罗磊, 汤达祯, 陶树, 等. 准东低阶煤孔隙特征及对气体传质方式的影响[J]. 煤炭学报, 2016, (4). DOI: 10.13225/j.cnki.jccs.2015.0702
引用本文: 罗磊, 汤达祯, 陶树, 等. 准东低阶煤孔隙特征及对气体传质方式的影响[J]. 煤炭学报, 2016, (4). DOI: 10.13225/j.cnki.jccs.2015.0702
LUO Lei, TANG Da-zhen, TAO Shu, et al. Pore structure and its influence on gas mass transfer of low rank coal in Eastern Junggar Basin,Xinjiang[J]. Journal of China Coal Society, 2016, (4). DOI: 10.13225/j.cnki.jccs.2015.0702
Citation: LUO Lei, TANG Da-zhen, TAO Shu, et al. Pore structure and its influence on gas mass transfer of low rank coal in Eastern Junggar Basin,Xinjiang[J]. Journal of China Coal Society, 2016, (4). DOI: 10.13225/j.cnki.jccs.2015.0702

准东低阶煤孔隙特征及对气体传质方式的影响

Pore structure and its influence on gas mass transfer of low rank coal in Eastern Junggar Basin,Xinjiang

  • 摘要: 准东以褐煤和长焰煤为主,属于低灰、高挥发分煤;显微组分镜质组占优,惰质组次之,偶见腐泥组分;褐煤惰质组含量远大于长焰煤,且水分含量也高于后者。根据非润湿相的汞侵入毛管获得的孔隙分布和BET模型得出微小孔特征。在此基础上,并对甲烷在不同尺度孔隙中的传质方式进行探讨。结果显示:褐煤以中大孔为主,微小孔发育有限,主要储集空间孔径在0.1~2.0μm;长焰煤以微小孔为主,孔容主要来自微小孔,其单位孔容远小于褐煤。在多级孔隙配置的煤储层中划分出达西流、滑脱流、过渡流和分子扩散4种传质方式。褐煤孔隙连通性好,以达西流、滑脱渗流为主;长焰煤微小孔发育,各级孔隙连通性差,以达西流、过渡流及分子扩散为主。相比较而言,纳米级孔隙中吸附甲烷分子层厚及滑脱效应对长焰煤单孔渗流能力的影响更显著,其将会在气藏开发过程中对增产稳产提供有益的支持。

     

    Abstract: The complexity of pore structure of low rank coal has a deep impact on methane storage status,gas transfer and estimated coalbed methane (CBM) resources. According to coal petrology research,the result shows that the coal rank is mainly sub-bituminous A ( Ro = 0. 42% -0. 59% ),the components of maceral and its properties are mainly constituted by vitrinite (51. 7% -79. 0% ),followed by inertinite (15. 2% -45. 5% ),and it has sporadic sapropelin- ite,generally the volatile matter content accounts for more than 30% . However the inertinite content and the moisture content of lignite are far greater than that of long flame coal. The characteristic and distribution of pore in both lignite and long flame coal were determined by using mercury injection and nitrogen adsorption,and the methods of methane mass transfer in different scales of pore throat were analyzed. The results show that the pore features and distribution of lignite and long flame coal show obvious differences in mercury intrusion and nitrogen adsorption testing,although the lignite coal and long flame coal are classified as the low rank coal. Lignite coal gives priority to macroporous develop- ment,micro pore volume is limited. The pore feature of long flame coal is dominated by micro pore,which has less unit pore volume than lignite. The reservoir space of lignite mainly distributes with pore throats ranging from 0. 1 μm to 2 μm. The pore volume of long flame coal is mainly made up of micro pore by nitrogen adsorption test. Based this study,combining with the law of gas mass transfer,the study identified four types of mass transfer at multi-scale pore configuration in the coal reservoir,including Darcy flow,slippage effect flow,transition flow and molecular diffusion. The different pore characteristics of long flame coal and lignite make the mass transfer modes be not the same. The lim- ited growth of micro pore of lignite,in which the seepage pores are well connected,gives priority to Darcy flow and slip flow. The micro pore developed well in long flame coal,but the seepage pores are not well connected,and the mass transfer manners dominated by Darcy flow,transition flow and molecular diffusion. The thickness of adsorption methane and slippage effect both have significantly effect on nano pore seepage ability in long flame coal,which could provide a useful support to a stable production at the later period of CBM development.

     

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