天然气地球科学 ›› 2021, Vol. 32 ›› Issue (1): 125–135.doi: 10.11764/j.issn.1672-1926.2020.06.003

• 非常规天然气 • 上一篇    下一篇

甲烷吸附前后高煤级煤孔隙结构粒径效应

李腾1,2(),吴财芳3,4   

  1. 1.西安石油大学石油工程学院,陕西 西安 710065
    2.西安石油大学陕西省油气田特种增产技术重点实验室,陕西 西安 710065
    3.中国矿业大学资源与地球科学学院,江苏 徐州 221116
    4.中国矿业大学煤层气资源与成藏过程教育部重点实验室,江苏 徐州 221116
  • 收稿日期:2020-04-29 修回日期:2020-06-10 出版日期:2021-01-10 发布日期:2021-02-04
  • 作者简介:李腾(1989-),男,河南洛阳人,讲师,博士,主要从事非常规油气储层评价研究.E-mail: liteng2052@163.com.
  • 基金资助:
    国家科技重大专项“多煤层煤层气甜点选区选段技术”(2016ZX05044-001);陕西省自然科学基础研究计划(2019JQ-527);陕西省教育厅科研计划项目(20JS116)

The grain size effect on pore structure characteristics of high-rank coal before and after the methane adsorption

Teng LI1,2(),Cai-fang WU3,4   

  1. 1.College of Petroleum Engineering,Xi’an Shiyou University,Xi’an 710065,China
    2.Shaanxi Key Laboratory of Advanced Stimulation Technology for Oil & Gas Reservoirs,Xi’an Shiyou University,Xi’an 710065,China
    3.School of Mineral Resources and Geosciences,China University of Mining & Technology,Xuzhou 221116,China
    4.Key Laboratory of Coalbed Methane Resources and Reservoir Formation Process,Ministry of Education,Xuzhou 221116,China
  • Received:2020-04-29 Revised:2020-06-10 Online:2021-01-10 Published:2021-02-04
  • Supported by:
    The China National Science and Technology Major Project(2016ZX05044-001);The Natural Science Basic Research Plan of Shaanxi Province of China(2019JQ-527);The Scientific Research Program Funded by Shaanxi Provincial Education Department(20JS116)

摘要:

针对3种不同粒径的高煤级煤开展了甲烷高压等温吸附测试,并对不同粒径煤样甲烷吸附前后的孔隙结构特征进行了对比研究。结果表明,不同粒径煤样的等温吸附曲线没有显著的差异,随着煤岩粒径的减小,煤岩的吸附速率和最大过剩吸附量呈逐渐增加的趋势。甲烷吸附前后,不同粒径煤样的孔隙结构发生了不同的变化。甲烷等温吸附前,随着煤岩粒径的减小,低温液氮吸附滞后环开度呈逐渐减小的趋势,等效吸附率曲率则先减小后增大;甲烷吸附后,DY?5煤样的低温液氮吸附滞后环开度减小,而DY?6煤样和DY?7煤样的低温液氮吸附滞后环开度有所增加,说明甲烷吸附对小粒径煤样中孔和大孔的影响较为显著。甲烷的吸附作用对各阶段孔隙均有影响。大粒径煤样在甲烷吸附作用影响下,孔隙连通性得以改善,而小粒径煤样在甲烷吸附作用后孔隙分布更加的集中。

关键词: 高煤级煤, 甲烷吸附, 粒径效应, 孔隙结构

Abstract:

Methane isothermal adsorption experiments were carried out on the high rank coal samples with three different particle sizes, and dynamic change of the pore structure was measured with the low temperature N2 adsorption and the low temperature CO2 adsorption before and after the methane adsorption. The results show that the adsorption isothermal curves of the various grain sizes coal samples present no significant differences, the adsorption rate and maximum excess adsorption capacity increase with the decreasing particle sizes. Before the methane isothermal adsorption, the d(qde-qad)' decreases with the decreasing grain sizes, while that for the equivalent desorption rate curvatures decrease first and then increase. After the methane adsorption, the d(qde-qad)' for DY-5 coal sample decreases, while that for the DY-6 and DY-7 coal samples feature the contrary characteristics, indicating that the methane adsorption has a significant influence on the meso- and macropore structure for the small grain size coal samples. In fact, the methane adsorption could change the pore structures in the coal at all stages. For the coal samples with larger grain size, the pore connectivity is enhanced, while that for the coal samples with smaller grain sizes, the distribution of the pores would be more concentrate after the methane adsorption.

