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运用扫描电镜和压汞法研究江汉盆地古新统-白垩系砂岩储层孔喉结构及定量参数特征

蔡芃睿 王春连 刘成林 杨飞 徐海明 谢腾骁 余小灿 孟令阳

岩矿测试2017,Vol.36Issue(2):146-155,10.
岩矿测试2017,Vol.36Issue(2):146-155,10.DOI:10.15898/j.cnki.11-2131/td.2017.02.008

运用扫描电镜和压汞法研究江汉盆地古新统-白垩系砂岩储层孔喉结构及定量参数特征

Study on Pore Structure and Quantitative Parameters of the Paleocene-Cretaceous Sandstone Reservoir in Jiangling Depression by SEM and Mercury Injection Method

蔡芃睿 1王春连 2刘成林 2杨飞 1徐海明 2谢腾骁 3余小灿 4孟令阳1

作者信息

  • 1. 长江大学地球物理与石油资源学院,湖北 武汉 430100
  • 2. 中国地质科学院矿产资源研究所,国土资源部成矿作用与资源评价重点实验室,北京100037
  • 3. 北京理工大学,北京 100081
  • 4. 中国地质大学(北京)地球科学与资源学院,北京 100083
  • 折叠

摘要

Abstract

Evaluating reservoirs by pore structure has been widely used in oil and gas development,but this method has not yet been used in the evaluation of potassium salt reservoirs.The pore throat type and structure,capillary pressure curve,and quantitative feature parameters of pore throat of the Paleocene-Cretaceous-rich potassium-rich brine reservoir in Jianghan basin are studied by using a large number of reservoir porosity and pore throat data obtained by Scanning Electron Microscopy and Mercury Intrusion.Combined with the discharge pressure and other experimental parameters,the pore structure is divided into Ⅰ,Ⅱ,and Ⅲ types.The results show that the sandstone reservoirs of the Paleocene Shashi Formation are dominated by type Ⅱ pore structure with the average displacement pressure of 2.72 MPa and the average porosity of 6.32%.The sandstone reservoirs of the Cretaceous Honghuatao Formation are dominated by Ⅰ and Ⅱ pore structure types.The displacement pressure of type Ⅰ is 0.28 MPa,the average porosity is 16.99%,and the permeability is 87.79×10-3 μm2.The average displacement pressure of type Ⅱ is 1.103 MPa,the average porosity is 10.02%,and the permeability is 18.83×10-3 μm2.The quality of the reservoir was evaluated by a comprehensive analysis of pore throat quantitative parameters such as maximum mercury saturation,maximum pore throat radius,median radius and mercury recovery efficiency.It is believed that the sandstone type of the Paleocene Shashi Formation is dominated by siltstone,and the quality of the reservoir is poor,which belongs to the low porosity and low permeability reservoir.The sandstone type of the Cretaceous Honghuatao Formation is mainly fine sandstone,and the reservoir is of good quality and belongs to low porosity and low permeability reservoir.This study provides a reliable geological basis for the evaluation of potassium-rich brine reservoirs and for further exploration and development.

关键词

江陵凹陷/钾盐/毛细管压力曲线/孔喉特征参数/储层物性/相关性模型

Key words

Jiangling Depression/sylvite/capillary pressure curve/pore structure parameter/reservoir property/correlation model

分类

天文与地球科学

引用本文复制引用

蔡芃睿,王春连,刘成林,杨飞,徐海明,谢腾骁,余小灿,孟令阳..运用扫描电镜和压汞法研究江汉盆地古新统-白垩系砂岩储层孔喉结构及定量参数特征[J].岩矿测试,2017,36(2):146-155,10.

基金项目

国家自然科学基金青年基金资助项目(41502089) (41502089)

国家重点基础研究发展计划(973计划)项目(2011CB403007) (973计划)

中央级公益性科研院所基本科研业务费项目(K1415) (K1415)

中国地质调查局钾盐资源调查评价项目(DD20160054,DD20160056) (DD20160054,DD20160056)

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