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煤系有机质生成烃类中甾烷系列化合物地球化学特征——以高温封闭体系下热模拟实验为例

Keywords: 甾烷,泥炭,煤岩,成熟度

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Abstract:

?选择泥炭和褐煤进行热模拟试验并开展对比研究,目的是全面获得煤系有机质生烃特征。通过对草本泥炭和褐煤的热模拟实验液态产物饱和烃进行色谱—质谱分析得到,在泥炭和褐煤热模拟样品中均检测出丰富的甾族系列化合物,且以c29甾烷占优势。研究发现,随热模拟温度增高,c29甾烷相对含量减少,温度在350℃之后趋于稳定;而c27甾烷和c28甾烷相对含量具有增加的趋势,暗示了c29甾烷的去甲基效应。c2920s/(20s+20r)值和c29ββ/(ββ+αα)值可以判识样品是否成熟或未熟,是良好的成熟度指标。∑重排甾烷/∑规则甾烷值可以区分成样品成熟度。研究发现,在低演化阶段,泥炭和褐煤模拟曲线存在显著差异,而在高演化阶段,二者吻合较好。所以,对比研究泥炭和褐煤的地球化学特征,对认识煤系有机质生烃特征具有重要意义。

References

[1]  duanyi,zhoushixin.studyonthermalsimulationofcarboniferoussourcerocksintarimbasin:ⅱcompositionandevolutionofbiomakers[j].oilandgasgeology,2001,22(1):13-16.[段毅,周世新.塔里木盆地石炭系烃源岩热模拟实验研究—ⅱ生物标志化合物的组成和演化[j].石油与天然气地质,2001,22(1):13-16.]
[2]  gaogang,jiangzhenxue,zhaozhe,etal.influenceoftemperatureincreaseveocitytothehydrocarbonformationofsourcerockbyhydropyrolysis[j].naturalgasgeoscience,2004,15(5):461-464.[高岗,姜振学,赵喆,等.加水模拟条件下升温速率对烃源岩成烃特征的影响[j].天然气地球科学,2004,15(5):461-464.]
[3]  wubaoxiang,duanyi,wangchuanyuan,etal.thermalsimulationofpeatasanoriginalmatterofcoalgenerationanditsapplicationtothestudyofcoalbedgas[j].coalgeology&exploration,2005,33(2):21-25.[吴保祥,段毅,王传远,等.泥炭的热模拟实验及其在煤层气研究中的应用[j].煤田地质与勘探,2005,33(2):21-25.]
[4]  wubaoxiang,duanyi,suntao,etal.asimulationstudyonthecompositionandevolutionofthermogeniccoalbedgas[j].naturalgasindustry,2010,30(5):129-132.[吴保祥,段毅,孙涛,等.热成因煤层气组成与演化模拟[j].天然气工业,2010,30(5):129-132.]
[5]  philprp.fossilfuelbiomarkers[m].newyork:elsevier,1985:1-294.
[6]  fanp,lij.characteristicsofthebiomarkersfromnonmarinecrudeoilsinchina:areview[j].chinesejournalofgeochemistry,1991,10(2):131-139.
[7]  fanpu,mabaolin.tarimpetroleumgeology[m].beijing:sciencepress,1990:1-258.[范璞,马宝林.塔里木油气地质[m].北京:科学出版社,1990:1-258.]
[8]  peterske,moldowanjm.interpretingmolecularfossilsinpetroleumandancientsediments[m].prenticehall,inc.,1993:1-236.
[9]  wangchunjiang,luobinjie,zhengguodong,etal.organicgeochemicalcharacteristicsandgenesisofcrudeoilsfromtheturpanbasin[j].actasedimentologicasinica,1993,11(3):72-81.[王春江,罗斌杰,郑国东,等.吐鲁番盆地原油成因及地球化学特征[j].沉积学报,1993,11(3):72-81.]
[10]  huangdifan,qinkuangzong,wangtieguan,etal.oilfromcoal:formationandmechanism[m].beijing:petroleumindustrypress,1995:425.[黄第藩,秦匡宗,王铁冠,等.煤成油的形成和成烃机理[m].北京:石油工业出版社,1995:425.]
[11]  [jpchengkeming,zhaochangyi,suaiguo,etal.astudyofgeologicalandgeochemicalconditionsforcoal-derivedoilandgasformationinturpan-hamibasin[j].petroleumexplorationist,1997,2(2):5-10.[程克明,赵长毅,苏爱国,等.吐哈盆地煤成油气的地质地球化学研究[j].勘探家,1997,2(2):5-10.]
