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深层碳酸盐岩储层溶洞围岩应力分布研究

周汉国 郭建春 李静 彭成乐 王昌 高帅 郑金凯

地质力学学报2018,Vol.24Issue(1):35-41,7.
地质力学学报2018,Vol.24Issue(1):35-41,7.DOI:10.12090/j.issn.1006-6616.2018.24.01.004

深层碳酸盐岩储层溶洞围岩应力分布研究

DISTRIBUTION OF SURROUNDING ROCK STRESS IN DEEP CARBONATE RESERVOIR KARST CAVE

周汉国 1郭建春 2李静 1彭成乐 3王昌 4高帅 3郑金凯3

作者信息

  • 1. 西南石油大学油气藏地质及开发工程国家重点实验室,四川成都610500
  • 2. 中国石化胜利油田分公司油气勘探管理中心,山东东营257000
  • 3. 中国石油大学(华东)地质力学与工程研究所,山东青岛266580
  • 4. 河北康保广恒新能源有限公司,河北张家口075000
  • 折叠

摘要

Abstract

The Ordovician carbonate oil pool in northern Renqiu of the Jizhong depression is taken as an example in this article.The rock mechanical parameters in the study area were calculated based on the log data of the oil field,and the typical isolated water long elliptic karst cave of the target reservoir was selected,with its surrounding rock stress and its damage zone calculated by numerical simulation and third strength theory.The results show that:1) Under the combined action of overburden pressure and lateral pressure,the stress concentration effect zone of the long elliptic karst cave surrounding rock is 9 times of the radius.2) The surrounding rock stress of long elliptic karst cave is mainly compressive stress,mainly concentrating in the top and the bottom.3) The filling property of karst cave has great influence on the principal stress difference and damage range of surrounding rock.For the long-elliptic karst cave,the principal stress difference and shear damage of the surrounding rock increase with the increase of filling pressure when the filling pressure is less than 0.1 MPa;while the principal stress difference and the shear damage range of the surrounding rock gradually decrease with the increase of filling pressure when the filling pressure is more than 0.1 MPa.

关键词

碳酸盐岩/溶洞/围岩应力/数值模拟

Key words

carbonate rocks/karst cave/surrounding rock stress/numerical simulation

分类

天文与地球科学

引用本文复制引用

周汉国,郭建春,李静,彭成乐,王昌,高帅,郑金凯..深层碳酸盐岩储层溶洞围岩应力分布研究[J].地质力学学报,2018,24(1):35-41,7.

基金项目

国家自然科学基金项目(41272141) (41272141)

国家科技重大专项(2016ZX05002-002) (2016ZX05002-002)

地质力学学报

OACSCDCSTPCD

1006-6616

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