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1岩石解析气实验新方法对气源对比研究的突破显示文摘经多年反复实验和改进,建立了高真空条件下、球磨机碎样、不经水介质直接收集解析气的装置和方法,从而最大限度地排除大气污染、粉碎热解以及经水介质集气等各种干扰因素,使所获解析气中的烃类气体体积百分含量大幅度提高,最高可达80%以上,碳同位素系列可实测至δ13C。~δ13C5.利用新建立的装置进行初步研究,结果表明:(1)利用烃源岩解析气的乙烷碳同位素组成判识烃源岩类型,与应用烃源岩有机地球化学参数判识结果完全一致,说明利用天然气的乙炕碳同位素组成作为判识母质类型的参数是可行的;(2)利用烃源岩解析气甲烷碳同位素组成计算的烃源岩热演化程度R0值与烃源岩实测镜质体反射率吻合极好,证实了利用统计学方法得到的天然气甲烷碳同位素组成与热演化程度的对应关系是可靠的;(3)首次建立了天然气气一源直接对比方法,运用自然源岩样品解析气的实测δ13C1和实测R0值建立的lgR0vsδ13C1表达式,为油气勘探区进行精细油气源对比创造了条件.史宝光 沈平 王晓锋 郑建京 2013科学通报2013,58,5:4
2Groundbreaking gas source rock correlation research based on the application of a new experimental approach for adsorbed gas显示文摘Many years of experimentation have led to the development and improvement of equipment and methods used to make gas source rock correlations.By crushing samples using a ball mill and directly collecting adsorbed gases in the absence of aqueous media under high vacuum conditions,most possible interference factors,such as atmospheric pollution,crushing-induced pyrolysis,and gas collection by aqueous media are eliminated.This greatly enhances the volume percentage of hydrocarbon gas in the acquired adsorbed gases,with maxima up to more than 80%.The actual measurement of carbon isotopic series can be carried out to such an extent as to be δ13C1-δ13C5.A preliminary study using newly established equipment and methods has indicated the following.(1) The carbon isotopic composition of ethane in adsorbed gases on hydrocarbon source rocks can be used to distinguish the types of source rocks.This is consistent with results obtained by using organic geochemical parameters for source rocks,and illustrates that it is highly feasible to use the carbon isotopic composition of ethane in natural gases as a parameter for distinguishing the types of source rocks.(2) The thermal evolution degree(Ro) of hydrocarbon-source rocks calculated in terms of the carbon isotopic composition of methane in adsorbed gases on hydrocarbon source rocks agrees well with the vitrinite reflectance actually measured in the source rocks.This confirms the reliability of the relationship between the carbon isotopic composition of methane in natural gases and the thermal evolution degree determined using statistics.(3) Finally,a direct gas source correlation method for natural gases has been established,and the expression of log Ro vs.δ13C1 established in terms of actually measured δ13C1 values of methane in absorbed gases.Ro values of hydrocarbon source rocks have been established as well,thus creating favorable conditions for precise oil-and-gas source correlations in exploration areas.SHI BaoGuang SHEN Ping WANG XiaoFeng ZHEN JianJing 2012Chinese Science Bulletin2012,57,36:2
3Determination of carbon isotopic composition of individual light hydrocarbons evolved from pyrolysis of source rocks by using GC-IRMS显示文摘The carbon isotopic composition of individual light hydrocarbons generated from source rocks that had been pyrolysed in vacuum glass tube were determined by using the GC-IRMS techniques. The results indicate that abundant CO2 in the pyrolysates has a remarkable effect on the determination of CH4δ13C. Running cryogenically with an initial temperature of -40℃ can effectively eliminate the effect. In addition, it conduces to measuring the δ13C of C2+ hydrocarbons by increasing the injection volume and/or absorbing CO2 with the solution of sodium hydroxide. The above measures will help to get the carbon isotopic composition of C1-C7 components, which is of great significance for gas/source rock correlation and for study on the genesis of natural gas.GENG Ansong XIONG Yongqiang 2000Chinese Science Bulletin2000,45,S1:0
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