摘要
对中东约旦泥灰岩在高演化和低演化阶段的实验结果进行了分析，并探讨了气态烃和非气态烃的演化规律．研究表明，在相同温度热模实验中，干法热解利于甲烷、异构烷烃的产生，抑制烯烃气的生成；加水热解不利于甲烷气的产生，而利于重组分的产生．
The experimental results of the marl (K_2-E) in high and low evolution stages were analyzed, and the variation laws of gaseous hydrocarbons and non-hydrocarbons were researched. The affection of water content and adding or not adding water on various gaseous products was discussed. The results show that dried pyrolysis is favourable for production of methene, isomeric hydrocarbon and alkane. and resistant to production of gaseous alkene.Hydrous pyrolysis is favourable for production of heavy components. and not for gaseous methene..
出处
《石油大学学报（自然科学版）》
CSCD
1996年第2期12-16,共5页
Journal of the University of Petroleum,China(Edition of Natural Science)
关键词
泥灰岩
热模拟
干热解法
气态烃
石油地质
Marl
Thermal simulation
Nonhydrous pyrolysis
Gaseous hydrocarbon
