天然气中丁烷地球化学特征及应用
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:The geochemical characteristics of butane and its application
  • 作者:王鹏 ; 沈忠民 ; 何崇康 ; 王君泽 ; 黄飞 ; 潘树林 ; 尹帅
  • 英文作者:Wang Peng;Shen Zhong-min;He Chong-kang;Wang Jun-ze;Huang Fei;Pan Shu-lin;Yin Shuai;College of Mining and Safety Engineering,Yibin University;State Key Laboratory of Oil and Gas Reservoir Geology and Exploration,Chengdu University of Technology;Changqing Oilfield Company,PetroChina;School of Energy Resources,China University of Geosciences;
  • 关键词:丁烷地球化学特征 ; iC_4/nC_4 ; 生物降解 ; 运移示踪 ; 天然气成因
  • 英文关键词:Geochemical characteristics of butane;;iC_4/nC_4;;Biodegradation;;Trace migration;;Natural gas origin
  • 中文刊名:TDKX
  • 英文刊名:Natural Gas Geoscience
  • 机构:宜宾学院资源与环境工程学院;油气藏地质及开发工程国家重点实验室(成都理工大学);中国石油长庆油田分公司;中国地质大学能源学院;
  • 出版日期:2017-04-10
  • 出版单位:天然气地球科学
  • 年:2017
  • 期:v.28;No.173
  • 基金:国家自然科学基金(编号:41172119);; 宜宾学院科研启动项目(编号:2015QD09);; 宜宾市科技局重点科技项目联合资助
  • 语种:中文;
  • 页:TDKX201704007
  • 页数:10
  • CN:04
  • ISSN:62-1177/TE
  • 分类号:39-48
摘要
在分析内因(有机质类型、有机质成熟度)与外因(生物降解、运移)对天然气中丁烷地球化学特征影响的基础上,探讨了丁烷在天然气研究中的应用。首先明确了内因、外因对丁烷地球化学特征的影响:腐殖型有机质生成的煤型气iC_4/nC_4值、δ~(13)C_4值均高于腐泥型有机质生成的油型气;iC_4/nC_4值随成熟度增加而降低,且在成熟阶段快速降低、进入高成熟阶段后缓慢降低;微生物降解会使得天然气中iC_4/nC_4值增大,且降解作用越强iC_4/nC_4值越大。而目前有关运移是否会影响iC_4/nC_4值及如何影响iC_4/nC_4值还存在较大争议。发现丁烷在天然气生物降解、天然气成因、天然气成熟度等研究中都有较好的应用:iC_4/nC_4值能有效判识天然气是否发生生物降解,生物降解气iC_4/nC_4值大于2、普遍大于3,iC_4/nC_4值大于3可以判定天然气发生生物降解,未降解气iC_4/nC_4值小于3、普遍小于2,iC_4/nC_4值小于2可以判定天然气未发生生物降解;iC_4/nC_4值、δ~(13)C_4值均能有效判识受外因影响较小天然气的成因,其判别标准分别为油型气iC_4/nC_4值小于0.8、煤型气iC_4/nC_4值大于0.8与油型气δ~(13)C_4值小于-26‰、煤型气δ~(13)C_4值大于-26‰;iC_4/nC_4值对天然气成熟度判识也有重要作用。iC_4/nC_4值示踪天然气运移存在多解性,其有效性也明显不如其他指标,应慎重选择其示踪天然气运移。
        Based on comprehensive analysis of internal factors(i.e.,organic matter type and organic matter maturity) and external factor(i.e.,biodegradation and migration) on characteristics of butane,the application of geochemical characteristics of butane was studied.The paper cleared the effects of internal factors on characteristics of butane.The coal type gas derived from humic organic matters, "which had the higher iC_4/nC_4 ratio and δ~(13) C_4 value than the oil type gas from sapropellic organic matters.The iC_4/nC_4 ratio decreased with the increase of maturity,and it decreased quickly at the mature stage and slowly at the highmature stage.The iC_4/nC_4 ratio would increase as the biodegradation increases,and the stronger the biodegradation,the higher the iC_4/nC_4 ratio.Whether the migration would affect the iC_4/nC_4 ratio and how it affects,both are uncertain.It is found that the butane can provide information about the biodegradation,genesis and maturity of natural gas.The iC_4/nC_4 ratio can be used to effectively determine the gas is biodegraded or normal.The iC_4/nC_4 ratios of biodegraded gas were higher than 2 and most of them were higher than 3.If the iC_4/nC_4 ratio is higher than 3,the natural gas is biodegraded gas.The iC_4/nC_4 ratios of normal gas were lower than 3 and most of them were lower than 3,if the iC_4/nC_4 ratio is lower than 2,the natural gas is normal gas.For the gas suffered less influence by external factor,the oil type " which has iC_4/nC_4 ratios lower than 0.8 and δ~(13) C_4 value lower than-26‰,the coal type gas which has iC_4/nC_4 ratios higher than 0.8 and δ~(13) C_4 value higher than-26‰.The iC_4/nC_4 ratios can help analyze the maturity of natural gas.For the iC_4/nC_4 as trace index,there are still more controversial and poor effectiveness,and should be carefully to choose it for tracing migration.
