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一种泥页岩脆裂性质表征方法及其地质意义

鲍云杰 杨振恒 杨琦 陈红宇 付小东 王杰

石油实验地质Issue(6):694-697,4.
石油实验地质Issue(6):694-697,4.DOI:10.11781/sysydz201306694

一种泥页岩脆裂性质表征方法及其地质意义

One kind of brittle shale characterization method and its geological significance

鲍云杰 1杨振恒 2杨琦 1陈红宇 2付小东 1王杰2

作者信息

  • 1. 中国石油化工股份有限公司 石油勘探开发研究院 无锡石油地质研究所,江苏 无锡 214126
  • 2. 中国石油化工集团公司 油气成藏重点实验室,江苏 无锡 214151
  • 折叠

摘要

Abstract

The paper presents one kind of brittle shale characterization method:brittle index, and introduces the determination process and procedure for the index. This method is simple to operate, and has no special require-ments for sample size and shape, hence has universal significance for shale sample test. Experimental data show that the brittle index is positively correlated to porosity and specific surface area. According to measurement process, method, experimental data and literature analysis, the brittle index can characterize the extent and in-ternal structure of porosity, especially the potential application for micro pores and cracks. The prospects for the application of brittle index in the studies of shale internal structure and gas desorption are discussed preliminarily.

关键词

脆裂性质/脆裂指数/比表面积/解吸/泥页岩/页岩气

Key words

brittle nature/brittle index/specific surface area/desorption/shale/shale gas

分类

能源科技

引用本文复制引用

鲍云杰,杨振恒,杨琦,陈红宇,付小东,王杰..一种泥页岩脆裂性质表征方法及其地质意义[J].石油实验地质,2013,(6):694-697,4.

基金项目

中国石化江汉油田分公司科研项目“湘鄂西地区河页1井页岩含气性研究”( G0605-10-ZS-0041)资助。 ()

石油实验地质

OA北大核心CSCDCSTPCD

1001-6112

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