渤海海域渤中地区烃源岩封闭金管热解模拟生烃实验研究

王军; 王清斌; 王飞龙; 刘晓健; 潘文静

doi:10.11781/sysydz201703423

渤海海域渤中地区烃源岩封闭金管热解模拟生烃实验研究

doi: 10.11781/sysydz201703423

中海石油(中国)有限公司天津分公司, 天津 300452

基金项目: 中国石化科技部项目“西湖凹陷平湖组油气资源评价与区带优选”（G5800-13-ZS-KJB028）资助。

详细信息

作者简介:
王军(1984-),男,硕士,工程师,从事油气地球化学及成藏研究。E-mail:varran@163.com。

中图分类号: TE135.2
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出版历程
- 收稿日期: 2016-10-17
- 修回日期: 2017-03-13
- 刊出日期: 2017-05-28

Gold tube pyrolysis study of source rock hydrocarbon generation in Bozhong area, offshore Bohai Bay Basin

Tianjin Branch, CNOOC China Limited, Tianjin 300452, China

摘要

摘要: 选取渤海海域渤中地区沙南凹陷沙三段、沙一段和东三段烃源岩各1个样品，秦南凹陷沙三段烃源岩2个样品，进行封闭金管加水热解实验。烃源岩样品为湖相泥岩，有机质丰度高，干酪根类型为Ⅰ型，且处于低熟阶段。烃源岩矿物组成以黏土矿物为主，方解石、石英和长石也占有相当的比重。热解过程涵盖了主要的生油阶段，沙三段、沙一段和东三段烃源岩平均生烃活化能集中分布在219~222 kJ/mol，同一凹陷不同层系、不同凹陷同一层系差别不大，但黏土矿物含量较低和方解石含量较高的样品平均活化能略偏高。封闭热解生烃高峰C₁₄₊液态烃产物碳同位素相比原岩沥青“A”碳同位素增重幅度可达11.3%，应用低熟源岩沥青“A”碳同位素进行油源对比时须谨慎。残余固体总有机碳损失可达48%，对原本有机质丰度高和类型好、现处于高演化阶段的烃源岩评价时，有必要进行有机质丰度和类型的恢复。
- 烃源岩 /
- 封闭金管热解实验 /
- 生烃动力学 /
- 碳同位素 /
- 总有机碳 /
- 渤海海域
Abstract: Sealed gold tube pyrolysis was carried out for 3 source rock samples from the third (E₂s³) and first (E₃s¹) members of Shahejie Formation, and the third (E₃d³) member of Dongying Formation in the Shanan Sag, and 2 source rock samples from the E₂s³ in the Qinnan Sag in Bozhong area. These samples are lacustrine shale with a high organic matter content and low maturity, and contain type I kerogen. Minerals in the source rock samples are mainly clay minerals and contain a significant amount of calcite, quartz and feldspar. The gold tube pyrolysis experiments focus on liquid hydrocarbon generation. The mean hydrocarbon generation kinetics of E₂s³, E₃s¹ and E₃d³ source rock samples range between 219 and 222 kJ/mol, and the kinetics of all samples have a concentrated distribution. Samples from same sag but different intervals, and samples from different sags but same interval have no significant difference, but the samples with a relatively low content of clay minerals and a high content of calcite have a relatively higher mean hydrocarbon activation energy. Carbon isotopes of C_14⁺ liquid products during peak hydrocarbon generation can be 11.3% heavier than extracts from unpyrolyzed samples, and oil-source correlation with extracts from low maturity source rocks must consider this. TOC loss of residual solids can reach up to 48%. It is necessary to restore organic matter abundance and kerogen type when evaluating high maturity source rocks with a high organic abundance and favorable organic type.
- source rock /
- sealed gold pyrolysis experiment /
- hydrocarbon generation kinetics /
- carbon isotope /
- TOC /
- offshore Bohai Bay Basin

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参考文献(43)