引文
[1]Dai Jinxing.Significance of the study on carbon isotopes of alkane gases[J].Natural Gas Industry,2011,31(12):1-6.[戴金星.天然气中烷烃气碳同位素研究的意义[J].天然气工业,2011,31(12):1-6.]
    [2]Dai Jinxing,Pei Xigu,Qi Houfa.Geology of Natural Gas in China[M].Beijing:Petroleum Industry Press,1992.[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,1992.]
    [3]Liu Wenhui,Xu Yonghang.Genetic indicators for natural gases[J].Acta Sedimentologica Sinica,1996,14(1):110-115.[刘文汇,徐永昌.天然气成因类型及判别标志[J].沉积学报,1996,14(1):110-115.]
    [4]Zhang Houfu,Lv Fuliang.Genetic indicators for Natural Gas(taking Bohaiwan basin as an example)[C]//Geological Research Papers on the Natural Gas by Editorial Board.The Proceedings of Studying Natural Gas Geology.Beijing:Petroleum Industry Press,1989:90-100.[张厚福,吕福亮.天然气成因类型及其识别标志(以渤海湾盆地为例)[C]//天然气地质研究论文集编委会编.天然气地质研究论文集.北京:石油工业出版社,1989:90-100.]
    [5]Wang Shiqian.Geochemical characteristics of Jurassic-Sinian gas in Sichuan Basin[J].Natural Gas Industry,1994,14(6):1-5.[王世谦.四川盆地侏罗系-震旦系天然气的地球化学特征[J].天然气工业,1994,14(6):1-5.]
    [6]Miao Zhongying,Chen Jianfa,Guo Jianjun,et al.Geochemistical characteristics of butane gas in Tarim Basin[J].Journal of China University of Mining and Technology,2011,40(4):592-597.[苗忠英,陈践发,郭建军,等.塔里木盆地天然气中丁烷的地球化学特征[J].中国矿业大学学报,2011,40(4):592-597.]
    [7]Boreham C J,Edwards D S.Abundance and carbon isotopic composition of neo-pentane in Australian natural gases[J].Organic Geochemistry,2008,39(5):550-566
    [8]Katza B J,Narimanovb A,Huseinzadehc R.Significance of microbial processes in gases of the South Caspian basin[J].Marine and Petroleum Geology,2002,19(6):783-796.
    [9]Li Guangzhi,Wu Xianghua.The petroleum geological significance of somerization ratesφiC4nC4andφiC5/φnC5[J].Geophysical&Geochemical Exploration,2002,26(2):135-139.[李广之,吴向华.异构比φiC4/φnC4和φiC5/φnC5的石油地质意义[J].物探与化探,2002,26(2):135-139.]
    [10]Lu Jialan,Fu Jiamo,Zhang Huizhi,et al.Study on simulation of natural gas migration in different conditions[J].Oil&Gas Geology,1991,12(2):153-160.[卢家烂,傅家谟,张惠之,等.不同条件下天然气运移影响的模拟实验研究[J].石油与天然气地质,1991,12(2):153-160.]
