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Simulation study of argon adsorption on (001) faces of phyllosilicates

机译:氩在页硅酸盐(001)面上的吸附模拟研究

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Grand Canonical Monte Carlo molecular simulations have been performed for argon and nitrogen adsorption on the basal surfaces of phyllosilicates without surface cations. The results have been compared with derivative isotherms analysis of experimental data. An optimization of the surface-Ar interaction has been performed by varying the oxygen atom LJ ε/k_B parameter and the optimized value was used to perform the nitrogen adsorption simulations. The analysis of the argon adsorption simulation indicates that adsorption mechanisms are more complex than may be suggested by experimental results obtained by low-pressure adsorption. The structure of the adsorbed film has a marked dynamic behaviour and the monolayer capacity strongly depends on the equilibrium relative pressure. For nitrogen adsorption, while high pressure behaviour is simulated adequately, some deviation is observed in low-pressure region of the isotherms suggesting that additional simulation and perhaps the use of a more sophisticated potential to model the nitrogen molecule can be necessary to understand fully the behavior of this gas on clay minerals.
机译:已对不带表面阳离子的层状硅酸盐基底表面上的氩气和氮气吸附进行了Grand Canonical Monte Carlo分子模拟。将结果与实验数据的导数等温线分析进行了比较。通过改变氧原子的LJε/ k_B参数对表面-Ar相互作用进行了优化,并使用优化值进行了氮吸附模拟。对氩气吸附模拟的分析表明,吸附机理比低压吸附实验结果所表明的更为复杂。吸附膜的结构具有显着的动力学行为,单层容量在很大程度上取决于平衡相对压力。对于氮吸附,虽然可以充分模拟高压行为,但在等温线的低压区域观察到一些偏差,这表明可能需要额外的模拟,或者可能需要使用更复杂的潜力来模拟氮分子,以充分理解行为这种气体在粘土矿物上。

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