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用巨正则和正则动力学蒙特卡罗方法模拟表面和狭缝孔隙中的气体吸附。

Simulation of gas adsorption on a surface and in slit pores with grand canonical and canonical kinetic Monte Carlo methods.

机构信息

Ioffe Physical Technical Institute, 26 Polytechnicheskaya, St. Petersburg 194021, Russia.

出版信息

Phys Chem Chem Phys. 2012 Aug 21;14(31):11112-8. doi: 10.1039/c2cp41235g. Epub 2012 Jul 6.

Abstract

We present for the first time in the literature a new scheme of kinetic Monte Carlo method applied on a grand canonical ensemble, which we call hereafter GC-kMC. It was shown recently that the kinetic Monte Carlo (kMC) scheme is a very effective tool for the analysis of equilibrium systems. It had been applied in a canonical ensemble to describe vapor-liquid equilibrium of argon over a wide range of temperatures, gas adsorption on a graphite open surface and in graphitic slit pores. However, in spite of the conformity of canonical and grand canonical ensembles, the latter is more relevant in the correct description of open systems; for example, the hysteresis loop observed in adsorption of gases in pores under sub-critical conditions can only be described with a grand canonical ensemble. Therefore, the present paper is aimed at an extension of the kMC to open systems. The developed GC-kMC was proved to be consistent with the results obtained with the canonical kMC (C-kMC) for argon adsorption on a graphite surface at 77 K and in graphitic slit pores at 87.3 K. We showed that in slit micropores the hexagonal packing in the layers adjacent to the pore walls is observed at high loadings even at temperatures above the triple point of the bulk phase. The potential and applicability of the GC-kMC are further shown with the correct description of the heat of adsorption and the pressure tensor of the adsorbed phase.

摘要

我们首次在文献中提出了一种新的巨正则系综动力学蒙特卡罗方法(GC-kMC)方案。最近已经表明,动力学蒙特卡罗(kMC)方法是分析平衡系统的非常有效的工具。它已被应用于正则系综来描述氩在很宽的温度范围内的汽液平衡、石墨开放表面上的气体吸附和石墨狭缝孔中的气体吸附。然而,尽管正则系综和巨正则系综是一致的,但后者在正确描述开放系统方面更为相关;例如,在亚临界条件下气体在孔中的吸附中观察到的滞后回线只能用巨正则系综来描述。因此,本文旨在将 kMC 扩展到开放系统。所开发的 GC-kMC 被证明与在 77 K 下石墨表面上的氩吸附和在 87.3 K 下的石墨狭缝孔中的 kMC(C-kMC)的结果一致。我们表明,在狭缝微孔中,甚至在高于体相三相点的温度下,在靠近孔壁的层中也观察到六方堆积。通过正确描述吸附热和吸附相的压力张量,进一步展示了 GC-kMC 的适用性。

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