THE DISCUSSION OF THE ORIGIN OF SULFURETED HYDROGEN IN ASSOCIATED GAS OF DAQING PLACANTICLINE

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  • 1.Jilin University, Changchun 130026, China; 2. Exploration and Development Research Institute of Daqing Oilfield Company Ltd., Daqing 163712, China; 3. Natural Gas Branch of Daqing Oilfield Company Ltd., Daqing 163757, China

Received date: 2005-11-10

  Revised date: 2005-12-30

  Online published: 2006-02-20

Abstract

 There was no H2S in the associated gas of Daqing placanticline before the 80s  of last century. By the middle of 90s, the content of H2S in the associated ga s was detected. At the year of 2002, the content of H-2S reached 200 mg/m3 an d many oil pipes were eroded. By analyzing the 8 samples(H2S gas and FeS powde r) collected from Daqing placanticline, the values of δ34S of 8 samples v ary at the range of +12.73‰~+16.10‰. The isotope feature of this H2S is qui te different compare with the H2S which generated by bacterial sulfate reducti on(BSR) in other oilfield. The H2S maybe associate with the Thermochemical Sul fate Reduction(TSR) in the rock of Permo-Carboniferous in the basement of Songl iao basin.

Cite this article

WANG Lian-sheng;LIU Li;GUO Zhan-qian;MA Zhi-hong;CHI Dong\|hui . THE DISCUSSION OF THE ORIGIN OF SULFURETED HYDROGEN IN ASSOCIATED GAS OF DAQING PLACANTICLINE[J]. Natural Gas Geoscience, 2006 , 17(1) : 51 -54 . DOI: 10.11764/j.issn.1672-1926.2006.01.51

References

[1]  陈荣书. 石油与天然气地质学[M]. 北京:地质出版社,1996.
[2]徐文渊,蒋长安. 天然气利用手册[M].北京:中国石化出版社,2002:36.
[3]吴迪,孟祥春.含硫化亚铁颗粒的乳化原油净化处理方法[J].油气田环境保护,2003,13(1): 37-38.
[4] 戴金星. 中国含硫化氢天然气分布特征、分类及其成因探讨[J].沉积学报,1985,3(4):109-120.
[5] 朱有光,戴金星,张水昌,等.含硫化氢天然气的形成机制及分布规律研究[J].天然气地球科学,2004,15(2):166-170.
[6] 樊广锋,戴金星,戚厚发. 中国硫化氢天然气研究[J]. 天然气地球科学, 1992,3(3):1-10.
[7] 樊广锋,戴金星,戚厚发. 硫化氢天然气生物成因的控制因素[J].石油勘 探与开发,1992,19(增刊):71-76.
[8] 沈平,王先彬,徐永昌.天然气同位素组成及气源对比[J].石油勘探与开发,1982,(6):34-38.
[9] Anisimov L A. Conditions of a biogenic reduction of sulfate in oil -and gas-bearing basins[J]. Geochem Int, 1978,15:63-71.
[10] Machel H G, Krouse H R, Sassen R. Products and distingu ishing  criteria of bacterial and thermochemical sulfate reduction[J]. Applied Geochemistry,1995,10(4):373-389.
[11] 沈平,徐永昌,王晋江,等. 天然气中硫化氢同位素组成及沉积地球化学相[J]. 沉积学报,1997,15(2):216-219.
[12] 张景廉.论石油的无机成因[M].北京:石油工业出版社,2001:1-295.
[13] 余和中,蔡希源,韩守华,等. 松辽盆地石炭—二叠系烃源岩研究[J]. 沉积与 特提斯地质,2003,23(2):62-66.
[14] 庞庆山,方德庆,翟培民,等. 松辽盆地北部基底石炭—二叠系的分布[J]. 大 庆石油学院学报,2002,26(3):92-94.

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