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天然气地球科学 ›› 2011, Vol. 22 ›› Issue (3): 407–414.doi: 10.11764/j.issn.1672-1926.2011.03.407

• 天然气地质学 • 上一篇    下一篇

渤海湾盆地生物气成因类型与成藏条件

高阳, 金强, 帅燕华, 王浩   

  1. 1.中国石油大学地球科学与技术学院，山东 东营 257061;
    2.中国石油勘探开发研究院，北京 100083.
  • 收稿日期:2010-08-28 修回日期:2010-10-23 出版日期:2011-06-10 发布日期:2011-06-10
  • 通讯作者: 高阳swap124@163.com E-mail:swap124@163.com
  • 作者简介:高阳(1982-)，男，山东济南人，博士研究生，主要从事天然气成藏与地球化学研究.
  • 基金资助:

    中国石油天然气股份有限公司科研项目“生物气和低熟气的形成机理、成藏富集规律及资源潜力评价”(编号:2008A-0608)资助

Genetic Types and Accumulation Conditions of Biogas in Bohaiwan Basin

GAO Yang, JIN Qiang, SHUAI Yan-Hua, WANG Hao   

  1. 1.School of Geoscience,China University of Petroleum,Dongying 257061,China; 
    2.Petroleum Exploration and Development Institute,PetroChina,Beijing 100083,China.
  • Received:2010-08-28 Revised:2010-10-23 Online:2011-06-10 Published:2011-06-10

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摘要：

近年来在渤海湾盆地发现了多种成因、零星分布的生物气藏，由于地质条件的复杂性，生物气的成因类型不清、成藏条件不明。为查清生物气的成因类型，分析了生物气的地球化学特征，再结合成藏地质背景，将渤海湾盆地生物气划分为来自烃源岩的生物气和原油降解生物气，前者又包括原生生物气和后生生物气，后者划分为原油厌氧降解生物气和喜氧降解生物气，不同成因的生物气常与热成因气混合成藏。基于上述认识，分析了渤海湾盆地生物气成藏的气源条件、储盖条件、圈闭条件和保存条件，认为渤海湾盆地生物气气源充足、储集空间发育且具有合适的圈闭，盖层封堵能力、东营运动后断层活动性和封闭性成为制约渤海湾盆地生物气成藏的关键。

关键词: 渤海湾盆地, 生物气, 成因类型, 成藏条件, 后生生物气<, p>

Abstract:

Great volumes of biogases have been found in the Bohaiwan basin.But they are small and fragmented distribution,with multi\|genetic types.In this paper,based on gas geochemical characteristic and geological background,the biogases in the Bohaiwan basin are divided into two types of source rock-and hydrocarbon-derived biogases.The source rock-derived biogases are subdivided into primary and secondary biogases,and the hydrocarbon\|derived biogas could be subdivided into anaerobic degradation biogas and aerobic degradation biogases.Complex geological conditions make the genetic types of biogas in the Bohaiwan basin mixing.The coexistence of biogas and thermogenic gas occurs in some of biogas reservoirs.By mean of understanding the conditions of biogas source,reservoir,trap and preservation in the Bohaiwan basin,we consider that the Bohaiwan basin have sufficient source of biogas,developed reservoir and suitable trap.The sealing capacity of cap rock,fault activity after Dongying movement is the key for biogas accumulation.

 

Key words: Bohaiwan basin, Biogas, Genetic types, Accumulation conditions, Secondary biogas.<, p>

中图分类号: 