    [11]Chen Anding,Li Jianfeng.Study on geochemical index during natural gas migration[J].Natural Gas Geoscience,1994,24(5):38-67.[陈安定,李剑锋.天然气运移的地球化学指标研究[J].天然气地球科学,1994,24(5):38-67.]
    [12]Fu Jiamu,Liu Dehan.The Migration,Eservoir Conditions and Sealing Condition of Natural Gas[M].Beijing:Science Press,1992:80-85.[傅家谟,刘德汉.天然气运移、储集及封盖条件[M].北京:科学出版社,1992:80-85.]
    [13]Wang Tingdong,Yang Yuancong.Geological chromatograph and natural gas migration in Upper Triassic in the central part of Sichuan[J].Natural Gas Industry,1986,6(1):15-20.[王廷栋,杨远聪.地质色层作用与川中上三叠统天然气的运移[J].天然气工业,1986,6(1):15-20.]
    [14]Wang Peng,Liu Sibing,Shen Zhongmin,et al.Mechanism and effectiveness of geochemical index trace natural gas migration:A case study of Jurassic natural gas in western Sichuan Depression[J].Natural Gas Geoscience,2015,26(6):1147-1155.[王鹏,刘四兵,沈忠民,等.地球化学指标示踪天然气运移机理及有效性分析---以川西坳陷侏罗系天然气为例[J].天然气地球科学,2015,26(6):1147-1155.]
    [15]Hu Anping,Li Jian,Zhang Wenzheng,et al.Chemical characteristics and origin of gases from the Upper,Lower Paleozoic and the Mesozoic reservoirs in the Ordos Basin,China[J].Science in China:Series D,2007,37(supplement2):157-166.[胡安平,李剑,张文正,等.鄂尔多斯盆地上、下古生界和中生界天然气地球化学特征及成因类型对比[J].中国科学:D辑,2007,37(增刊2):157-166.]
    [16]Huang Futang.Geochemical characteristics of natural gas in northern Songliao Basin[J].Natural Gas Geoscience,1992,3(3):15-19.[黄福堂.松辽盆地北部不同成因类型天然气地球化学特征[J].天然气地球科学,1992,3(3):15-19.]
    [17]James A T,Burns B J.Microbial alteration of subsurface natural gas accumulations[J].The American Association of Petroleum Geologists Bulletin,1984,68(8):957-960.
    [18]Zhao Hongjing.The Origin of Gas in Taibei Depression Tupan-Hami Basin and Gas-Source Correlation[M].Beijing:Petroleum Industry Press,2013:115-123.[赵红静.吐哈盆地台北凹陷天然气成因及气源对比[M].北京:石油工业出版社,2013:115-123.]
    [19]Sun Hao,Zhang Min,Li Sumei.Geochemical characteristics and genetic analysis of shallow-buried natural gas in south Songliao Basin[J].Geoscience,2013,27(5):1173-1179.[孙浩,张敏,李素梅.松辽盆地南部浅层天然气地球化学特征及其成因分析[J].现代地质,2013,27(5):1173-1179.]
    [20]Gao Yuan,Wang Yongli,Zheng Guodong.Geochemical characteristics of natural gas from Dushanzi mud volcano in Junggar Basin,Xinjiang[J].Acta Geoscientica Sinica,2012,33(6):989-994.[高苑,王永莉,郑国东,等.新疆准噶尔盆地独山子泥火山天然气地球化学特征[J].地球学报,2012,33(6):989-994.]
    [21]Prinzhofer A,Santos Neto E V,Battani Anne.Coupled use of carbon isotopes and noble gas isotopes in the Potiguar Basin(Brazil):Fluids migration and mantle influence[J].Marine and Petroleum Geology,2010,27(6):1273-1284.
    [22]Li Meijun,Wang Tieguan,Liu Ju,et al.Genesis source of natural gas in the Fushan Sag,Beibuwan Basin[J].Natural Gas Geoscience,2007,18(2):260-265.[李美俊,王铁冠,刘菊,等.北部湾盆地福山凹陷天然气成因与来源[J].天然气地球科学,2007,18(2):260-265.]
