Equilibrium isotope effects on the hydration of gas-phase ions. The effect of hydrogen bond formation on deuterium isotopic fractionation factors for H3O+, H5O2+, F(H2O)-, and Cl(H2O)-
作者:J. W. Larson、T. B. McMahon
DOI:10.1021/ja00212a015
日期:1988.2
Etude des reactions d'echange isotopique pour le transfert des ions du titre. Dans chaque cas les ions sont coordines plutot a H 2 O qu'a D 2 O. Role important du mode d'inversion de H 3 O + sur l'effet isotopique
Etude des reactors d'echange isotopique pour le transfert des ions du titre。Dans chaque cas les ions sont coordines plutot a H 2 O qu'a D 2 O. 重要角色 du mode d'inversion de H 3 O + sur l'effet isotopique
Studies of the binary reactions of H<sub>3</sub>O<sup>+</sup>⋅(H<sub>2</sub>O)<sub>0,1,2</sub> ions and their deuterated analogues with D<sub>2</sub>O, H<sub>2</sub>O, and NH<sub>3</sub>
作者:D. Smith、N. G. Adams、M. J. Henchman
DOI:10.1063/1.439781
日期:1980.5
The rate coefficients and product ion distributions for the binary reactions of H3O+⋅(H2O)0,1,2 and D3O+⋅(D2O)0,1,2 ions with D2O and H2O, respectively, and with NH3 have been studied at 300 K using a selected ion flow tube (SIFT) apparatus. The ions were created in a flowing afterglow ion source and after mass filtering were injected at low energy into the SIFT. All the reactions proceeded at or near the gas kinetic limit. In the D2O and H2O thermoneutral isotopic exchange reactions, the distribution of H and D amongst the product ions and neutrals was seen to be purely statistical. This implies that these reactions proceed via the formation of an intermediate long-lived association ion in which total randomization of the H and D atoms takes place prior to unimolecular decomposition. No appreciable isotopic exchange occurred in the exothermic NH3 reactions which apparently proceeded via the simpler mechanisms of D+ (or H+) or D3O+ (or H3O+) transfer. The differing mechanisms for the H2O and D2O reactions compared to the NH3 reactions are rationalized in terms of the thermicities of the reactions and the lifetimes of the respective intermediate ions.
Proton Affinity of Water
作者:Shuang‐Ling Chong、Ransom A. Myers、J. L. Franklin
DOI:10.1063/1.1677551
日期:1972.3
By employing elevated pressures in the ion source of a quadrupole mass filter, it is shown that D3S+ does not transfer a deuteron to D2O and that D3O+ transfers a deuteron to D2S. Studies were carried out in most instances under conditions where the reactant ion undergoes 30–60 collisions before reacting. Thus, most excess energy should have been removed. The transfer of deuteron from D3O+ to D2S appears to go to equilibrium with an equilibrium constant of 14.4 which corresponds to a heat of reaction of 1.8 kcal/mole. From this we deduce the proton affinity of water to be 168 kcal/mole.