天然气地球科学 ›› 2010, Vol. 21 ›› Issue (3): 513–517.doi: 10.11764/j.issn.1672-1926.2010.03.513

• 煤层气 • 上一篇    下一篇

晋城煤层气井产能的地质控制因素分析

张典坤, 王生维, 李梦溪, 张建国, 杨青雄, 唐江林   

  1. 1.中国地质大学(武汉)资源学院,湖北 武汉 430074;
    2.中国石油山西煤层气分公司,山西 晋城 048026
  • 收稿日期:2009-10-26 修回日期:2009-12-29 出版日期:2010-06-10 发布日期:2010-06-10
  • 通讯作者: 张典坤fcxzdk@163.com. E-mail:fcxzdk@163.com.
  • 作者简介:张典坤(1986-),男,山东聊城人,硕士研究生,主要从事煤及煤层气开发地质研究.
  • 基金资助:

    国家重大专项“大型油气田与煤层气开发”子课题“煤层气井生产过程中煤储层气水相渗动态变化规律研究”项目(编号:2008ZX05034-002);国家自然科学基金面上项目“晋城煤储层大裂隙系统研究” (编号:40672099);国家深部煤层“973”项目专题“地质动力、构造样式对深部煤层瓦斯赋存的控制作用”(编号:2006CB202204);国家 “863”课题“晋城煤层气探测与增产技术研究”(编号:2006AA06Z232)联合资助.

Geologically Controlling Factors on Coalbed Methane (CBM) Productivity in Jincheng

ZHANG Dian-Kun, WANG Sheng-Wei, LI Meng-Xi, ZHANG Jian-Guo, YANG Qing-Xiong, TANG Jiang-Lin   

  1. 1. The Faculty of Resources,China University of Geosciences(Wuhan), Wuhan 430074,China;
    2. Shanxi Branch of PetroChina Coalbed Methane Company Limited,Jincheng 048026,China
  • Received:2009-10-26 Revised:2009-12-29 Online:2010-06-10 Published:2010-06-10

摘要:

以研究煤储层物性非均质性,识别煤层气藏类型为切入点,分析产能与煤层气藏类型之间的关系,发现高产井(>3000 m3/d)主要分布在富集高渗煤层气藏内,中产井(1500~3000 m3/d)主要分布在高饱和度低渗透煤层气藏内,而高渗透率低饱和度煤层气藏和低渗透率中低饱和度煤层气藏这2类气藏,受渗透率和含气量制约,其煤层气井产能一般偏低。

关键词: 晋城煤层气区, 煤层气井产能, 煤层气藏类型, 地质控制因素

Abstract:

According to physical heterogeneity of coal seam as gas reservoir and type of coalbed gas reservoir, we discuss the relationship between types of coalbed gas reservoir and gas productivity, and find out that the CBM well with high gas productivity (>3 000 m3/d) is distributed in the high permeability coalbed methane reservoir; the well with middle gas productivity (1 500~3 000 m3/d) is in the high saturation and low permeability coalbed methane reservoir. But two types of coalbed reservoirs with high permeability and low saturation, and low permeability and high saturation, respectively, are restricted by permeability and gas content, with low gas productivity.

Key words: Jincheng CBM zone, CBM well productivity, CBM reservoir types, Geologically controlling factors.

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