    [23]Lin Liangbiao,Lin Hongbin,Hou Mingcai,et al.Geochemistry and accumulation of the Upper Palaeozoic natural gas in the Sulige Gasfield,Ordos Basin[J].Sedimentary Geology and Tethyan Geology,2009,29(2):77-82.[林良彪,蔺宏斌,侯明才,等.鄂尔多斯盆地苏里格气田上古生界天然气地球化学及成藏特征[J].沉积与特提斯地质,2009,29(2):77-82.]
    [24]Qian Zhihao,Chen Zhengfu.The origin of natural gas in the northern Tarim Baisn[J].Petroleum Geology&Expeximent,1992,14(3):217-226.[钱志浩,陈正辅.塔里木盆地北部天然气成因类型研究[J].石油实验地质,1992,14(3):217-226.]
    [25]Wang Qiang.Geochemical Characteristics of Natural Gas of T3x2 Gas Reservoirs in Bimamiao,Qiongxi and Pingluoba of West Sichuan[D].Chengdu:Southwest Petroleum University.2006.[王强.川西白马庙-邛西-平落坝地区须二段天然气成藏地球化学研究[D].成都:西南石油大学,2006.]
    [26]Liu Dawei.The Comparative Analysis of the Hydrocarbon Generation Kinetics Characteristics of Marine Carbonate Rocks and Marine Mudstone[D].Daqing:Northeast Petroleum University,2012.[刘大为.海相碳酸盐岩和泥岩生烃动力学特征对比分析[D].大庆:东北石油大学,2012.]
    [27]Jia Cunshan.Studies on Origins and Migration Direction of Petroleum in Shaya Uplift of Tarim Basin[D].Beijing:China U-niversity of Mining and Technology,2012.[贾存善.塔里木盆地沙雅隆起油气成因及运移方向研究[D].北京:中国矿业大学,2012.]
    [28]Yuyong.Origin of Natural Gas and Natural Gas Accumulation from Middle-shallow Layer in South Songzhan[D].Daqing:Northeast Petroleum University,2010.[于勇.松辽盆地宋站南地区中浅层天然气来源与成藏条件[D].大庆:东北石油大学,2010.]
    [29]Shi Yingmin.Volcano Edifices and Gas Pool Formation in Changling Faulted Depression,Songliao Bain,China[D].Beijing:China University of Mining and Technology,2011.[时应敏.松辽盆地长岭断陷火山机构及天然气成藏特征研究[D].北京:中国矿业大学,2011.]
    [30]Zhao Jie.Study on Natural Gas Origin and Effective Source Rock of Nanpu Depression[D].Beijing:China University of Petroleum,2011.[赵杰.南堡凹陷天然气成因及有效烃源岩研究[D].北京:中国石油大学,2011.]
    [31]Wen Nuan.Signature of Volcanic Reservoirs of Xujiaweizi Fault Depression,North Songliao Basin,NE China[D].Changchun:Jilin University,2004.[温暖.徐家围子断陷火山岩天然气藏研究[D].长春:吉林大学,2004.]
    [32]Kotarba M J,Nagao K.Composition and origin of natural gases accumulated in the Polish and Ukrainian parts of the Carpathian region:Gaseous hydrocarbons,noble gases,carbon dioxide and nitrogen[J].Chemical Geology,2008,255(3-4):426-438.
    [33]Cai C F,Hu G Y,He H,et al.Geochemical characteristics and origin of natural gas and thermochemical sulphate reduction in Ordovician carbonates in the Ordos Basin,China[J].Journal of Petroleum Science and Engineering,2005,48(3):209-226.
    [34]Tao Xiaowan,Li ming,Zhang Xinxin,et al.Influence of microbial oxidation onδ13C values of hydrocarbon gases[J].Petroleum Exploration and Development,2014,19(3):41-49.[陶小晚,李明,张欣欣,等.微生物氧化作用对有机烷烃气碳同位素的影响[J].石油勘探与开发,2014,19(3):41-49.]
    [35]Guo Jianjun,Chen Jianfa,Zhu Lei,et al.Geochemical characteristics and genesis of the natural gas in the Tazhong Uplift,the Tarim Basin[J].Petroleum Geology&Experiment,2007,29(6):577-582.[郭建军,陈践发,朱雷,等.塔里木盆地塔中天然气的地球化学特征及其成因[J].石油实验地质,2007,29(6):577-582.]
