煤炭工程 ›› 2016, Vol. 48 ›› Issue (3): 119-122.doi: 10.11799/ce201603037

• 研究探讨 • 上一篇    下一篇

基于分形理论的龙口褐煤孔隙特征研究

邵培,王爱宽   

  1. 中国矿业大学
  • 收稿日期:2015-07-16 修回日期:2015-09-06 出版日期:2016-03-10 发布日期:2016-04-08
  • 通讯作者: 王爱宽 E-mail:wake198110@163.com

Studying on Pore Characteristics of Longkou Lignite based on Fractal Theory

  • Received:2015-07-16 Revised:2015-09-06 Online:2016-03-10 Published:2016-04-08

摘要: 基于压汞实验测试结果,运用分形理论,研究龙口褐煤的孔隙大小分级、孔隙发育特征以及孔隙分形维数。结果表明:龙口褐煤的孔隙系统可以分为三个部分,孔径大于1028nm的孔隙属于大孔,孔径小于72nm的孔隙属于微小孔,介于72nm和1028nm的孔隙属于过渡孔|孔隙度介于10%~15%,平均为12.669%,比孔容介于0.09~0.13mL/g,平均为0.115mL/g,比表面积介于39~70m2/g,平均为56.529m2/g,煤样的孔隙发育较好,且具有较大的孔容和表面积,其中微小孔的孔容占总孔容的80%以上,且分布均匀|大孔和过渡孔具有很好的孔隙分形分维特征,分形维数平均为2.56,表明这部分孔隙有较好的孔隙结构。

关键词: 龙口褐煤, 压汞实验, 分形理论, 孔隙特征

Abstract: Based on pressured-mercury testing and fractal theory, studying on pore size classification, pore development characteristics and pore fractal dimension. The results showed that the pore system of Longkou lignite was divided into three parts. The pore with a radius over 1028nm was macro pore; the pore with a radius less than 72nm was micro pore; and the pore with a radius of 72~1028nm was transition pore. The porosity ranged from 10% to 15%, and the mean was 12.669%. The specific pore volume ranged from 0.09ml/g~0.13ml/g, and the mean was 0.115ml/g. The specific surface area was between 39m2/g and 70m2/g, and the mean was 56.529m2/g. The pore development of coal sample was great, and pore volume and surface area were large. The pore volume of micro pore was more than 80% of the total capacity, and micro pore was spread more evenly. The fractal characteristics of macro pore and transition pore was very good and the average fractal dimension was 2.56, which showed that this part of pore had greater pore structure and permeability was better.

中图分类号: