新疆石油地质 ›› 2022, Vol. 43 ›› Issue (1): 92-101.doi: 10.7657/XJPG20220114

• 应用技术 • 上一篇    下一篇

连通导电模型参数确定及其在白云岩储集层评价中的应用

谢芳1(), 蔡德洋2, 刘瑞林1, 张承森2, 冯程3   

  1. 1.长江大学 地球物理与石油资源学院,武汉 430100
    2.中国石油 塔里木油田分公司 勘探开发研究院,新疆 库尔勒 841000
    3.中国石油大学(北京) 克拉玛依校区 石油学院,新疆 克拉玛依 834000
  • 收稿日期:2021-04-05 修回日期:2021-05-20 出版日期:2022-02-01 发布日期:2022-01-24
  • 作者简介:谢芳(1987-),女,湖北荆州人,讲师,博士,测井资料处理,(Tel)15507169923(E-mail) xiefang1010@qq.com
  • 基金资助:
    国家自然科学基金(42004089)

Parameters of Connected Conducting Model and Its Application in Dolomite Reservoir Evaluation

XIE Fang1(), CAI Deyang2, LIU Ruilin1, ZHANG Chengsen2, FENG Cheng3   

  1. 1. School of Geophysics and Petroleum Resources, Yangtze University, Wuhan, Hubei 430100, China
    2. Research Institute of Exploration and Development, Tarim Oilfield Company, PetroChina, Korla, Xinjiang 841000, China
    3. School of Petroleum, Karamay Campus, China University of Petroleum(Beijing), Karamay, Xinjiang 834000, China
  • Received:2021-04-05 Revised:2021-05-20 Online:2022-02-01 Published:2022-01-24

摘要:

以白云岩储集层物性、岩电、CT扫描、核磁共振和薄片分析资料为基础,提出了一种确定储集层临界含水孔隙度、临界含水饱和度、临界导通指数等连通导电模型参数的方法。将计算得到的临界含水饱和度与T2截止值、渗透率、CT扫描和薄片分析结果进行对比,并将临界导通指数与胶结指数进行对比,分析了临界含水饱和度、临界含水孔隙度及临界导通指数的物理意义。将岩心样品的连通导电饱和度理论曲线与阿尔奇饱和度理论曲线进行对比,分析了连通导电公式与阿尔奇公式计算结果的差别。最后,根据确定的连通导电模型参数,利用连通导电公式计算了2口井白云岩储集层的含水饱和度,计算结果与试油结论一致。

关键词: 白云岩储集层, 连通导电模型, 阿尔奇模型, 临界导通指数, 临界含水孔隙度, 临界含水饱和度

Abstract:

Based on reservoir physical properties and the data of rock electricity, CT scan, nuclear magnetic resonance and thin slices, a method for determining the parameters of a connected conducting model is proposed for studying dolomite reservoirs, including the critical water-filled porosity, critical water saturation and critical conductivity index. Then the calculated critical water saturation is compared with the T2 cut-off value, permeability, CT scan photos and thin slice analysis results, the critical conductivity index is compared with the cementation index, and the physical meanings of critical water saturation, critical water-filled porosity and critical conductivity index are discussed. The theoretical saturation curves from connected conduction is compared with the theoretical saturation curves from Archie’s formula, and the difference between them is discussed. Finally, according to the determined parameters of the connected conducting model, the water saturations of the dolomite reservoir in two wells are calculated using the connected conductance formula and the calculated results are consistent with formation test results.

Key words: dolomite reservoir, connected conducting model, Archie model, critical conductivity index, critical water-filled porosity, critical

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