    [36]Qin Shengfei,Li Xianqi,Xiao Zhongyao,et al.Geochemistry,origin and distribution of natural gases in Tarim Basin,NWChina[J].Petroleum Exploration and Development,2005,32(4):70-78.[秦胜飞,李先奇,肖中尧,等.塔里木盆地天然气地球化学及成因与分布特征[J].石油勘探与开发,2005,32(4):70-78.]
    [37]Xu Yongchang,Shen Ping,Zheng Jianjin,et al.Geochemical characteristics of lower mature natural gas in Small and Medium basin of Yunan[J].Cinese Science Bulletin,1999,44(8):887-889.[徐永昌,沈平,郑建京,等.云南中、小盆地低演化天然气地球化学特征[J].科学通报,1999,44(8):887-889.]
    [38]Sun Ping’an,Wang Xulong,Tang Yong,et al.Geochemical constraints on the multiple origins of shallow-buried natural gases in the Junggar Basin[J].Geochimica,2012,41(2):109-121.[孙平安,王绪龙,唐勇,等.准噶尔盆地浅层天然气多种成因地球化学研究[J].地球化学,2012,41(2):109-121.]
    [39]Guo Yingqiang.Characteristics and genetic types of oil-gas of Chaiwopu Depression in Xinjiang[J].Xinjiang Geology,1997,15(1):59-68.[郭英强.新疆柴窝堡凹陷油气特征及成因类型探讨[J].新疆地质,1997,15(1):59-68.]
    [40]Zhang Xiaobao,Hu Yong,Ma Liyuan,et al.The gas carbon isotope characteristics,causes and distribution in western Qaidam Basin Tertiary salt lake[J].Science in China:Series D,2002,32(7):598-608.[张晓宝,胡勇,马立元,等.柴达木盆地西部第三系盐湖相天然气碳同位素特征、成因与分布[J].中国科学:D辑,2002,32(7):598-608.]
    [41]Miao Z Y,Chen J F,Wang J,et al.Application of butane geochemistry of natural gas in hydrocarbon exploration[J].Petroleum Science,2012,9(4):455-462.
    [42]Song Yan.Main factors affecting the changes in compositions of natural gas[J].Petroleum Exploration and Development,1991,18(2):42-49.[宋岩.影响天然气组分变化的主要因素[J].石油勘探与开发,1991,18(2):42-49.]
    [43]Dai Jinxing,Xia Xinyu,Qin Shengfei,et al.Causation of partly reversed orders ofδ13C in biogenic alkane gas in China[J].Oil and Gas Geology,2003,24(1):1-6.[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):1-6.]
    [44]Gao Gang,Huang Zhilong,Liang Hao,et al.Analysis on selectivity biodegradation of natural gas in Yanmuxi Oilfield of Tuha Basin[J].Acta Petrolei Sinica,2008,29(4):494-498.[高岗,黄志龙,梁浩,等.吐哈盆地雁木西油田天然气的选择性生物降解作用[J].石油学报,2008,29(4):494-498.]
    [45]Chen Jianfa,Chen Zhenyan,Ji Dongmin,et al.Discussion about the isotopically heavy ethane&propane in natural Gases from Liaohe Basin[J].Acta Sedimentologica Sinica,1998,16(2):5-8.[陈践发,陈振岩,季东民,等.辽河盆地天然气中重烃异常富集重碳同位素的成因探讨[J].沉积学报,1998,16(2):5-8.]
    [46]Barker J F,Fritz P.Carbon isotope fractionation during microbial methane oxidation[J].Nature,1981,293(5830):289-291.
    [47]Wang Wanchun.Li Nengshu,Liu Wenhui,et al.Simulating test of microbial degradation of natural gas[J].Natural Gas Industry,2008,28(11):34-37.[王万春,李能树,刘文汇,等.微生物降解天然气模拟试验[J].天然气工业,2008,28(11):34-37.]
    [48]Kinnaman F S,Valentine D L,Tyler S C.Carbon and hydrogen isotope fractionation associated with the aerobic microbial oxidation of methane,ethane,propane and butane[J].Geochimica et Cosmochimica Acta,2007,71(2):271-283.
