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淮南煤田煤系泥页岩组成特征及吸附性能

  • 卜红玲 ,
  • 琚宜文 ,
  • 王国昌 ,
  • 房立志 ,
  • 颜志丰 ,
  • 李清光
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  • 中国科学院大学地球科学学院 中国科学院计算地球动力学重点实验室, 北京 100049

收稿日期: 2014-02-20

  修回日期: 2014-03-25

  网络出版日期: 2015-01-15

基金资助

国家自然科学基金(41372213,41030422,40972131)、中国科学院战略性先导科技专项(XDA05030100)和国家科技重大专项(2011ZX05060-005,2011ZX05039-004)资助

Composition and adsorptivity of shales in coal-bearing rock strata of Huainan coalfield

  • BU Hongling ,
  • JU Yiwen ,
  • WANG Guochang ,
  • FANG Lizhi ,
  • YAN Zhifeng ,
  • LI Qingguang
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  • Key Laboratory of Computational Geodynamics of Chinese Academy of Sciences College of Earth Science, University of Chinese Academy of Sciences, Beijing 100049, China

Received date: 2014-02-20

  Revised date: 2014-03-25

  Online published: 2015-01-15

摘要

通过泥页岩有机质和矿物的定性定量分析,研究淮南煤田煤系地层泥页岩组成特征及吸附性能.结果如下.1)研究区泥页岩TOC含量为0.13%~8.58%,平均含量为1.98%;有机质类型以Ⅲ型为主,少量Ⅱb型;Ro值为0.61%~1.48%,平均值0.93%;矿物主要为粘土矿物和石英,粘土矿物以高岭石和伊/蒙混层矿物为主.2)TOC含量增加,吸附量增大;Ro值增加,单位TOC的最大吸附量增加;粘土矿物吸附性与其类型有关系.3)脆性和脆-韧性变形的泥页岩等温吸附特征不同.

本文引用格式

卜红玲 , 琚宜文 , 王国昌 , 房立志 , 颜志丰 , 李清光 . 淮南煤田煤系泥页岩组成特征及吸附性能[J]. 中国科学院大学学报, 2015 , 32(1) : 82 -90 . DOI: 10.7523/j.issn.2095-6134.2015.01.014

Abstract

Based on qualitative and quantitative analyses of organic and mineral in shales, the composition geological characteristics and adsorptivity of shales in coal-bearing strata were systematically studied in Huainan mining area. Results are given below, 1) TOC content of shale in study area varies between 0.13% and 8.58% with the average content of 1.98%; the organic matter type is mainly Ⅲ and a little Ⅱb; thermal maturity of organic matter ranges from 0.61% to 1.48% with the average of 0.93%; and mineral composition of shale mainly consists of clay minerals and quartz and kaolinite and mixed layer illite/smectite (I/S) are the staple clay types. 2) Adsorption capacity increases with TOC content, and the maximum adsorption amount per unit TOC increases with Ro value; and the adsorptivity of clay mineral is associated with its type. 3) Brittle deformed shale and brittle-ductile deformed shale have different adsorption isotherm characteristics.

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