[1]	周心怀,余一欣,汤良杰,等.渤海海域新生代盆地结构与构造单元划分[J].中国海上油气,2010,22(5):285-289. Zhou Xinhuai,Yu Yixin,Tang Liangjie,et al.Cenozoic offshore basin architecture and division of structural elements in Bohai Sea[J].China Offshore Oil and Gas,2010,22(5):285-289.
[2]	朱伟林,米立军,龚再升.渤海海域油气成藏与勘探[M].北京:科学出版社,2009. Zhu Weilin,Mi Lijun,Gong Zaisheng.Hydrocarbon accumulation and exploration offshore Bohai Bay Basin[M].Beijing:Science Press,2009.
[3]	夏庆龙,周心怀,薛永安,等.渤海海域油气藏形成分布与资源潜力[M].北京:石油工业出版社,2012. Xia Qinglong,Zhou Xinhuai,Xue Yong'an,et al.Reservoir formation,distribution and hydrocarbon resource offshore Bohai Bay Basin[M].Beijing:Petroleum Industry Press,2012.
[4]	任拥军,杜雨佳,郭潇潇,等.渤中凹陷古近系优质烃源岩特征及分布[J].油气地质与采收率,2015,22(1):5-13. Ren Yongjun,Du Yujia,Guo Xiaoxiao,et al.Characteristics and distribution of Paleogene high-quality source rocks in Bozhong sag[J].Petroleum Geology and Recovery Efficiency,2015,22(1):5-13.
[5]	柴永波,李伟,刘超,等.渤海海域古近纪断裂活动对烃源岩的控制作用[J].断块油气田,2015,22(4):409-414. Chai Yongbo,Li Wei,Liu Chao,et al.Controlling effect of fault activity on source rocks during Paleogene in Bohai sea area[J].Fault-Block Oil and Gas Field,2015,22(4):409-414.
[6]	王建宝,肖贤明,郭汝泰,等.渤海湾盆地东营凹陷烃源岩生烃动力学研究[J].石油实验地质,2003,25(4):403-409. Wang Jianbao,Xiao Xianming,Guo Rutai,et al.Study on the hydrocarbon generation kinetics of source rocks from the Dongying Depression,the Bohaiwan Basin[J].Petroleum Geology & Experiment,2003,25(4):403-409.
[7]	Behar F,Vandenbroucke M,Tang Y,et al.Thermal cracking of kerogen in open and closed systems:Determination of kinetic parameters and stoichiometric coefficients for oil and gas generation[J].Organic Geochemistry,1997,26(5/6):321-339.
[8]	刘金钟,唐永春.用干酪根生烃动力学方法预测甲烷生成量之一例[J].科学通报,1998,43(11):1187-1191. Liu Jinzhong,Tang Yongchun.Kinetics of early methane generation from Green River shale[J].Chinese Science Bulletin,1998,43(22):1908-1912.
[9]	Hill R J,Zhang E,Katz B J,et al.Modeling of gas generation from the Barnett shale,Fort Worth Basin,Texas[J].AAPG Bulletin,2007,91(4):501-521.
[10]	Wang Qi,Zou Huayao,Hao Fang,et al.Modeling hydrocarbon gene-ration from the Paleogene source rocks in Liaodong Bay,Bohai Sea:A study on gas potential of oil-prone source rocks[J].Organic Geochemistry,2014,76:204-219.
[11]	Behar F,Roy S,Jarvie D M.Artificial maturation of a type Ⅰ kerogen in closed system:Mass balance and kinetic modelling[J].Organic Geochemistry,2010,41(11):1235-1247.
[12]	Zhang E,Hill R J,Katz B J,et al.Modeling of gas generation from the Cameo coal zone in the Piceance Basin,Colorado[J].AAPG Bulletin,2008,92(8):1077-1106.
[13]	郭显令,熊敏,周秦,等.烃源岩生排烃动力学研究:以惠民凹陷临南洼陷沙河街组烃源岩为例[J].沉积学报,2009,27(4):723-731. Guo Xianling,Xiong Min,Zhou Qin,et al.Petroleum generation and expulsion kinetics:A case study of the Sahejie Formation source rocks from Linnan Sag of Huimin Depression[J].Acta Sedimentologica Sinica,2009,27(4):723-731.
[14]	Behar F,Lorant F,Lewan M.Role of NSO compounds during pri-mary cracking of a type Ⅱ kerogen and a type Ⅲ lignite[J].Organic Geochemistry,2008,39(1):1-22.
[15]	Pan Changchun,Geng Ansong,Zhong Ningning,et al.Kerogen pyrolysis in the presence and absence of water and minerals.1.Gas components[J].Energy & Fuels,2008,22(1):416-427.
