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Accessibility of pores in coal to methane and carbon dioxide

机译:煤中的气孔易接近甲烷和二氧化碳

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摘要

Fluid-solid interactions in natural and engineered porous solids underlie a variety of technological pro cesses, including geological storage of anthropogenic greenhouse gases, enhanced coal bed methane recovery, membrane separation, and heterogeneous catalysis. The size, distribution and interconnectivity of pores, the chemical and physical properties of the solid and fluid phases collectively dictate how fluid molecules migrate into and through the micro- and meso-porous media, adsorb and ultimately react with the solid surfaces. Due to the high penetration power and relatively short wavelength of neutrons, small-angle neutron scattering (SANS) as well as ultra small-angle scattering (USANS) techniques are ideally suited for assessing the phase behavior of confined fluids under pressure as well as for evaluating the total porosity in engineered and natural porous systems including coal. Here we demonstrate that SANS and USANS can be also used for determining the fraction of the pore volume that is actually accessible to fluids as a function of pore sizes and study the fraction of inaccessible pores as a function of pore size in three coals from the Illinois Basin (USA) and Bowen Basin (Australia). Experiments were performed at CO_2 and methane pressures up to 780 bar, including pressures corresponding to zero average contrast condi tion (ZAC), which is the pressure where no scattering from the accessible pores occurs. Scattering curves at the ZAC were compared with the scattering from same coals under vacuum and analysed using a newly developed approach that shows that the volume fraction of accessible pores in these coals varies between ~90% in the macropore region to ~30% in the mesopore region and the variation is distinctive for each of the examined coals. The developed methodology may be also applied for assessing the volume of acces sible pores in other natural underground formations of interest for CO_2 sequestration, such as saline aqui fers as well as for estimating closed porosity in engineered porous solids of technological importance.
机译:天然和工程多孔固体中的流固相互作用是多种技术过程的基础,包括人为温室气体的地质存储,增强的煤层甲烷回收率,膜分离和非均相催化作用。孔的大小,分布和相互连通性,固相和流体相的化学和物理性质共同决定了流体分子如何迁移到微孔和中孔介质中并通过微孔和中孔介质,如何吸附并最终与固体表面反应。由于中子具有较高的穿透能力和相对较短的波长,小角度中子散射(SANS)以及超小角度散射(USANS)技术非常适合评估承压流体在压力下的相态以及评估包括煤在内的工程和天然多孔系统的总孔隙度。在这里,我们证明了SANS和USANS还可以用于确定流体实际可访问的孔隙体积分数与孔径的函数,并研究伊利诺伊州三种煤中不可访问的孔隙分数与孔径的关系。盆地(美国)和鲍文盆地(澳大利亚)。实验是在高达780 bar的CO_2和甲烷压力下进行的,其中包括对应于零平均对比度条件(ZAC)的压力,该压力为从可进入的孔中不发生散射的压力。将ZAC处的散射曲线与相同煤在真空下的散射进行比较,并使用新开发的方法进行分析,结果表明,这些煤中可到达的孔隙的体积分数在大孔区域的〜90%到中孔的〜30%之间变化区域和变化对于每种被检查的煤来说都是独特的。所开发的方法还可以用于评估其他自然感兴趣的自然地下地层中可封存的孔隙的数量,以封存CO_2,例如盐水层,以及估计具有技术重要性的工程多孔固体中的封闭孔隙度。

著录项

  • 来源
    《Fuel》 |2012年第1期|p.200-208|共9页
  • 作者单位

    Neutron Scattering Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA,Department of Physics and Astronomy, University of Tennessee, Knoxville, TN 37996, USA;

    Neutron Scattering Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA;

    CSIRO Energy Technology, 11 Julius Avenue, North Ryde, 2113 NSW, Australia;

    (375 H.L. Hunter Laboratories, Clemson University, Clemson, SC 29634-0973, USA;

    Nanoscale Science and Technology Centre, Griffith University, Nathan 4111, Brisbane, Australia;

    Indiana Geological Survey, Indiana University, Bloomington, IN 47405-2208, USA;

    Nanoscale Science and Technology Centre, Griffith University, Nathan 4111, Brisbane, Australia,Indiana Geological Survey, Indiana University, Bloomington, IN 47405-2208, USA;

    Sandia National Laboratories, Livermore, CA 94551, USA,Joint BioEnergy Institute, Emeryville, CA 94608, USA;

    Center for Neutron Research, National Institute of Standards and Technology, Gaithersburg, MD 20899, USA;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    coal; accessible pores; CO_2; methane; small-angle neutron scattering;

    机译:煤;可通孔;CO_2;甲烷;小角中子散射;

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