Water was reacted with gas-phase oxyanions having the general composition S
ixOyHz- that were formed and isolated in an ion trap-secondary ion mass spe
ctrometer (IT-SIMS). The radical SiO2.- reacted slowly with H2O to abstract
HO., forming SiO3H-, at a rate of 8 x 10(-13) cm(3) molecule(-1) s(-1), co
rresponding to an efficiency of about 0.03% compared with the theoretical c
ollision rate constant (average dipole orientation). The product ion SiO3H-
underwent a consecutive condensation reaction with H2O to form SiO4H3- at
a rate that was approximately 0.4-0.7% efficient. SiO4H3- did not undergo f
urther reaction with water. The multiple reaction pathways by which radical
SiO3.- reacted with H2O were kinetically modeled using a stochastic approa
ch. SiO3.- reacted with water by three parallel reaction pathways: (1) abst
raction of a radical H-. to form SiO3H-, which then reacted with a second H
2O to form SiO4H3-; (2) abstraction of a radical OH. to form SiO4H-, which
further reacted by consecutive H-. abstractions to form SiO4H2.- and then S
iO4H3-; and (3) condensation with H2O to form SiO4H2.-, which subsequently
abstracted a radical H-. from a second H2O to form SiO4H3-. In all of these
reactions, the rate constants were determined to be very slow, as determin
ed by both direct measurement and stochastic modeling. For comparison, the
even electron ion Si2O5H- was also investigated: it underwent condensation
with H2O to form Si2O6H3-, with a rate constant corresponding to 50% effici
ency. The reactions were also modeled using ab initio calculations at the U
B3LYP/6-311 + G(2d,p) level. Addition of H2O to SiO3.-, SiO3H-, and Si2O5H-
was calculated to be approximately 42, 45, and 55 kcal mol(-1) exothermic,
respectively, and encountered low activation barriers. Modeling Of SiO2.-
and SiO3.- reactions with H2O failed to produce radical abstraction reactio
n pathways observed in the IT-SIMS, possibly indicating that alternative re
action mechanisms are operative.