Wongkoblap Atichat, Do Duong D, Nicholson David
Department of Chemical Engineering, University of Queensland, St. Lucia, Brisbane, Queensland, 4072, Australia.
Phys Chem Chem Phys. 2008 Feb 28;10(8):1106-13. doi: 10.1039/b714478d. Epub 2007 Dec 13.
Heats of adsorption and adsorption isotherms of argon, nitrogen and methane on a perfect graphitic surface and a defective graphitic surface are studied with a Grand Canonical Monte Carlo Simulation (GCMC). For the perfect surface, the isosteric heat versus loading shows a typical pattern of adsorption of simple fluids on graphite. Depending on adsorbate, degree of graphitization and temperature, a spike in the heat curve versus loading is observed when the first layer is mostly covered with adsorbate molecules. The heat spike is observed for argon and nitrogen at 77 K while for argon at 87.3 K it is no longer present. These simulation results are consistent with the experimental data of J. Rouquerol, S. Partyka and F. Rouquerol, J. Chem. Soc., Faraday Trans. 1, 1977, 73, 306. In the case of methane we observe heat spikes at low temperatures, 84.5, 92.5 and 104 K. The heat spike shifts to higher loading with temperature and it then disappears at high temperatures. These observations are in qualitative agreement with the experimental data of A. Inaba, Y. Koga and J. A. Morrison, J. Chem. Soc., Faraday Trans. 2, 1986, 82, 1635. In all cases where heat spikes are observed, the GCMC simulation results indicate that the heat spike is associated with the squeezing of molecules into the already dense first layer, and the rearrangement of molecules to form a highly structured fluid of this layer. While this squeezing into the first layer is happening, molecules continue to adsorb onto the relatively sparse second layer.
采用巨正则蒙特卡罗模拟(GCMC)研究了氩气、氮气和甲烷在完美石墨表面和缺陷石墨表面上的吸附热及吸附等温线。对于完美表面,等量吸附热与负载量的关系呈现出简单流体在石墨上吸附的典型模式。根据吸附质、石墨化程度和温度的不同,当第一层大部分被吸附质分子覆盖时,会观察到热曲线与负载量关系中的一个峰值。在77 K时,氩气和氮气出现热峰,而对于87.3 K的氩气,热峰不再出现。这些模拟结果与J. Rouquerol、S. Partyka和F. Rouquerol在《化学学会志,法拉第会刊1》,1977年,第73卷,第306页中的实验数据一致。对于甲烷,我们在84.5 K、92.5 K和104 K的低温下观察到热峰。热峰随温度向更高负载量移动,然后在高温下消失。这些观察结果与A. Inaba、Y. Koga和J. A. Morrison在《化学学会志,法拉第会刊2》,1986年,第82卷,第1635页中的实验数据定性一致。在所有观察到热峰的情况下,GCMC模拟结果表明,热峰与分子挤入已经致密的第一层以及分子重排以形成该层高度结构化流体有关。当发生挤入第一层的情况时,分子继续吸附到相对稀疏的第二层上。