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不同烃源岩实验评价方法的对比

刘全有 刘文汇 王晓锋 王万春

刘全有, 刘文汇, 王晓锋, 王万春. 不同烃源岩实验评价方法的对比[J]. 石油实验地质, 2007, 29(1): 88-94. doi: 10.11781/sysydz200701088
引用本文: 刘全有, 刘文汇, 王晓锋, 王万春. 不同烃源岩实验评价方法的对比[J]. 石油实验地质, 2007, 29(1): 88-94. doi: 10.11781/sysydz200701088
Liu Quanyou, Liu Wenhui, Wang Xiaofeng, Wang Wanchun. COMPARISONS OF GEOCHEMICAL METHODS FOR ASSESSMENT OF HYDROCARBON-GENERATING POTENTIAL[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(1): 88-94. doi: 10.11781/sysydz200701088
Citation: Liu Quanyou, Liu Wenhui, Wang Xiaofeng, Wang Wanchun. COMPARISONS OF GEOCHEMICAL METHODS FOR ASSESSMENT OF HYDROCARBON-GENERATING POTENTIAL[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2007, 29(1): 88-94. doi: 10.11781/sysydz200701088

不同烃源岩实验评价方法的对比

doi: 10.11781/sysydz200701088
详细信息
    作者简介:

    刘全有(1975- ),男(汉族),山西朔州人,博士后,主要从事油气地质与地球化学领域的研究工作.

  • 中图分类号: TE122.1

COMPARISONS OF GEOCHEMICAL METHODS FOR ASSESSMENT OF HYDROCARBON-GENERATING POTENTIAL

  • 摘要: 在Rock-Eval热解法、H/C比及加水热模拟实验3种烃源岩生烃潜力评价方法对比的基础上,对塔里木盆地满加尔坳陷低成熟侏罗系煤岩进行了生烃评价。对比结果表明,H/C比值与加水热解实验法评价结果较接近,生烃量分别为9.62和9.72 mg/g,而Rock-Eval热解法得到的生烃潜力为32.75 mg/g,远高于其他两种评价结果。Rock-Eval热解法得到的是烃源岩的最大排烃量,而H/C比与加水热模拟实验法获得的是烃源岩的有效排烃量。因此,在对烃源岩的生烃评价中要根据实际需求选择不同的评价方法。

     

