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Molecular Simulations of Methane Adsorption Behavior in Illite Nanopores Considering Basal and Edge Surfaces

机译:考虑基面和边缘表面的伊利石纳米孔中甲烷吸附行为的分子模拟

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摘要

The adsorption properties of methane (CH4) have a great influence on shale gas exploration and development. The surface chemistry characteristics of nanopores are key factors in adsorption phenomena. The clay pores in shale formations exhibit basal surface and edge surfaces (mainly as A and C chain and B chain surfaces in illite). Little research regarding CH4 adsorption on clay edge surfaces has been carried out despite their distinct surface chemistries. In this work, the adsorption of CH4 confined in nanoscale illite slit pores with basal and edge surfaces was investigated by grand canonical Monte Carlo and molecular dynamics simulations. The adsorbed phase density, adsorption capacity, adsorption energy, isosteric heat of adsorption, and adsorption sites were calculated and analyzed. The simulated adsorption capacity compares favorably with the available experimental data. The results show that the edge surfaces have van der Waals interactions that are weaker than those of the basal surfaces. The adsorption capacity follows the order basal surface B chain surface A and C chain surface. However, the differences of adsorption capacity between these surfaces are small; thus, edge surfaces cannot be ignored in shale formation. Additionally, we confirmed that the adsorbed phase has a thickness of approximately 0.9 nm. The pore size determines the interaction overlap strength on the gas molecules, and the threshold value of the pore size is about 2 nm. The preferential adsorption sites locate differently on edge and basal surfaces. These findings could provide deep insights into CH4 adsorption behavior in natural illite-bearing shales.
机译:甲烷(CH4)的吸附特性对页岩气的勘探和开发有很大的影响。纳米孔的表面化学特征是吸附现象的关键因素。页岩地层中的粘土孔隙表现出基面和边缘表面(主要是伊利石中的A和C链和B链表面)。尽管CH4吸附在粘土边缘表面上,但它们的表面化学性质不同,却很少进行研究。在这项工作中,通过大正则蒙特卡罗法和分子动力学模拟研究了局限在具有基面和边缘表面的纳米级伊利石狭缝孔中的CH4的吸附。计算并分析了吸附相的密度,吸附容量,吸附能,等规吸附热和吸附部位。模拟的吸附容量与现有的实验数据相比具有优势。结果表明,边缘表面的范德华相互作用弱于基面。吸附能力依次为基面> B链表面> A和C链表面。但是,这些表面之间的吸附能力差异很小;因此,在页岩形成过程中不能忽略边缘表面。此外,我们证实了吸附相的厚度约为0.9 nm。孔径决定了在气体分子上的相互作用重叠强度,并且孔径的阈值约为2nm。优先吸附位在边缘和基面上的位置不同。这些发现可以为深入了解天然伊利石页岩中CH4的吸附行为提供深刻的见解。

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  • 来源
    《Energy & fuels》 |2018年第4期|4783-4796|共14页
  • 作者单位

    Univ Sci & Technol China, Dept Modern Mech, Hefei 230026, Anhui, Peoples R China;

    Univ Sci & Technol China, Dept Phys Chem, Hefei 230026, Anhui, Peoples R China;

    Shanghai Univ Engn Sci, Sch Mech Engn, Shanghai 201620, Peoples R China;

    Univ Sci & Technol China, Dept Phys Chem, Hefei 230026, Anhui, Peoples R China;

    Hefei Univ Technol, Dept Math, Hefei 230009, Anhui, Peoples R China;

    Univ Sci & Technol China, Dept Modern Mech, Hefei 230026, Anhui, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);
  • 原文格式 PDF
  • 正文语种 eng
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