西南石油大学学报(自然科学版) ›› 2018, Vol. 40 ›› Issue (5): 84-94.DOI: 10.11885/j.issn.1674-5086.2017.07.26.04

• 地质勘探 • 上一篇    下一篇

宜宾地区页岩微孔特征及吸附解吸特性研究

岳长涛, 李术元, 许心怡, 马跃, 杨飞   

  1. 中国石油大学(北京)理学院, 北京 昌平 102249
  • 收稿日期:2017-07-26 出版日期:2018-10-01 发布日期:2018-10-01
  • 通讯作者: 李术元,E-mail:syli@cup.edu.cn
  • 作者简介:岳长涛,1977年生,男,汉族,山东德州人,教授,主要从事应用化学方面的研究工作。E-mail:yuect@cup.edu.cn;李术元,1959年生,男,汉族,山东诸城人,教授,主要从事石油化学和固体燃料化学方面的研究工作。E-mail:syli@cup.edu.cn;许心怡,1992年生,女,汉族,辽宁本溪人,硕士,主要从事应用化学方面的研究工作。E-mail:xxyiCUP@sina.com;马跃,1984年生,男,汉族,天津人,讲师,主要从事新能源化学等研究工作。E-mail:yuem@cup.edu.cn;杨飞,1992年生,男,汉族,陕西延安人,硕士,主要从事应用化学方面的研究工作。E-mail:ygfei0301@163.com
  • 基金资助:
    国家自然科学基金(41372152)

Micropore Characteristics and Adsorption and Desorption Properties of Shales in the Yibin Region

YUE Changtao, LI Shuyuan, XU Xinyi, MA Yue, YANG Fei   

  1. College of Science, China University of Petroleum(Beijing), Changping, Beijing 102249, China
  • Received:2017-07-26 Online:2018-10-01 Published:2018-10-01

摘要: 选取四川宜宾地区志留系龙马溪组页岩,对总有机碳、黏土矿物含量等储层性质进行表征。利用扫描电镜、高压压汞法、低温氮气吸附-解吸法和二氧化碳气体吸附法对孔隙结构特征进行定性和定量分析。采用质量法对页岩样品进行不同温度时的等温吸附和解吸实验,结合吸附势理论对吸附解吸过程进行解释。结果表明,页岩样品TOC较高,页岩样品主要以微孔为主,介孔次之,大孔发育较少;微孔和介孔的发育增大了页岩的表面积,提供了更多的吸附位,有利于页岩气的吸附。页岩样品等温吸附曲线表明,随着压力的增大,吸附量先迅速增大而后逐渐趋于稳定,解吸曲线与吸附曲线相似并存在滞后现象;TOC与页岩吸附性能有着较好的正相关性;吸附势能曲线中势能零点与吸附曲线的拐点基本一致,通过吸附势的变化可以解释吸附解吸过程中页岩气的赋存状态。

关键词: 页岩气, 微孔特征, 等温吸附, 等温解吸, 吸附势

Abstract: Shales of the Silurian Longmaxi Formation in the Yibin Region, Sichuan, were investigated and their geological parameters, including total organic carbon (TOC) contents and clay mineral contents, were measured. Scanning electron microscopy, high pressure mercury injection, low temperature nitrogen adsorption-desorption, and carbon dioxide gas adsorption methods were employed to qualitatively and quantitatively analyze pore structure characteristics. The mass method was utilized to conduct isothermal adsorption and desorption experiments on shale samples at different temperatures and adsorption and desorption processes were explained using the adsorption potential theory. The results demonstrate that these shale samples have relatively high TOC contents, and pore structures are dominated by micropores, followed by mesopores and macropores. Connected micropores and mesopores increase surface areas of shales, and provide more adsorption spaces, thus facilitating adsorption of shale gas. The isothermal adsorption curves of the shale samples reveal that as the pressure increases, the adsorption volume increases rapidly at first and then levels off gradually. The desorption curves resemble the adsorption ones, but show some delays. The TOC contents indicate relatively good positive correlations with the adsorption performances of shales. The zero-potential point of the absorption potential curve is generally consistent with the turning point of the adsorption curve. The occurrence of shale gas during adsorption and desorption can be explained by variations in adsorption potentials.

Key words: shale gas, micropore characteristic, isothermal adsorption, isothermal desorption, adsorption potential

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