  • [1] Baskin D K.Atomic H/C ratio of kerogen as an estimate of thermal maturity and organic matter conversion[J].AAPG Bulletin,1997,81(9):1437~1450
    [2] Larter S R.Intergrated kerogen typing in the recognition and quantitative assessment of petroleum source rocks[A].In:Thomas B M,Dore A G,Eggen S S,eds.Petroleum geochemistry in exploration of the Norwegian shelf[M].London:Graham and Trotman.1985.269~286
    [3] Schmoker J W.Volumetric calculations of hydrocarbons generation[M].Colorado:Geology Survey,1986.323~326
    [4] Espitalie J,Madec J,Tissot B.Role of mineral matter in kerogen pyrolysis:influence on petroleum genration and migration[J].AAPG Bulletin,1980,64(1):59~66
    [5] Espitalie J,Laporte J,Madec M,et al.Rapid method for characterizing the petroleum potential and degree of evolution of source rock[J].Evue de I'institute Francais du petrole,1977,1:23~42
    [6] Jones R W.Organic facies[A].In:brooks J,Wehe D,eds.Problems of petroleum geochemistry[M].New York:Academic,1987.1~90
    [7] 程克明,王兆云.高成熟和过成熟海相碳酸盐岩生烃条件评价研究[J].中国科学D辑,1996,26(6):537~543
    [8] 曾凡刚,程克明.下古生界海相碳酸盐烃源岩地球化学的研究现状[J].地质地球化学,1998,26(3):1~8
    [9] Demaison G J,Holck A J J,Jones R W,et al.Predictive source bed stratigraphy:a guide to regional petroleum occurrence[A].In:World Petroleum Congress,ed.Proceedings of 11th World Petroleum Congress[C] ,London:World Petroleum Congress,1983.17~30
    [10] Wenger L M,Baker D R.Variations in organic geochemistry of anoxic-oxic black shale-carbonate sequences in the Pennsylvanian of the Midcontient,USA[J].Organic Geochemistry,1986,10:85~95
    [11] Peters K E,Moldowan J M.Interpreting molecular fossils in petroleum and ancient sediments[M].New Jersy:Prentice Hall Inc,1993.236
    [12] Dow W G.Application of oil correlation and source rock data to exploration in the williston basin[J].AAPG Bulletin,1977,58:1253~1262
    [13] Saxby J D,Bennett A J R,Coreoran J F,et al.Petroleum generation-simulation of six years of hydrocarbon formation from torbanite and brown coal in a subsiding basin[J].Organie Geochemistry,1986,9:69~81
    [14] Behar F,Vandenbroucke M.Chemical modeling of kerogen[J].Organic Geochemistry,1987,11:15~24
    [15] Daly A R,Edman J D.Loss of organic carbon from source rocks during thermal maturation[J].AAPG Bulletin,1987,71:546
    [16] Raiswell R.Berner R A.Organic carbon loss during burial and thermal maturity of normal marine shales[J].Geology,1987,15:853~856
    [17] Larter S R.Some pragmatic perspectives in source rock geochemistry[J].Marine and Petroleum Geology,1988,5:194~204
    [18] Hunt J M.Petroleum geochemistry and geology[M].San Francisco:W H Freeman & Co Ltd,1995.1~743
    [19] Waples D.Organic geochemistry for exploration geologists[M].Minneapolis:Burgess Publication,1981.151
    [20] Tissot B T,Durand B,Espitalie J,et al.Influence of nature and diagenesis of orgainc matter in formation of petroleum[J].AAPG Bulletin,1974,58:499~506
    [21] Jones R W,Edison T A.Microscopic observations of kerogen related to geochemical parameters with emphasis on thermal maturation[A].In:Oltz D F,ed.Low temperature metamorphism of kerogen and clay minerals[C] ,Los Angeles:SEPM Pacific Section,1978.1~12
    [22] Jones R W,Demaison J G.Organic facies:a stratigraphic contept and exploration tool[A].In:ASEAN,ed.Proceedings of the second ASCOPE conference and exhibition[C] ,Manila:ASEAN,1981.51~68
    [23] Peters K E,Moldowan J M,McCaffrey M A,et al.Selective biodegradation of extended hopanes to 25-norhopanes in petroleum reservoirs,insights from molecular mechanics[J].Organic Geochemistry,1996,24(8-9):765~783
    [24] Orr W L.Comments on pyrolytic hydrocarbon yields in source rock evaluation[J].Organic Geochemistry,1981.3:775~787
    [25] Katz B J.Limitations of Rock-Eval pyrolysis for typing organic matter[J].Organic Geochemistry,1983,4:195~199
    [26] Crossey L J,Hagen E S,Surdam R C,et al.Correlation of organic parameters derived from elemental analysis and programmed pyrolysis of kerogen[A].In:Gautier D L,ed.Roles of organic matter in sediment diagenesis[C] ,Los Angeles:SEPM Special Publication,1986.35~46
    [27] Burwood R,Droad R J,Halpern H I,et al.Carbon isotope variations of kerogen pyrolyzates[J].Organic Geochemistry,1988,12:195~205
    [28] Horsfield B,Douglas A G.The influence of minerals on the pyrolysis of kerogens[J].Geochimica et Cosmochimica Acta,1980,44:1119~1131
    [29] Peters K E.Guidelines for evaluating petroleum source rocks using programmed pyrolysis[J].AAPG Bulletin,1986,70:31 8~329
    [30] Dung N G.Pyrolysis behavior of Australian oil shales in a fluidized bed reactor and in a material balance modified Fischer assay retort[J].Fuel,1989,68:1570~1579
    [31] Huizinga B J,Aizenshtat Z A A,Peters K E.Programmed pyrolysis-gas chromatography of artificially mature Green River keogen[J].Energy & Fuels,1988,2:74~81
    [32] Lewan M D.Evaluation of petroleum generation by hydrous pyrolysis experimentation[J].Philosophical Transactions of the Royal Society,1985,315:123~134
    [33] Peters K E,Moldowan J M,Sundaraman P.Effects of hydrous pyrolysis on biomarker thermal maturity parameters:Monterey Phosphatic and Silicenous Members[J].Organic Geochemistry,1990,15:249~265
    [34] Teerman S C,Hwang R J.Evaluation of the liquid hydrocarbon potential of coal by artifical maturation techniques[J].Organic Geochemistry,1991,17:749~764
    [35] 刘全有,刘文汇,秦胜飞等.煤岩及其显微组分热模拟成气特征[J].石油实验地质,2002,24(2):49~53
    [36] 刘全有,刘文汇,陈践发等.塔里木盆地煤系有机质热模拟实验中液态烃特征研究[J].天然气地球科学,2004,15(4):37~41
    [37] Peters K E.Cossa M R.Applied source rock geochemistry,AAPG Memoir 60[M].Tulsa:AAPG,1994.93~117
    [38] Lewan M D,Henty M E,Higley D K,et al.Material-balance assessment of the New Albany-Chesterian petroleum system of the Illinois basin[J].AAPG Bulletin,2002,86(5):745~777
    [39] Behar F,Vandenbroucke M,Tang Y,et al.Thermal cracking of kerogen in open and closed system:determination of kinetic parameters and stoichiometric coefficients for oil and gas generation[J].Organic Geochemistry,1997,26:321~339
    [40] Lewan M D.Experiments on the role of water in petroleum formation[J].Geochimica et Cosmochimica Acta,1997,61:3691~3723
    [41] Lewan M D,Comer J B,Hamilton-Smith T,et al.Feasibility study of material-balance assessment of petroleum from the New Albany Shale in the Illinsois basin[A].In:USGS,ed.U S Geological Survey Bulletin 2173[M].Denver:US Geological Survey,1995
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出版历程
  • 收稿日期:  2006-03-19
  • 修回日期:  2006-12-06
  • 刊出日期:  2007-01-28

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