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黏土表面结合水的低场核磁共振定量研究

苏俊霖 董汶鑫 冯杰 杨培强 罗平亚

钻井液与完井液2018,Vol.35Issue(1):8-12,5.
钻井液与完井液2018,Vol.35Issue(1):8-12,5.DOI:10.3969/j.issn.1001-5620.2018.01.002

黏土表面结合水的低场核磁共振定量研究

Quantitative Study on Surface Bound Water of Clay with Low Field NMR

苏俊霖 1董汶鑫 1冯杰 2杨培强 3罗平亚1

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,成都610500
  • 2. 中国石油集团钻井工程技术研究院,北京102206
  • 3. 纽迈电子科技有限公司,上海200333
  • 折叠

摘要

Abstract

The types and extents of clay hydration are directly related to the stabilization of water sensitive shale borehole.Thermogravimetric analysis,a widely used method presently in determining the type and content of clay in formation rocks,is unable to quickly,intuitively and quantitatively measure the type and extent of clay hydration.Based on the relationship between low field NMR T2 relaxation spectrum and the mobility of water molecules,the total signal amplitude of the T2 peak is used to determine the total water content in clay,the ranges of T2 values to determine the types of clay hydration,and the area of the T2 peak to determine the contents of three kinds of water.Laboratory experiments showed that the strongly bound water,weakly bound water and free water in water-saturated clay have T2 values ranging in 0.001-0.1 ms,0.1-15 ms and 15-200 ms,respectively,corresponding to the contents of the three kinds of water,which are 14.83%,67.69% and 17.48%,respectively.The T2 relaxation spectrum also intuitively demonstrates that temperature buildup drives water molecules in clay from low degree of freedom to high degree of freedom.BPEI with 8 amino groups is able to dispel more than 90% of the strongly and weakly bound water and all the free water from clay.

关键词

泥页岩/表面水化/低场核磁/定量/井壁稳定

Key words

Mud shale/Surface hydration/Low field nuclear and magnet/Quantitative/Borehole wall stabilization

分类

能源科技

引用本文复制引用

苏俊霖,董汶鑫,冯杰,杨培强,罗平亚..黏土表面结合水的低场核磁共振定量研究[J].钻井液与完井液,2018,35(1):8-12,5.

基金项目

国家科技重大专项“页岩气水平井水基钻井液技术研究”(2016ZX05002001-001) (2016ZX05002001-001)

中石油重大应用基础研究“井筒工作液新材料新体系基础研究”(2016A-3903). (2016A-3903)

钻井液与完井液

OA北大核心CSTPCD

1001-5620

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