天然气地球科学 ›› 2004, Vol. 15 ›› Issue (2): 144–149.doi: 10.11764/j.issn.1672-1926.2004.02.144

• 天然气地球化学 • 上一篇    下一篇

轮南和塔河油田稠油沥青质钌离子催化氧化研究

马安来1,2, 张水昌2,张大江2   

  1. (1.长江大学地球化学系, 湖北 荆州 434023; 2.中国石化石油勘探开发研究 院,北京 100083)
  • 收稿日期:2004-02-13 修回日期:2004-03-01 出版日期:2004-04-20 发布日期:2004-04-20
  • 通讯作者: 马安来
  • 作者简介:马安来(1969-),男,安徽淮南人,副教授,博士,现从事 石油地球化学、有机岩石学研究与教学工作.
  • 基金资助:

    国家“九五”科技攻关项目(编号:99-111-01-03)资助.

RUTHENIUM-INOS-CATALYZED OXIDATION OF THE ASPHALTENES OF HEAVY OILS FROM LUN NAN AND TAHE OILFIELDS OF THE TARIM BASIN, NW CHINA

MA An- lai1,2, ZHANG Shui-chang2, ZHANG Da-jiang2   

  1. (1. Department of Geochemistry, Yangtze University, Jingzhou 434023,  China; 
    2. Petroleum Exploration and Production Research Institute, SINOPEC, Beijing 100083, China)
  • Received:2004-02-13 Revised:2004-03-01 Online:2004-04-20 Published:2004-04-20

摘要:

运用钌离子催化氧化(RICO)技术,研究了轮南和塔河油田以及TD2井稠油沥青质。在轮南和塔河油田稠油沥青质分子结构中,键合在沥青质芳核结构中的官能团以烷基侧链为主,烷基桥次之,此外还有一定的支链烷烃及生物标志物,这些化合物绝大部分是以C-C键键合在沥青质结构中的。沥青质中的芳核体系大多以萘、菲、联苯型为主,高度缩合的芳核结构较少。轮南和塔河油田稠油沥青质RICO产物具有较高的一元和二元酸比值,甾烷酸的异构化参数均大于0.40,表明原油具有较高的成熟度;一元酸和甾烷酸的分布均与典型寒武系生源的TD2井稠油具有明显的差异,指示轮南和塔河油田稠油源于中上奥陶统烃源岩。

关键词: 沥青质, 稠油, 钌离子催化氧化, 生物标志物, 塔里木盆地

Abstract:

The asphaltenes of the heavy oils from Lunnan, Tahe oilfie lds and TD2 well were studied by ruthenium-ions-catalyzed oxidation. The subst ituted functions bounded on the aromatic structure of the asphaltene were domina ted by n-alkyl chains, with n-alkyl bridges secondary. A certain amount of bra nched alkanes and biomarkers were also identified. Most of these compounds were  bounded on the asphaltene through C-C bounds. The aromatic systems of the aspha ltenes were dominated by naphthalene, phenantherne and biphenyl, with little hig hly condensed aromatic system. The products of the asphaltene RICO with high n- alkanoic/di-n-alkanoic acid ratios and the isomeric ratio of the steranoic aci d great than 0.4 suggested that the oils have high maturity. The distributions o f n-alkanoic and steranoic acids of the products of asphaltenes RICO of heavy o ils from Lunnan, Tahe oilfields showed great difference from that of the oils fr om TD2 well, a typical oil from the Cambrian, indicating the heavy oils from Lun nan and Tahe oilfields were originated from middle-upper Ordovician. 

Key words: Asphaltene, Heavy oil, Ruthenium-ions-catalyzed oxidation(RICO), Biomarker, Tarim basin.

中图分类号: 

  • TE122.1

[1 ]  Tissot B P, Welte D H. Petroleum Formation and Occurrence [M ]. New York: Springer-Verlag, 1984.
 [2 ]  Rubinstein I, Strausz O P. Thermal treatment of the Athabasca oil sand bitumen and its component parts [J ]. Geochimica et Co smochimica Acta,1979,43(12): 887-893.
 [3 ]  Rubinstein I, Spyskerelle C, Strausz P O. Pyrolysis of asphaltenes, a source of geochemical information [J ]. Geochimica et Cosmochim ica Acta, 1979,43(1): 1-6.
  [4 ]  Behar F, Pelet R, Roucache J. Geochemistry of asphaltenes [J ]. Org anic Geochemistry,1984,16(6): 587-595.
  [5 ]  熊永强,耿安松.辽河油田生物降解原油沥青质热解产物中单体化合物碳同位素组成[J ].地球化学,1998,27(6):532-536.
  [6 ]  Di Primio R, Horsfield B. Predicting the generation of heavy oils i n carbonate/evaporitic environments using pyrolysis methods [J ]. Organic Geoche mistry, 1996,24:999-1016.
  [7 ]  Zhang S C, Hanson D G, Liang D G, et al. Paleozoic oil-source  rock correlations in the Tarim basin, NW China [J ]. Organic Geochemistry, 2000,31(4):273-286.
  [8 ]  Mojelsky T W, Ignasiak M, Frakman Z, et al. Structural features of Alberta oil sand bitumen and heavy oil asphaltenes [J ]. Energy  and Fuels, 1992,6(1): 83-96.
  [9 ]  Peng P, Fu J, Sheng G,et al. Ruthenium-iron-catalyzed oxidation of an immature asphaltene: Structural features and biomarker distr ibution [J ]. Energy and Fuel, 1999,13(2): 266-277.
 [10 ]  Strausz O P, Mojelsky T W, Lown E M. Structural features of Bo scan and Duri asphaltene [J ]. Energy and Fuel, 1999,13(2): 228-247.
 [11 ]  Strsusz O P, Mojelsky T W, Farhad F, et al. Additional structural de tails on Athabasca asphaltene and their ramifications [J ]. Energy and Fuel, 1 999,13(2): 207-227.
 [12 ]  Strausz O P, Mojelsky T W, Lown E M. The molecular structure of asphalte ne: An unfolding story [J ]. Fuel, 1992,71(12):1355-1363.
 [13 ]  张水昌,梁狄刚,黎茂稳,等.分子化石与塔里木盆地油源对比[J ].科学通报,2002,47(增刊):16-23.

