高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

吐哈盆地水溶气组分与同位素特征形成机理及意义探讨

张晓宝,  徐永昌,  刘文汇,  沈平,  吉利明,  马立元

downloadPDF
文章导航 > 沉积学报  > 2002 >  20(4): 705-709
张晓宝, 徐永昌, 刘文汇, 沈平, 吉利明, 马立元. 吐哈盆地水溶气组分与同位素特征形成机理及意义探讨[J]. 沉积学报, 2002, 20(4): 705-709.
引用本文: 张晓宝, 徐永昌, 刘文汇, 沈平, 吉利明, 马立元. 吐哈盆地水溶气组分与同位素特征形成机理及意义探讨[J]. 沉积学报, 2002, 20(4): 705-709.
shu
ZHANG Xiao bao, XU Yong-chang, LIU Wen hui, SHEN Ping, JI Li ming, MA Li yuan. A Discussion of Formation Mechanism and Its Significance of Characteristics of Chemical Composition and Isotope of Water-dissolved Gas in Turpan-Hami Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 705-709.
Citation: ZHANG Xiao bao, XU Yong-chang, LIU Wen hui, SHEN Ping, JI Li ming, MA Li yuan. A Discussion of Formation Mechanism and Its Significance of Characteristics of Chemical Composition and Isotope of Water-dissolved Gas in Turpan-Hami Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 705-709.
shu

吐哈盆地水溶气组分与同位素特征形成机理及意义探讨

  • 中国科学院兰州地质研究所气体地球化学国家重点实验室,兰州,730000

基金项目: 国家自然科学基金项目(批准号:49972051,40172053)和中国科学院资源环境领域知识创新工程重大(重要方向)项目(KZCX2-111)资助
详细信息
    作者简介:

    张晓宝 男 1958年出生 博士研究员 天然气地质地球化学

  • 中图分类号: P593

A Discussion of Formation Mechanism and Its Significance of Characteristics of Chemical Composition and Isotope of Water-dissolved Gas in Turpan-Hami Basin

  • State Key Laboratory of Gas Geochemistry, Lanzhou Institute of Geology, Chinese Academy of Sciences, Lanzhou 730000

    摘要
  • 摘要: 测量了吐哈盆地 6个水溶气样品的组分和碳同位素值,并通过与盆地天然气的对比,探讨了水溶气组分及碳同位素特征形成机理及其应用的可能性。水溶气基本受制约于烃类气体溶解度的特征,与盆地天然气应属同源,但二者也存在明显的差异,如C1/C1～ 5值水溶气应大于天然气,实际反而较小,甲烷同系物碳同位素均较天然气富集-6 C。作者认为这些特征的形成与水溶气的溶解量小于扩散运移量相关,并认为水溶气与天然气组分和同位素差异的大小可用于探讨采样层位与天然气动态成藏体系关联的紧密程度。
    Abstract: The chemical composition and carbon isotope of the six water-dissolved gas samples in the Turpan- Ha-mi basin are measured and the characteristic of formation mechanism and the possibility of application of the com-position and isotope to natural gas geology are discussed by comparison with the natural gas in the basin. The char-acteristic of the composition of the water-dissolved gas hydrocarbons is mainly controlled by dissolution degree of the hydrocarbons. They are derived from the same source rocks as the natural gases, but they are different from the natural gases, e. g., the C 1/C 1 ～ 5 of the water-dissolved gas should be higher than that of the natural gas, but in fact it is lower; the homologue of the water-dissolved gas CH 4 is enriched in13C than that of the natural gas. the above characteristic was thought to be related with that the dissolved content of the natural gases in the dis-solved-water was less than the migrated content. It is considered that the differences of the composition and isotope between the water-dissolved gas and the natural gasindicate the relation of between the sampling membersand nat-ural gas dynamics pool-forming system.
    • HTML全文
    • 参考文献(13)
  • [1] 陈荣书主编. 天然气地质学[M]. 北京:石油工业出版,1989. 161～164[Chen Rongshu ed. Natural gas geology[M]. Beijing:Petroleum Industry Press, 1989.161～164]
    [2] 王昌桂, 程克明, 徐永昌.吐哈盆地煤成烃地球化学[M]. 北京:科学出版社,1998. 191～230[Wang Changgui, Cheng Keming, Xu Yongchang. Geochemistry of coal-derived hydrocarbons in the Turpan-Hami basin[M]. Beijing:Science Press,1998.191～230]
    [3] 袁明生, 王武和, 曾晓明. 吐哈盆地成油条件及勘探方向[A]. 见:王昌桂,路锡良主编. 吐哈盆地石油地质研究论文集[C]. 北京: 石油工业出版社, 1995. 75～83[Yuan Mingsheng,Wang Wuhe, Zeng Xiaoming. Petroleum formation conditions and exploration direction in the Turpan-Hami basin[A]. In:Wang Changgui,Lu Xiliang, eds. Works of petroleum gelogical research in the Turpan-Hami basin[C].Beijing: Petroleum Industry Press, 1995.75～83]
    [4] 程克明主编. 吐哈盆地油气生成[M]. 北京:石油工业出版社,1994. 131～169[Cheng Keming ed. Petroleum formation in the Turpan-Hami Basin[M]. Beijing: Petroleum Industry Press,1994.131～169]
    [5] 徐永昌, 刘文汇, 沈平. 含油气盆地油气同位素地球化学研究概述[J]. 沉积学报,2001, 19(1): 161～168[Xu Yongchang,Liu Wenhu,Shen Ping. An outline of petroleum isotopic geochemical research in petroleum-bearing Basins[J]. Acta Sedimentologica Sinica,2001,19(1):161～168]
    [6] 郝石生, 张振英. 天然气在地层中的溶解度变化特征及地质意义[J]. 石油学报,1993,14(2):12～22[Hao Shisheng, Zhang Zhenying. Varian characteristics and geological significance of natural gas solubility in strata[J].Acta Petrolei Sinica,1993,14(2):12～22]
    [7] Coleman D D, Risati J B, Schoell M. Fractionation of carbon and hydrogen isotopes by methane-oxidizing bacteria[J]. Geochimica et Cosmochimia Acta, 1981,45: 1 033～1 037
    [8] 戴金星, 裴锡古, 戚厚发. 中国天然气地质学[M]. 北京:石油工业出版社,1995. 42～43[Dai Jinxing,Pei Xigu, Qi Houfa. Natural gas geology in China[M]. Beijing:Petroleum Industry Press, 1995. 42～43]
    [9] Douglas A G, ed. Advances in Organic Geochemistry [C]. Oxford: Pergamon, 1979. 725～732
    [10] 戴金星, 王庭斌, 宋岩, 张洪年, 徐永昌, 张启明. 中国大中天然气田形成条件与分布规律[M]. 北京:地质出版社,1997. 47～57[Dai Jinxing, Wang Tingbin, Song Yan, Zhang Hongnian, Xu Yongchang, Zhang Qiming. Formation conditions and Distibution of large to mediate sized natural gas fields in China[M]. Beijing:Geological Publishing House, 1997. 47～57]
    [11] 王涛主编.中国天然气地质理论基础与实践[M].北京:石油工业出版社,1997.190～236[Wang Tao ed.Theoreticae foundation and practice of natural gas geology in China[M]. Beijing:Petroleum Industry Press,1997. 190～236]
    [12] Prinzhofer A, Pernaton é. Isotopically light methane in natural gas: bacterial imprint or diffusive fractionation?[J]. Chemical Geology, 1997, 142: 193～200
    [13] Prinzhofer A, Mello M R, Takaki T. Geochemical characterization of natural gas: a physical multivariable and its applications in maturity and migration estimates[J]. AAPG Bulletin, 2000, 84: 1 152～1 17
    • 相关文章
    • 施引文献
  • 资源附件(0)
  • 加载中
WeChat 点击查看大图
计量
  • 文章访问数:  213
  • HTML全文浏览量:  19
  • PDF下载量:  15
  • 被引次数: 0
出版历程
  • 收稿日期:  2002-01-14
  • 修回日期:  2002-03-17

