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基于流线数值模拟研究高含水后期油田的剩余油分布

谭河清 傅强 李林祥 崔文福 黄少雄 官敬涛 李祥同 成士兴

成都理工大学学报(自然科学版)2017,Vol.44Issue(1):30-35,6.
成都理工大学学报(自然科学版)2017,Vol.44Issue(1):30-35,6.DOI:10.3969/j.issn.1671-9727.2017.01.04

基于流线数值模拟研究高含水后期油田的剩余油分布

Application of streamline numerical simulation method to study of remaining oil distribution in high water-cut stage oilfield

谭河清 1傅强 2李林祥 1崔文福 1黄少雄 2官敬涛 1李祥同 3成士兴3

作者信息

  • 1. 中国石化 胜利油田分公司 孤东采油厂,山东 东营 257001
  • 2. 同济大学 海洋与地球科学学院,上海 200092
  • 3. 中国石化 胜利油田分公司 东胜公司,山东 东营 257001
  • 折叠

摘要

Abstract

According to the geologic and developmental features of the Ng6 3+4 of Neogene Guantao Formation in western No.7 district in Gudong Oilfield,one experimental zone in Ng63+4 unit is used to study the distribution of remaining oil in high water cut stage oilfield.The history matching of the reserves,pressure,moisture content and single drilling well water cut in the experimental zone produces a fine 3D geological model and parameters mode of less than 5% errors for 85% single-drilling wells. With the help of streamline numerical simulation technique, it obtains the characteristics of fluid migration under the condition of dense well pattern in high water-cut stage and divides remaining oil distribution patterns.It shows that large channel and high permeability zone are formed in the underground reservoir and the fluid migrates mostly along the high permeability zone. At the same time,oil displacement efficiency decreases obviously.The remaining oil distribution is controlled by sedimentary facies,sedimentary rhythm intraformational heterogeneity and drilling well network,the remaining oil occurs in the top of micro-structures,low permeable section in the plane and mainly concentrates on the top of the positive rhythm in the thick oil layer.

关键词

孤东油田/馆陶组/流线数值模拟/剩余油分布

Key words

Gudong oilfield/Guantao Formation/streamline numerical simulation/remaining oil distribution

分类

能源科技

引用本文复制引用

谭河清,傅强,李林祥,崔文福,黄少雄,官敬涛,李祥同,成士兴..基于流线数值模拟研究高含水后期油田的剩余油分布[J].成都理工大学学报(自然科学版),2017,44(1):30-35,6.

基金项目

国家科技重大专项(2011ZX05011-002)。 ()

成都理工大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1671-9727

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