  • TE122.1+1

［1］Whiticar M J.Carbon and hydrogen isotope systematics of bacterial [JP]formation and oxidation of methane［J］.Chemical Geology,1999,161(1/3):291-314.
［2］Rice D D,Claypool G E.Generation,accumulation,and resource potential of biogenic gas［J］.AAPG Bulletin,1981,65(1):5-25.
［3］Zhang Ying,Li Jian,Hu Chaoyuan,et al.Reservoir formation and resource potretial of biogenic-low maturity gases  in China［J］.Petroleum Exploration and Development,2005,32(4):37-41.［张英,李剑,胡朝元,等.中国生物气—低熟气藏形成条件与潜力分析［J］.石油勘探与开发,2005,32(4):37-41.］
［4］Shuai Yanhua,Zhang Shuichang,Su Aiguo,et al.Preliminary analysis of exploration potential of biogenetic gas［J］.Natural Gas Industry,2006,26(8):1-4.［帅燕华,张水昌,苏爱国,等.生物成因天然气勘探前景初步分析［J］.天然气工业,2006,26(8):1-4.］
［5］Lin Chunming,Li Yanli,Qi Bingwen.Research status and exploration potential of biogenic gas［J］.Journal of Palaeogeography,2006,8(3):317-328.［林春明,李艳丽,漆滨汶.生物气研究现状与勘探前景［J］.古地理学报,2006,8(3):317-328.］
［6］Guo Zeqing,Li Benliang,Zeng Fuying,et al.Distribution characteristics and reservoir formation conditions of the biogenetic gas［J］.Natural Gas Geosciences,2006,17(3):407-413.［郭泽清,李本亮,曾富英,等.生物气分布特征和成藏条件［J］.天然气地球科学,2006,17(3):407-413.］
［7］Li Xianqi,Zhang Shuichang,Zhu Guangyou,et al.Types and research direction of biogenic gas in China［J］.Natural Gas Geosciences,2005,16(4):478-484.［李先奇,张水昌,朱光有,等.中国生物成因气的类型划分与研究方向［J］.天然气地球科学,2005,16(4):478-484.］
［8］Gao Yang,Jin Qiang,Zhu Guangyou.Genetic types and distribution of shallow-buried natural gases［J］.Petroleum Science,2010,7(3):347-354.
［9］Dai Jinxin,Xia Xinyu,Qin Shengfei,et al.Causation of partly reversed orders of δ13C in biogenic alkane gas in China［J］.Oil & Gas Geology,2003,24(1):1-11.［戴金星,夏新宇,秦胜飞,等.中国有机烷烃气碳同位素系列倒转的成因［J］.石油与天然气地质,2003,24(1):1-11.］
［10］Li Zanhao,Li Ji,Xiang Longbin,et al.Degradation of anaerobic bacteria in crude oil and its product property[J].Oil & Gas Geology,1998,19(1):29-34.［李赞豪,李季,向龙斌,等.原油的厌氧细菌降解作用及其产物特征［J］.石油与天然气地质,1998,19(1):29-34.］
［11］Zhang Linye,Li Juyuan,Li Xiangchen,et al.Light hydrocarbon constituents of the biodegradation gas and gas-source correlation[J].Experimental Petroleum Geology,1996,18(1):88-95.［张林晔,李钜源,李祥臣,等.细菌降解气轻烃组成及气源对比［J］.石油实验地质,1996,18(1):88-95.］
［12］Pallasser R J.Recognising biodegradation in gas/oil accumulations through the δ13C compositions of gas components［J］.Organic Geochemistry,2000,31(12):1363-1373.
［13］Masterson W D,Dzou L I P,Holba A G,et al.Evidence for biodegradation and evaporative fractionation in west Sak,Kuparuk and Prudhoe Bay field areas,north slope,Alaska［J］.Organic Geochemistry,2001,32(3):411-441.
［14］Zhu Guangyou,Zhang Shuichang,Zhao Wenzhi,et al.Geochemical characteristics and genetic mechanisms of shallow layer gas in heavy oil areas of China[J].Science in China:Series,D,Earth Science,2007,37(supplementⅡ):80-89.［朱光有,张水昌,赵文智,等.中国稠油区浅层天然气地球化学特征与成因机制［J］.中国科学:D辑,地球科学,2007,37(增刊Ⅱ):80-89.］
［15］Gieg L M,Duncan K E,Suflita J M.Bioenergy productionvia microbial conversion of residual oil to natural gas［J］.Applied and Environmenral Microbiology,2008,74(10):3022-3029.
［16］Dariusz Strapoc,Maria M,Schimmelmann A S,et al.Variability of geochemical properties  in a microbially dominated coalbed gas system from the eastern margin of the Illinois basin,USA［J］.International Journal of Coal Geology,2008,76(1/2):98-110.
［17］Jin Q,Cheng F Q,Su A G,et al.Biogas charging and dissipating process and its accumulation in the Sebei gasfield,Qaidam basin,China[J].Science in China:Series  D,Earth Sciences,2008,51:36-44.
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