Lakatos G, Patey G N
Department of Physics, University of British Columbia, Vancouver, BC V6T 1Z1, Canada.
J Chem Phys. 2007 Jan 14;126(2):024703. doi: 10.1063/1.2400857.
Grand canonical Monte Carlo simulations are used to examine the adsorption of water into cylindrical nanopores containing single ions. The isotherms for water adsorbing into nanopores with radii of 0.44, 0.54, 0.64, and 0.74 nm and containing Na+, K+, Ca2+, Cl-, or F- at 298 K are computed. In all cases the nanopores are found to fill at reservoir chemical potentials below the chemical potential of saturated water vapor at 298 K. The threshold chemical potential is found to be sensitive to both the size of the channel and the ion species, with the anion-bearing pores filling at lower chemical potentials. Additionally, the filling threshold chemical potential is found to decrease as the radius of the pores is decreased. Pores with K+ and Cl- are compared, and the Cl- pores are found to exhibit higher water densities in the filled states and a more energetically favorable water structure while yielding lower per particle entropies. Sample simulation configurations are also examined and indicate that at low chemical potentials, the adsorbed water forms a cluster around the ion. Finally, the influence of the choice of water model on the adsorption isotherms is examined.
巨正则蒙特卡罗模拟用于研究水在含有单离子的圆柱形纳米孔中的吸附情况。计算了298K时水吸附到半径为0.44、0.54、0.64和0.74nm且含有Na +、K +、Ca2 +、Cl - 或F - 的纳米孔中的等温线。在所有情况下,发现纳米孔在低于298K饱和水蒸气化学势的储层化学势下填充。发现阈值化学势对通道尺寸和离子种类均敏感,含阴离子的孔在较低化学势下填充。此外,发现填充阈值化学势随着孔半径的减小而降低。比较了含有K + 和Cl - 的孔,发现含Cl - 的孔在填充状态下表现出更高的水密度和能量上更有利的水结构,同时产生更低的单粒子熵。还检查了样本模拟构型,结果表明在低化学势下,吸附的水在离子周围形成簇。最后,研究了水模型的选择对吸附等温线的影响。