天然气地球化学

干酪根类型及生烃潜力确定新方法

展开
  • 1.中国科学院地质与地球物理研究所油气资源研究重点实验室,甘肃省油气资源研究重点实验室,甘肃兰州 730000;
    2.中国科学院大学,北京 100049;3.新疆油田公司实验检测研究院,新疆 克拉玛依 834000
熊德明(1984-),男,四川大竹人,博士研究生,主要从事天然气地质学和油气地球化学研究. E-mail:xiongdeming2004@126.com.

收稿日期: 2013-06-20

  修回日期: 2013-09-06

  网络出版日期: 2014-06-10

基金资助

中国科学院知识创新工程重要方向项目(编号:KZCX2-EW-104);中国科学院西部行动计划项目(编号:KZCX2-XB3-12)联合资助.
〖HTH〗作者简介〖HTSS〗:

New Method for the Determination of Kerogen Type and the Hydrocarbon Potential

Expand
  • 1.Key Laboratory of Petroleum Resources Research,Institute of Geology and Geophysics,Chinese Academy of Sciences,Gansu Provincial Key Laboratory of Petroleum Resources,Lanzhou  730000,China;
    2.University of Chinese Academy of Sciences,Beijing  100049,China;
    3.Xinjiang Oilfield Company Experiment and Detection Research Institute,Karamay 834000,China

Received date: 2013-06-20

  Revised date: 2013-09-06

  Online published: 2014-06-10

摘要

干酪根是由千差万别的原始有机物质经过生化作用和物化作用改造而成,它们彼此之间的化学组成、内部结构、形状及大小各不相同。对于干酪根类型的划分,目前存在很多方法,如三分法、四分法、五分法和“X”图解等,最常用的是Tissot的三分法。虽然有这么多的分类方法,但是无法对干酪根类型进行准确定量分析。因此,在四型分类法的基础上提出了新的定量分析方法。拟合“Van Kerevenlen”图版上4种类型曲线方程,然后计算目标点到4种类型曲线的距离,从而确定干酪根类型(到哪条曲线的距离值最小,目标点就属于该型的干酪根)。采用新建立的干酪根生烃潜力指数确定干酪根的生烃潜力。通过对比分析干酪根类型和生烃潜力的计算结果,研究发现,新建立数值化方法的结果和生烃潜力计算结果基本吻合,说明新的数值化类型确定方法是正确的、可靠的。并且具有计算速度快、精度高、计算范围大、计算机操作方便等多方面的特点。

本文引用格式

熊德明,马万云,张明峰,吴陈君,妥进才 . 干酪根类型及生烃潜力确定新方法[J]. 天然气地球科学, 2014 , 25(6) : 898 -905 . DOI: 10.11764/j.issn.1672-1926.2014.06.898

Abstract

Kerogen is substances of sedimentary rock that is neither soluble in alkaline aqueous solvents nor in common organic solvents solid organic substances.It is composed of the original organic matter that are vastly different biochemical effects and role of transformation from the physical,chemical composition,they have internal structure,shape,size varies.For the division of kerogen types,there are now a lot of methods,such as three types,four types,five types,and “X” diagrams,etc.The most commonly used is the Tissot three types.Although there are so many classification methods,but it cannot be accurately kerogen quantitative analysis.Therefore,based on four types,this paper proposed new method for quantitative analysis.With “Van Kerevenlen” plate,curve equation will can be got four types curves,and then calculate the target point to the distance of four types of curves to determine the type of kerogen (where the value of the minimum distance curve,the target point belongs to this type of kerogen).And then,with new formula,the Hydrocarbon potential of source rock is gotten.By comparing the results,it is found that the result of new numerical method agree with the result of the hydrocarbon generation potential,and the numerical method for determining the type is correct and reliable.And it has many characteristics,such as fast calculation speed,high precision calculation range,easy to operate computers and so on.

参考文献

[1]Tissot B,Durand B.Influence of natures and diagenesis of organic matter in formation of petroleum[J].AAPG Bulltin,1974,58(3):438-459.
[2]Welte D H,Tissot B P.Petroleum Formation and Occurrence[M].Berlin:Springer-Verlag,1984.
[3]Huang Fei,Xin Mao′an.The Geochemical Evaluation Method of Terrestrial Source Rocks[S].SY-T 5735-1995.Beijing:Petroleum Industry Press,1995.[黄飞,辛茂安.陆相烃源岩地球化学评价方法[S].SY-T 5735-1995.北京:石油工业出版社,1995.]
[4]Huang Difan,Li Jinchao.X-diagram of kerogen classification and the characters of kerogen of standard humic type[J].Geochimica,1982,(1):21-30.[黄第藩,李晋超.干酪根类型划分的X图解[J].地球化学,1982,(1):21-30.]
[5]Lu Shuangfang,Pang Xiongqi,Li Taiming,et al.A discussion on the digitalization of kerogen types[J].Natural Gas Industry,1986,3(6):17-23.[卢双舫,庞雄奇,李泰明,等.干酪根类型数值化的探讨[J].天然气工业,1986,3(6):17-23.]
[6]Durand B .Kerogen:Insoluble Organic Matter from Sedimentary Rocks[M].Paris:Technip,1980.
[7]Fu Jiamo,Qin Kuangzong.Kerogen Geochemistry[M].Guangzhou:Guangdong Scientific Publication Press,1995:1-292.[傅家漠,秦匡宗.干酪根地球化学[M].广州:广东科技出版社,1995:1-292.]
[8]Wang Qijun,Chen Jianyu.Petroleum Geochemistry[M].Wuhan:China University of Geosciences Press,1988.[王启军,陈建渝.油气地球化学[M].武汉:中国地质大学出版社,1988.]
[9]Du Yingchun.Practical Numerical Analysis[M].Beijing:Chemical Industry Press,2007.[杜迎春.实用数值分析[M].北京:化学工业出版社,2007.]
[10]Guo Zhizhong.College Mathematics[M].Beijing:Tsinghua University Press,2013.[郭治中.高等数学[M].北京:清华大学出版社,2013.]
[11]Lu Shuangfang,Zhang Min.Petroleum Geochemistry[M].Beijing:Petroleum Industry Press,2007.[卢双舫,张敏.油气地球化学[M].北京:石油工业出版社,2007.]
[12]Baskin D K.Atomic H/C ratio of kerogen as an estimate of thermal maturity and organic matter conversion[J].Liu Quanyou,Translation.Natural Gas Geoscience,2002,13(5/6):41-49.[Baskin D K.利用干酪根H/C比评价烃源岩热成熟度与生烃潜力[J].刘全有译.天然气地球科学,2002:13(5/6):41-49.]
[13]Chen Xiaoming,Li Jianzhong,Zheng Min,et al.Kerogen solution theory and its exploratory application in shale gas assessment[J].Natural Gas Geoscience,2012,23(1):14-18.[陈晓明,李建忠,郑民,等.干酪根溶解理论及其在页岩气评价中的应用探索[J].天然气地球科学,2012:23(1):14-18.]

文章导航

/