石英胶结作用化学动力学模型及应用

杨俊生; 孟元林; 张洪; 李国会

doi:10.11781/sysydz200204372

石英胶结作用化学动力学模型及应用

doi: 10.11781/sysydz200204372

1.
中国地质大学, 北京, 100083
2. 中国石油, 大庆石油管理局, 勘探开发研究院, 黑龙江, 大庆, 163712

基金项目: 中国石油“九五”科技攻关项目(970206-02-01)

详细信息

作者简介:
杨俊生(1972- ),男(汉族),辽宁北票人,博士生,主要从事石油地质方面的研究工作.

中图分类号: TE122.2
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- 被引次数: 0
出版历程
- 收稿日期: 2002-01-24
- 修回日期: 2002-05-15
- 刊出日期: 2002-07-25

KINETIC MODEL OF QUARTZ CEMENTATION AND ITS APPLICATION

1.
China University of Geosciences, Beijing 100083, China
2. Research Institute of Petroleum Exploration and Development, Daqing Petroleum Administration, Daqing, Heilongjiang 163712, China

摘要

摘要: 石英(硅质)胶结作用是储层成岩作用中的重要类型,目前常根据镜下观察获得的石英加大级别确定储层所处的成岩阶段。该文综合考虑温度、时间、石英颗粒含量、粒径和粘土包壳对自生石英形成的影响,建立了石英胶结作用的化学动力学模型。该模型可以模拟碎屑岩储层成岩作用过程中任一时刻石英胶结物的含量及由此而引起的孔隙损失,这对于成岩作用的定量化研究及储层描述均具有重要意义。最后,以松辽盆地大庆油田汪家屯地区为例对这一模型进行了应用。
- 数值模拟 /
- 化学动力学 /
- 石英胶结
Abstract: Quartz cementation is one of the most important diagenetic process. The quartz overgrowth order obtained from observation of thin section often used to determine the diagenetic stage of reservoir rocks. In this article, we established a kinetic model of quartz cementation, in which temperature history, reaction time, detrital mineralogy, grain size and grain coating abundance were all considered. The model can be used to simulate the volume percentage of quartz cementation and the porosity loss during the diagenetic process of siliciclastic reservoir rocks. This has great significance for quantitative study of diagenesis and reservoir description. At last, the kinetic modeling of quartz cementation was successfully applied to the study of reservoirs in Wangjiatun area of Daqing oilfield.
- numerical simulation /
- chemical dynamics /
- quartz cementation

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参考文献(13)

[1]	裘怿楠,薛叔浩,应凤祥.中国陆相油气储集层[M].北京:石油工业出版社,1997.157.
[2]	应凤祥.中华人民共和国石油与天然气行业标准——碎屑岩成岩阶段划分规范[S].北京:石油工业出版社,1993.2-3.
[3]	Melvyn R.Giles.Diagenesis: a quantitative perspective[M].Kluwer Academic Publications, 1996.17-21.
[4]	Olav Walderhaug.Kinetic modeling of quartz cementation and porosity loss in deeply buried sandstone reservoirs[J].AAPG Bulletin, 1996, 80: 732-745.
[5]	Bjrkum P A, Oelkers E H, Nadeall P H, et al. Porosity prediction in quartzose sandstones as a function of time, temperature, depth, stylolite frequency and hydrocarbon saturation[J].AAPG Bulletin, 1998, 82: 637-648.
[6]	Olav Walderhaug.Modelling quartz cementation and porosity in middle Jurassic Brent group sandstone of the KvitebjΦrn field, northern North Sea[J].AAPG Bulletin, 2000, 84: 1325-1339.
[7]	涂光炽.低温地球化学[M].北京:科学出版社,1996.163-167.
[8]	Olav Walderhaug.Precipitation rates for quartz cements in sandstones determined by fluid-inclusion microthermometry and temperature-history modeling[J].Journal of Sedimentary Research, 1994, A64: 324-333.
[9]	李昌存,韩秀丽.塔里木盆地克孜勒苏群碎屑岩成岩作用研究[J].石油实验地质,1998,20(2):135-137.
[10]	项希勇,穆星.济阳坳陷沾化凹陷东部热史模拟研究[J].石油实验地质,2000,22(2):172-173.
[11]	袁彩萍,徐思煌.西藏伦坡拉盆地地温场特征及烃源岩演化史[J].石油实验地质,2000,22(2):157-158.
[12]	Lasaga A C.Chemical kinetics of water-rock interactions[J].Journal of Geophysical Research, 1984, 89: 4009-4025.
[13]	王志武,杨继良,高瑞祺,等.中国石油地质志(第二卷)——大庆、吉林油田[M].北京:石油工业出版社,1993.44-50.