目录

    吐哈盆地水溶气组分与同位素特征形成机理及意义探讨

    • 中国科学院兰州地质研究所气体地球化学国家重点实验室,兰州,730000
      • 基金项目:  国家自然科学基金项目(批准号:49972051,40172053)和中国科学院资源环境领域知识创新工程重大(重要方向)项目(KZCX2-111)资助
      作者简介:

      张晓宝 男 1958年出生 博士研究员 天然气地质地球化学

    • 收稿日期: 2002-01-14
    • 修回日期: 2002-03-17

    • 中图分类号: P593

    摘要: 测量了吐哈盆地 6个水溶气样品的组分和碳同位素值,并通过与盆地天然气的对比,探讨了水溶气组分及碳同位素特征形成机理及其应用的可能性。水溶气基本受制约于烃类气体溶解度的特征,与盆地天然气应属同源,但二者也存在明显的差异,如C1/C1～ 5值水溶气应大于天然气,实际反而较小,甲烷同系物碳同位素均较天然气富集-6 C。作者认为这些特征的形成与水溶气的溶解量小于扩散运移量相关,并认为水溶气与天然气组分和同位素差异的大小可用于探讨采样层位与天然气动态成藏体系关联的紧密程度。

    English Abstract

    张晓宝, 徐永昌, 刘文汇, 沈平, 吉利明, 马立元. 吐哈盆地水溶气组分与同位素特征形成机理及意义探讨[J]. 沉积学报, 2002, 20(4): 705-709.
    引用本文: 张晓宝, 徐永昌, 刘文汇, 沈平, 吉利明, 马立元. 吐哈盆地水溶气组分与同位素特征形成机理及意义探讨[J]. 沉积学报, 2002, 20(4): 705-709.
    shu
    ZHANG Xiao bao, XU Yong-chang, LIU Wen hui, SHEN Ping, JI Li ming, MA Li yuan. A Discussion of Formation Mechanism and Its Significance of Characteristics of Chemical Composition and Isotope of Water-dissolved Gas in Turpan-Hami Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 705-709.
    Citation: ZHANG Xiao bao, XU Yong-chang, LIU Wen hui, SHEN Ping, JI Li ming, MA Li yuan. A Discussion of Formation Mechanism and Its Significance of Characteristics of Chemical Composition and Isotope of Water-dissolved Gas in Turpan-Hami Basin[J]. Acta Sedimentologica Sinica, 2002, 20(4): 705-709.
    shu

      全文HTML

    参考文献 (13)

    目录

      /

      返回文章
      返回

      友情链接

      期刊在线

      联系我们

      • 网站版权 © 2011《沉积学报》编辑部
      • 地址: 兰州市天水中路8号
      • 邮编: 730000   Tel:（0931）8264231
      • 陇ICP备2021001824号-28
      • 甘公网安备 62010202000673号
      关注微信公众号

      Email alert

      RSS

      系统由 北京仁和汇智信息技术有限公司 设计集成    百度统计

      x 关闭 永久关闭