluation of petroleum generation from resinites by hydrous pyrolysis. AAPG,1987.71(2).
[22]Stalker L,Farrimond P,Larter S R. Water as an oxygen source for the production of oxygenated lompounds during kerogen maturation. Org Geochem, 1994,22(3-5):477-486.
[23]Tang Y C and Stauffer M. Formation of pristene pristane and phytane:kinetic study by laboratory pyrolysis of monterey source rock. Org Geochem,1995,23(5):451-460.
[24]Ritter V, Myhr M B, Vinge T. Experimental heating and kinetic models of source rocks; comparison of different methods. Org Geochem,1995,23(1):1-9.
[25]Treund H,Kelemen S R.格林河干酪根的低温热解.谢觉新译.地质地球化学,1991, (4): 43-48.
[26]Reyaokis J G,Burnham A K. Comparison of kinetic analysis of source rocks and kerogen concentrates. Org Geochem,1995,23(1):11-19.
[27]Andresen B. Thronden T. Barth T.  Thermal generation of carbon doxide and organic acids from different source rocks. Org Geochem,1995,21(12):1229-1242.
[28]吴肇亮,邬立言,杨国华,等.I类生油岩人工熟化热解动力学及热解气相色谱研究.石油学报,1992, 13(1): 30-36.
[29]卢双舫,王子文,黄第藩,等.煤岩显微组分的成烃动力学.中国科学((B辑),1995, 25(1): 101-107.
[30]Espitalie, Madec,Tissot B P. Role of mineral matrix in kerogen pyrolysis; influence on petroleum generation and migration. AAPG,1980,64:59-66.
[31]Durand B. Kerogen Imprimerie Bayeusaine,14401 Bayeux,France. 1980.
[32]Rowland S.早期成岩作用阶段硫加入植醇衍生物的模拟,马柯阳译.石油地质,1994, 10(2): 224-228.
[33]Hetenyi M. Experimental evolution of oil shales and kerogen isolation from them. Acta Miner Petr, 1983,X X V I/1,73-85.
[34]陈传平,梅博文,贾发敬.生油岩产生低分子量有机酸的模拟实验研究.地球化学,1994, 23(2): 155-160.
[35]堵建忠,孔庆云.显微热台油气生成模拟实验.石油勘探与开发,15 (3) : 38-43.
[36]Eglinton T I, Douglas A G,Rowland S T.  Release of aliphatic, aromatic and sulphur compounds from kimmeridge kerogen by hydrous pyrolysis: A Quantitative Study. Org Geochem,1988,(13):655-663.
[37]Kolandaisany M,Barry D B, John W S. Determination of longer chain n-alkyl content of coals. Fuel,1990, 69, October.

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