Pickard Frank C, Dunn Meghan E, Shields George C
Department of Chemistry, Hamilton College, 198 College Hill Road, Clinton, New York 13323, USA.
J Phys Chem A. 2005 Jun 9;109(22):4905-10. doi: 10.1021/jp0514372.
The G2, G3, CBS-QB3, and CBS-APNO model chemistry methods and the B3LYP, B3P86, mPW1PW, and PBE1PBE density functional theory (DFT) methods have been used to calculate deltaH(o) and deltaG(o) values for ionic clusters of the ammonium ion complexed with water and ammonia. Results for the clusters NH4(+) (NH3)n and NH4(+) (H2O)n, where n = 1-4, are reported in this paper and compared against experimental values. Agreement with the experimental values for deltaH(o) and deltaG(o) for formation of NH4(+) (NH3)n clusters is excellent. Comparison between experiment and theory for formation of the NH4(+) (H2O)n clusters is quite good considering the uncertainty in the experimental values. The four DFT methods yield excellent agreement with experiment and the model chemistry methods when the aug-cc-pVTZ basis set is used for energetic calculations and the 6-31G* basis set is used for geometries and frequencies. On the basis of these results, we predict that all ions in the lower troposphere will be saturated with at least one complete first hydration shell of water molecules.
已使用G2、G3、CBS-QB3和CBS-APNO模型化学方法以及B3LYP、B3P86、mPW1PW和PBE1PBE密度泛函理论(DFT)方法来计算与水和氨络合的铵离子的离子簇的ΔH⁰和ΔG⁰值。本文报告了NH₄⁺(NH₃)ₙ和NH₄⁺(H₂O)ₙ簇(其中n = 1 - 4)的结果,并与实验值进行了比较。对于NH₄⁺(NH₃)ₙ簇形成的ΔH⁰和ΔG⁰的实验值,二者吻合度极佳。考虑到实验值的不确定性,对于NH₄⁺(H₂O)ₙ簇形成的实验与理论比较结果相当不错。当使用aug-cc-pVTZ基组进行能量计算以及使用6-31G*基组进行几何结构和频率计算时,四种DFT方法与实验以及模型化学方法的结果高度吻合。基于这些结果,我们预测对流层下部的所有离子将被至少一个完整的水分子第一水合层所饱和。