Key words: High-rank coal, Methane isothermal adsorption, Grain sizes effect, Pore structure

中图分类号: 

  • TE122

图1

研究区构造纲要(a)及岩性柱状图(b)"

表1

不同粒径煤样工业分析"

样品号粒度/目Ro,max/%工业分析/%
MadAdVdafFCad
DY-540~603.131.848.418.0282.69
DY-660~801.908.648.2482.24
DY-780~1001.829.158.2581.84

图2

空白测试中ρHe与M1b线性负相关散点图"

图3

不同粒径煤样浮力测试ρHe与M1线性负相关散点图"

图4

不同粒径煤样等温吸附曲线"

图5

不同粒径煤样甲烷吸附前后低温液氮吸附—脱附曲线"

图6

不同粒径煤样甲烷吸附前后低温液氮吸附滞后环开度"

图7

不同粒径煤样甲烷吸附前后低温二氧化碳吸附曲线"

图8

不同粒径煤样甲烷吸附前后等效吸附率斜率曲线"

图9

不同粒径煤样甲烷吸附前后中孔、大孔孔容、孔比表面积柱状对比"

图10

煤样扫描电镜"

图11

不同粒径煤样甲烷吸附前后微孔孔容、孔比表面积柱状对比"

表2

煤样Dq谱多重分形特征"

样品吸附前后吸附类型D-10D0D1D2D10D-10D10D0D10D-10D0
DY-5吸附前液氮吸附1.5210.950.90510.840.680.160.52

二氧化碳

吸附

1.4010.830.660.440.960.560.40
吸附后液氮吸附1.1810.980.960.900.270.100.18

二氧化碳

吸附

1.2210.880.750.580.650.420.22
DY-6吸附前液氮吸附1.3510.960.920.860.490.140.35

二氧化碳

吸附

1.2310.850.690.500.730.500.23
吸附后液氮吸附1.0810.940.880.680.400.320.08

二氧化碳

吸附

1.2310.870.730.520.700.480.23
DY-7吸附前液氮吸附1.4210.990.980.940.480.060.42

二氧化碳

吸附

1.2310.850.710.530.710.470.23
吸附后液氮吸附1.3110.960.920.840.480.160.31

二氧化碳

吸附

1.2310.850.710.480.750.520.23

图12

不同粒径煤样甲烷吸附前后D1、D2变化曲线"

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[2] 马立祥;. 断层封闭性研究在烃类聚集系统分析中的意义[J]. 天然气地球科学, 2000, 11(3): 1 -8 .
[3] 马立祥. 岩石物理流动单元的概念及其研究现状[J]. 天然气地球科学, 2000, 11(2): 30 -36 .
[4] 李在光;杨占龙;李琳;郭精义;黄云峰;吴青鹏;李红哲;. 胜北地区油气分布规律[J]. 天然气地球科学, 2006, 17(1): 94 -96 .
[5] 王杰,刘文汇,秦建中,张隽. 中国东部幔源气藏存在的现实性与聚集成藏的规律性[J]. 天然气地球科学, 2007, 18(1): 19 -26 .
[6] 李亮,万晓龙,李志伟,张永强,张振红. 油气成藏模拟实验在白于山油藏开发中的应用[J]. 天然气地球科学, 2006, 17(2): 219 -222 .
[7] 李广之;袁子艳;胡斌;邓天龙;. 利用顶空气技术判别凝析气(油)储层[J]. 天然气地球科学, 2006, 17(3): 309 -312 .
[8] 李凤杰;王多云;. 鄂尔多斯盆地西峰油田延长组高分辨率层序地层学研究[J]. 天然气地球科学, 2006, 17(3): 339 -344 .
[9] 赵孟军;宋岩;柳少波;秦胜飞;洪峰;傅国友;达江;. 中国中西部前陆盆地成藏特征的初步分析[J]. 天然气地球科学, 2006, 17(4): 445 -451 .
[10] 姚亚明;周继军;何明喜;付代国;陈建军;. 对焉耆盆地油气地质条件的认识[J]. 天然气地球科学, 2006, 17(4): 463 -467 .