[12]  liuquanyou,liuwenhui,mengqianxiang.geochemicalcharacteristicsofsteranesinsaturatedhydrocabonsfromcoalandexiniteinpyrolysisunderclosedsystems[j].naturalgasgeoscience,2007,18(2):249-253.[刘全有,刘文汇,孟仟祥.热模拟实验中煤岩及显微组分饱和烃甾烷系列化合物有机地球化学特征[j].天然气地球科学,2007,18(2):249-253.]
[13]  mackenzieas,patiencerl,maxwelljr,etal.molecularparametersofmaturationinthetoarcianshales,paris,francei:changesintheconfigurationoftheacyclicisoprenoidalkanes,steranesandtriterpanes[j].geochimicaetcosmochimicaacta,1980,44:1709-1721.
[14]  seifertwk,moldowanjm.useofbiologicalmarkersinpetroleumexploration[j].methodsingeochemistryandgeophysics,1986,24:261-290.
[15]  alomonwr,johnswd.petroleumformingreactions:themechanismandrateofclaycatalyzedfattyaciddecarboxiolation[j].advanceoforganicgeochemistry,1975:157-170.
[16]  vassayevichnb.theroleofclaysinoilformation[j].internetgeologyreview,1976,18(2):125-134.
[17]  [jpbeharf,vandenbrouckem,tangy,etal.thermalcrackingofkerogeninopenandclosedsystems:determinationofkineticparametersandstoichiometriccoefficientforoilandgasgeneration[j].organicgeochemistry,1997,26(5/6):321-339.
[18]  [jpmasuping,hejianqiao,tangwei,etal.theinfluenceofhigh-pressureautoclaveonhydrogenproductduringhydroussimulationexperime[j].actasedimentologicasinica,2003,4(21):713-716.[马素萍,贺建桥,汤渭,等.高压釜对加水模拟实验中氢产物的影响[j].沉积学报,2003,4(21):713-716.]
[19]  xiayanqing,luobinjie.studyonsteroidsintertiarywoodcoalfromnanningbasinbythermal-modellingexperiments[j].experimentalpetroleumgeology,1995,17(3):301-309.[夏燕青,罗斌杰.南宁盆地第三系木质褐煤中甾类化合物热模拟实验研究[j].石油实验地质,1995,17(3):301-309.]
[20]  yingguangguo,zhangbaisheng,jilimin.studyonthermalsimulatedpeat:adiscussiononthegeneticmechanismoftransitionalzonegas[j].actasedimentologicasinica,1995,13(2):44-47.[应光国,张柏生,吉利民.泥炭的热模拟研究—过渡带气形成机理探讨[j].沉积学报,1995,13(2):44-47.]
[21]  zhengjianjing,wendeshun,mengqianxiang,etal.characteristicsofgeochemicalparametersofcoalmeasuressourcerockinthethermalsimulationexperiment[j].naturalgasgeoscience,2003,14(2):134-139.[郑建京,温德顺,孟仟祥,等.煤系烃源岩热模拟演化过程的地球化学参数特征——以准噶尔盆地侏罗系煤系烃源岩为例[j].天然气地球科学,2003,14(2):134-139.]
[22]  [jphuangdifan,lijinchao,zhangdajiang,etal.maturationsequenceofcontinentalcrudeoilsinqaidambasinanditssignificance[j].actapetroeisinica,1989,10(3):1-11.[黄第藩,李晋超,张大江,等.柴达木盆地第三系原油的熟化序列及其在石油资源预测中的重要意义[j].石油学报,1989,10(3):1-11.]

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