[1] 张荣虎,王珂,王俊鹏,孙雄伟,李君,杨学君,周露. 塔里木盆地库车坳陷克深构造带克深8区块裂缝性低孔砂岩储层地质模型[J]. 天然气地球科学, 2018, 29(9): 1264-1273.
[2] 王清龙,林畅松,李浩,韩剑发,孙彦达,何海全. 塔里木盆地西北缘中下奥陶统碳酸盐岩沉积微相特征及演化[J]. 天然气地球科学, 2018, 29(9): 1274-1288.
[3] 周波,曹颖辉,齐井顺,黄世伟,刘策,贾进华,陈秀艳. 塔里木盆地古城地区下奥陶统储层发育机制[J]. 天然气地球科学, 2018, 29(6): 773-783.
[4] 朱光有,曹颖辉,闫磊,杨海军,孙崇浩,张志遥,李婷婷,陈永权. 塔里木盆地8 000m以深超深层海相油气勘探潜力与方向[J]. 天然气地球科学, 2018, 29(6): 755-772.
[5] 王珊,曹颖辉,杜德道,王石,李洪辉,董洪奎,严威,白莹. 塔里木盆地柯坪—巴楚地区肖尔布拉克组储层特征与主控因素[J]. 天然气地球科学, 2018, 29(6): 784-795.
[6] 曹颖辉,李洪辉,闫磊,王洪江,张君龙,杨敏,赵一民. 塔里木盆地满西地区寒武系台缘带分段演化特征及其对生储盖组合的影响[J]. 天然气地球科学, 2018, 29(6): 796-806.
[7] 闫磊,李洪辉,曹颖辉,杨敏,赵一民. 塔里木盆地满西地区寒武系台缘带演化及其分段特征[J]. 天然气地球科学, 2018, 29(6): 807-816.
[8] 杨敏,赵一民,闫磊,李洪辉,张欣欣,徐振平,罗浩渝. 塔里木盆地东秋里塔格构造带构造特征及其油气地质意义[J]. 天然气地球科学, 2018, 29(6): 826-833.
[9] 陈斐然,张义杰,朱光有,张宝收,卢玉红,张志遥. 塔里木盆地台盆区深层天然气地球化学特征及成藏演化[J]. 天然气地球科学, 2018, 29(6): 880-891.
[10] 黄少英, 杨文静, 卢玉红, 张科, 赵青, 凡闪. 塔里木盆地天然气地质条件、资源潜力及勘探方向[J]. 天然气地球科学, 2018, 29(10): 1497-1505.
[11] 陈燕燕,胡素云,李建忠,王铜山, 陶小晚. 原油裂解过程中组分演化模型及金刚烷类化合物的地球化学特征[J]. 天然气地球科学, 2018, 29(1): 114-121.
[12] 任宇泽,林畅松,高志勇,刘景彦,宋宁宁. 塔里木盆地西南坳陷白垩系层序地层与沉积充填演化[J]. 天然气地球科学, 2017, 28(9): 1298-1311.
[13] 张建勇,倪新峰,吴兴宁,李文正,郝毅,陈娅娜,吕学菊,谷明峰,田瀚,朱茂. 中国主要克拉通盆地深层白云岩优质储层发育主控因素及分布[J]. 天然气地球科学, 2017, 28(8): 1165-1175.
[14] 冀昆,郭少斌,李新,罗燕颖,姜黎明,曹先军. 溶孔发育的含沥青质碳酸盐岩核磁共振特征分析——以四川盆地高磨地区龙王庙组储层为例[J]. 天然气地球科学, 2017, 28(8): 1257-1263.
[15] 石书缘,刘伟,黄擎宇,王铜山,周慧,王坤,马奎. 塔里木盆地北部震旦系齐格布拉克组白云岩储层特征及成因[J]. 天然气地球科学, 2017, 28(8): 1226-1234.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!