[16]	Pan Changchun,Geng Ansong,Zhong Ningning,et al.Kerogen pyrolysis in the presence and absence of water and minerals:Amounts and compositions of bitumen and liquid hydrocarbons[J].Fuel,2009,88(5):909-919.
[17]	Huizinga B J,Tannenbaum E,Kaplan I R.The role of minerals in the thermal alteration of organic matter-Ⅲ.Generation of bitumen in laboratory experiments[J].Organic Geochemistry,1987,11(6):591-604.
[18]	李术元,林世静,郭绍辉,等.矿物质对干酪根热解生烃过程的影响[J].石油大学学报(自然科学版),2002,26(1):69-71. Li Shuyuan,Lin Shijing,Guo Shaohui,et al.Catlaytic effects of minerals on hydrocarbon generation in kerogen degradation[J].Journal of the University of Petroleum,China,2002,26(1):69-71.
[19]	Pan Changchun,Geng Ansong,Zhong Ningning,et al.Kerogen pyrolysis in the presence and absence of water and minerals:Steranes and triterpenoids[J].Fuel,2010,89(2):336-345.
[20]	Reynolds J G,Burnham A K.Comparison of kinetic analysis of source rocks and kerogen concentrates[J].Organic Geoche-mistry,1995,23(1):11-19.
[21]	Behar F,Lewan M D,Lorant F,et al.Comparison of artificial maturation of lignite in hydrous and nonhydrous conditions[J].Organic Geochemistry,2003,34(4):575-600.
[22]	张彩明,郑伦举,许锦.不同模拟实验条件下烃源岩生油气能力对比及意义[J].石油实验地质,2016,38(5):665-671. Zhang Caiming,Zheng Lunju,Xu Jin.Hydrocarbon generation potential under different experimental conditionsand its petroleum geology significance[J].Petroleum Geology & Experiment,2016,38(5):665-671.
[23]	蒋启贵,申宝剑,仰云峰,等.渤南洼陷页岩生烃组分动力学分析及其对页岩油气勘探的意义[J].石油实验地质,2016,38(2):231-239. Jiang Qigui,Shen Baojian,Yang Yunfeng,et al.Kinetic analysis of hydrocarbon generation components in shales from the Bonan sub-Sag and its significance for hydrocarbon exploration[J].Petroleum Geology & Experiment,2016,38(2):231-239.
[24]	李丕龙.济阳坳陷"富集有机质"烃源岩及其资源潜力[J].地学前缘,2004,11(1):317-322. Li Pilong.The organic-rich hydrocarbon source rocks and their resource potentials in Jiyang Depression[J].Earth Science Frontiers,2004,11(1):317-322.
[25]	邓运华,张功成,刘春成,等.中国近海两个油气带地质理论与勘探实践[M].北京:石油工业出版社,2013. Deng Yunhua,Zhang Gongcheng,Liu Chuncheng,et al.Geology theory and exploration application of oil and gas belts offshore China Sea[M].Beijing:Petroleum Industry Press,2013.
[26]	Pepper A S,Corvi P J.Simple kinetic models of petroleum formation.Part I:Oil and gas generation from kerogen[J].Marine and Petroleum Geology,1995,12(3):291-319.
[27]	刘立峰,姜振学,钟宁宁,等.辽河西部凹陷古近系烃源岩生烃动力学特征[J].地球科学(中国地质大学学报),2009,34(5):799-805. Liu Lifeng,Jiang Zhenxue,Zhong Ningning,et al.Hydrocarbon-generating dynamic characteristics of Paleogene source rocks in western depression,Liaohe Basin[J].Earth Science(Journal of China University of Geosciences),2009,34(5):799-805.
[28]	Jiang Qigui,Wang Yanbin,Qin Jianzhong,et al.Kinetics of the hydrocarbon generation process of marine source rocks in South China[J].Petroleum Exploration and Development,2010,37(2):174-180.
[29]	李术元,钱家麟,秦匡宗,等.干酪根热解平行反应模型中表观活化能与视频率因子的关联[J].华东石油学院学报,1987,11(2):64-70. Li Shuyuan,Qian Jialin,Qin Kuangzong,et al.Correlation of activation energy with frequency factor in Tissot's parallel reaction model of kerogen pyrolysis[J].Journal of East China Petroleum Institute,1987,11(2):64-70.