    [49]Gao Gang,Gang Wenzhe,Hao Shisheng,et al.The evolution characteristics of gaseous products of humic coal and its geological significance[J].Acta Sedimentologica Sinica,1998,16(2):30-33.[高岗,刚文哲,郝石生,等.腐殖煤气态产物演化特征的模拟实验研究[J].沉积学报,1998,16(2):30-33.]
    [50]Chen Qin,Lei Xumei,Zhang Yuancheng,et al.A pyrolysis experiment of organic matter with a program of slowly rising temperature[J].Journal of Jianghan Petroleum Institute,1997,19(4):29-34.[陈沁,雷绪梅,张远成.有机质加压慢速程序升温条件下的生气模拟实验[J].江汉石油学院学报,1997,19(4):29-34.]
    [51]Wang Zhaoyun,Cheng Keming,Zhang Bosheng,et al.The study on the characteristics and evolution regularity of product of gas under pyrolysis simulatin experiments[J].Petroleum Exploration and Development,1995,22(3):36-40.[王兆云,程克明,张柏生.加水热模拟实验气态产物特征及演化规律研究[J].石油勘探与开发,1995,22(3)36-40.]
    [52]Yuan Dongshan,Zhang Zhihuan,Zeng Yangtao,et al.Evolution characteristics of gaseous hydrocarbon during thermal simulation of deep source rocks[J].Natural Gas Geoscience,2006,17(6):833-836.[袁东山,张枝焕,曾艳涛,等.深层烃源岩热模拟过程中气态烃产物变化特征[J].天然气地球科学,2006,17(6):833-836.]
    [53]Shen Zhongmin,Wang Peng,Liu Sibing,et al.Geochemical characteristics of light hydrocarbon in natural gas of west Sichuan Depression,China[J].Journal of Chengdu university of technology:Sinence&Technology Edition,2011,38(5):500-506.[沈忠民,王鹏,刘四兵,等.川西坳陷中段天然气轻烃地球化学特征[J].成都理工大学学报:自然科学版,2011,38(5):500-506.]
    [54]Liu Zhaolu,Li Jian,Fang Jiahu,et al.Experimental investigation on physical simulation of gas dissolved in water during migration[J].Natural Gas Geoscience,2004,15(1):32-36.[刘朝露,李剑,方家虎,等.水溶气运移成藏物理模拟实验技术[J].天然气地球科学,2004,15(1):32-36.]
    [55]Shi Ji’an,Sun Xiujian,Wang Jinpeng,et al.Physical simulating experiment of natural gas migration and its characteristics of composition differentiation and carbon isotope fractionation[J].Petroleum Geology&Experiment,2005,27(3):293-298.[史基安,孙秀建,王金鹏,等.天然气运移物理模拟实验及其组分分异与碳同位素分馏特征[J].石油实验地质,2005,27(3):293-298.]
    [56]Xu Guosheng,Liu Shugen,Li Guorong,et al.Phase state evolution in the cross formational flow of natural gas in the west Sichuan Foreland Basin,China[J].Journal of Chengdu University of Technology,2001,28(4):383-389.[徐国盛,刘树根,李国蓉,等.川西前陆盆地碎屑岩天然气跨层运移过程中的相态演变[J].成都理工大学学报,2001,28(4):383-389.]
    [57]Hou Dujie,Pang Xiong,Xiao Jianxin,et al.The geological and geochemical evidence on the identification of natural gas migra-tion through fault system,Baiyun Sag,Pearl River Mouth Basin,China[J].Earth Science Frontiers,2008,15(4):81-87.[侯读杰,庞雄,肖建新,等.白云凹陷断裂作为天然气运移通道的地质-地球化学证据[J].地学前缘,2008,15(4):81-87.]
    [58]Fu Ning,Li Youchuan,Liu Dong,et al.Geochemical characteristics of natural gas migration in Pinghu Gasfield,East China Sea[J].Petroleum Exploration and Development,2005,32(5):34-37.[傅宁,李友川,刘东.东海平湖气田天然气运移地球化学特征[J].石油勘探与开发,2005,32(5):34-37.]

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700