R—ReO3的构型和电子结构的密度泛函研究

在X3LYP /6-311+G(2d,p)的水平下系统地研究了一系列高价有机铼氧化物(R—ReO3·Ln)的几何构型和电子结构. 研究结果表明, 用X3LYP方法预测的几何结构与实验值符合得很好, 键长的误差一般小于0.001 nm, 而键角的误差小于1°. 同时发现不同配位类型的R基和L配体显著影响铼氧化合物的酸性以及Re—O键能. 应用NBO分析和前线轨道理论可以合理地阐明配体调变的实质.     

FeO+(6∑+)催化CO还原N2O的理论研究

在B3LYP/6-311+G(2d)//B3LYP/6-31C(d)计算水平下,考察了FeO+(6∑+)分子如何催化CO还原N2O微观机理.计算结果表明,FeO+(6∑+是一种有效的催化剂,其可从N2O中夺取一个O原子,然后再传递给CO,完成整个氧转移过程.结果发现,反应中可能生成各种过氧[Fe(O2)+]或双端氧(OFeO+)物种,其中前者比较稳定,后者更活泼.     

Mg2(BH4)2(NH2)2脱氢机理的理论研究

对Mg₂(BH₄)₂(NH₂)₂的脱氢机理展开系统的理论研究发现相对于分子内的脱氢过程,分子间的脱氢过程在热力学和动力学方面都是比较有利的. Mg₂(BH₄)₂(NH₂)₂脱氢过程的第一步是BH₄^-中的B-H^δ-和NH2-中     

FeO+(6Σ+)催化CO还原N2O的理论研究

在B3LYP/6-311+G(2d)//B3LYP/6-31G(d)计算水平下, 考察了FeO+(6Σ+)分子如何催化CO还原N2O微观机理. 计算结果表明, FeO+(6Σ+)是一种有效的催化剂, 其可从N2O中夺取一个O原子, 然后再传递给CO, 完成整个氧转移过程. 结果发现, 反应中可能生成各种过氧[Fe(O2)+]或双端氧(OFeO+)物种, 其中前者比较稳定, 后者更活泼.     

二氧化碳在电解质溶液中的盐溶盐析机制

The solvation of carbon dioxide in sea water plays an important role in the carbon circle and the world climate. The salting-out/salting-in mechanism of CO₂ in electrolyte solutions still remains elusive at molecule level. The ability of ion salting-out/salting-in CO₂ in electrolyte solution follows Hofmeister Series and the change of water mobility induced by salts can be predicted by the viscosity B-coefficients. In this work, the chemical potential of carbon dioxide and the dynamic properties of water in aqueous NaCl, KF and NaClO₄ solutions are calculated and analyzed. According to the viscosity B-coefficients, NaClO₄ (0.012) should salt out the carbon dioxide relative to in pure water, but the opposite effect is observed for it. Our simulation results suggest that the salting-in effect of NaClO₄ is due to the strongly direct anion-CO₂ interaction. The inconsistency between Hofmeister Series and the viscosity B-coefficient suggests that it is not always right to indicate whether a salt belongs to salting-in or salting-out just from these properties of the salt solution in the absence of solute.