[30]	王民,卢双舫,董奇,等.有机质生烃动力学模型对比[J].中国石油大学学报(自然科学版),2011,35(3):12-18. Wang Min,Lu Shuangfang,Dong Qi,et al.Comparison on hydrocarbon generation kinetic models[J].Journal of China University of Petroleum,2011,35(3):12-18.
[31]	Hao Fang,Zhou Xinhuai,Zhu Yangming,et al.Charging of the Neogene Penglai 19-3 field,Bohai Bay Basin,China:Oil accumulation in a young trap in an active fault zone[J].AAPG Bulletin,2009,93(2):155-179.
[32]	Hao Fang,Zhou Xinhuai,Zhu Yangming,et al.Mechanisms for oil depletion and enrichment on the Shijiutuo uplift,Bohai Bay Basin,China[J].AAPG Bulletin,2009,93(8):1015-1037.
[33]	Hao Fang,Zhou Xinhuai,Zhu Yangming,et al.Mechanisms of petroleum accumulation in the Bozhong sub-basin,Bohai Bay Basin,China.Part 1:Origin and occurrence of crude oils[J].Marine and Petroleum Geology,2009,26(8):1528-1542.
[34]	Hao Fang,Zhou Xinhuai,Zhu Yangming,et al.Charging of oil fields surrounding the Shaleitian uplift from multiple source rock intervals and generative kitchens,Bohai Bay Basin,China[J].Marine and Petroleum Geology,2010,27(9):1910-1926.
[35]	高先志,张万选,张厚福.矿物质对热解影响的研究[J].石油实验地质,1990,12(2):201-205. Gao Xianzhi,Zhang Wanxuan,Zhang Houfu.Study of the influence of minerals on pyrolysis[J].Experimental Petroleum Geology,1990,12(2):201-205.
[36]	曹慧缇,张义纲,徐翔,等.碳酸盐岩生烃机制的新认识[J].石油实验地质,1991,13(3):222-237. Cao Huiti,Zhang Yigang,Xu Xiang,et al.A new understanding of hydrocarbon generation mechanism of carbonate rocks[J].Experimental Petroleum Geology,1991,13(3):222-237.
[37]	Tannenbaum E,Huizinga B J,Kaplan I R.Role of minerals in thermal alteration of organic matter,Ⅱ:A material balance[J].AAPG Bulletin,1986,70(9):1156-1165.
[38]	Dembicki H Jr.The effects of the mineral matrix on the determination of kinetic parameters using modified Rock Eval pyrolysis[J].Organic Geochemistry,1992,18(4):531-539.
[39]	黄第藩.陆相烃源岩有机质中碳同位素组成的分布特征[J].中国海上油气(地质),1993,7(4):1-5. Huang Difan.Distributive characteristics of carbon isotope composition in organic matters of continental source rock[J].China Offshore Oil and Gas (Geology),1993,7(4):1-5.
[40]	钟宁宁,卢双舫,黄志龙,等.烃源岩生烃演化过程TOC值的演变及其控制因素[J].中国科学(D辑地球科学),2004,34(SⅠ):120-126. Zhong Ningning,Lu Shuangfang,Huang Zhilong,et al.TOC changes in the process of thermal evolution of source rock and its controls[J].Science in China (Series D Earth Sciences),2004,47(S2):141-149.
[41]	Wang Min,Lu Shuangfang,Xue Haitao.Kinetic simulation of hydrocarbon generation from lacustrine type I kerogen from the Songliao Basin:Model comparison and geological application[J].Marine and Petroleum Geology,2011,28(9):1714-1726.
[42]	Zhou Yongsheng,Littke R.Numerical simulation of the thermal maturation,oil generation and migration in the Songliao Basin,northeastern China[J].Marine and Petroleum Geology,1999,16(8):771-792.
[43]	Tegelaar E W,Noble R A.Kinetics of hydrocarbon generation as a function of the molecular structure of kerogen as revealed by pyrolysis-gas chromatography[J].Organic Geochemistry,1994,22(3/5):543-574.