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有机酸溶蚀作用对泥页岩储层孔隙结构的影响

罗瑞 查明 何皓 高长海 曲江秀 张勇 朱文慧 孙冲

中国石油大学学报(自然科学版)2017,Vol.41Issue(2):49-59,11.
中国石油大学学报(自然科学版)2017,Vol.41Issue(2):49-59,11.DOI:10.3969/j.issn.1673-5005.2017.02.006

有机酸溶蚀作用对泥页岩储层孔隙结构的影响

Effect of mineral dissolution by organic acids on pore structure of shale reservoir

罗瑞 1查明 1何皓 2高长海 1曲江秀 1张勇 2朱文慧 2孙冲2

作者信息

  • 1. 中国石油大学地球科学与技术学院,山东青岛266580
  • 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
  • 折叠

摘要

Abstract

In order to know the dissolution of common mineral ions in shale dissolved by organic acid,the impact of dissolution on secondary pore structure of shale was investigated,in which the dissolution experiments were designed on shale samples from the member 3 of Shahejie Formation of Paleogene in Nanpu sag with different types of organic acids (acetic acid and oxalic acid) and different temperatures.The plasma-atomic emission spectrometry was conducted on the solution after the reaction.Also,the X-ray diffraction,scanning electron microscopy and low-temperature nitrogen adsorption analysis were conducted on dissolved samples.The results show that dissolution of common mineral ions in shale with increasing reaction temperature has two situations,which are " increase,decrease,compound and little" by acetic acid,and "increase,decrease,compound" by oxalic acid respectively.And different ions show different dissolution coefficients.In general,the organic acid dissolution of shale shows obvious positive correlation with temperature.And different types of organic acids show different dissolution mechanisms on shale significantly.In the dissolved shale,the size and distribution of intragranular pore in shale increase.It is also found that the small scale of erosion occurs in the contact part of intergranular pore,resulting in net-pore phenomenon and increased width of micro crack.Also the accompanied new-born clay minerals are formed,such as illite,kaolinite and montmorillonite.The acetic dissolution promotes the formation of microporeand mesoporein the shale,which increases the surface area.Meanwhile oxalic acid dissolution results in the formation of mesopore and macropore,which increases the average pore size of the shale.The preliminary determination of shale porosity enhancement by organic acid dissolution shows the limited capacity of enhancing porosity,which is not as significant as expected.

关键词

有机酸/溶蚀作用/离子释放/泥页岩孔隙结构/增孔效应

Key words

organic acids/dissolution/ions release/shale pore structure/porosity enhancement effect

分类

天文与地球科学

引用本文复制引用

罗瑞,查明,何皓,高长海,曲江秀,张勇,朱文慧,孙冲..有机酸溶蚀作用对泥页岩储层孔隙结构的影响[J].中国石油大学学报(自然科学版),2017,41(2):49-59,11.

基金项目

国家“973”计划项目(2014CB239005) (2014CB239005)

国家重大科技专项(2011ZX05001-001-006) (2011ZX05001-001-006)

山东省自然科学基金项目(ZR2013DM016) (ZR2013DM016)

中国石油大学学报(自然科学版)

OA北大核心CSCDCSTPCD

1673-5005

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