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四川盆地平桥地区五峰—龙马溪组页岩微观孔隙特征研究

王运海

石油实验地质2018,Vol.40Issue(3):337-344,8.
石油实验地质2018,Vol.40Issue(3):337-344,8.DOI:10.11781/sysydz201803337

四川盆地平桥地区五峰—龙马溪组页岩微观孔隙特征研究

Micro?pore characteristics of shale from Wufeng-Longmaxi formations in Pingqiao area, Sichuan Basin

王运海1

作者信息

  • 1. 中国石化 华东油气分公司,南京 210011
  • 折叠

摘要

Abstract

The microscopic pore characteristics of shale from the lower Wufeng-Longmaxi formations in the Pingqiao area of the Sichuan Basin were studied using argon ion polished sample scanning electron microscopy and nitrogen adsorption-desorption experiments. Organic-rich siliceous shale and carbonaceous shale micro-pores are dominated by organic pores and micro-cracks. The pore structure is relatively complex, with rich pore morphology and a wide range of pore sizes. Argon ion polishing scanning electron microscopy showed that the organic pores are mainly thin and partly belong to micro-pores. Nitrogen adsorption-desorption experiments showed that the shale has narrow parallel plate-like holes, a small number of conical plate holes and wedge-shaped holes with a poor connectivity,and regular open round holes and ink bottle-shaped holes with open ends. The specific surface area measured by nitrogen adsorption-desorption experiments was 9-32.6 m2/g, with an average of 18.0 m2/g,which was low. The pore diameters measured by the BET method were 3.23 to 4.35 nm, and the average pore volume by the BJH method was 0.016 5 cm3/g. The fine meso-pores were dominant, and they were biased toward the micro-pore boundary. According to the comprehensive analysis, the microscopic pores of shale reservoirs in the study area are mainly mesoporous, and meso-pores and micro-pores contribute most of the specific surface area.

关键词

孔隙类型/孔隙结构/页岩/五峰—龙马溪组/四川盆地

Key words

pore type/pore structure/shale/Wufeng-Longmaxi formations/Sichuan Basin

分类

能源科技

引用本文复制引用

王运海..四川盆地平桥地区五峰—龙马溪组页岩微观孔隙特征研究[J].石油实验地质,2018,40(3):337-344,8.

基金项目

国家科技重大专项项目(2016ZX05061)"彭水地区常压页岩气勘探开发示范工程"资助. (2016ZX05061)

石油实验地质

OA北大核心CSCDCSTPCD

1001-6112

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