A multifacet mechanism for the OH+HNO3 reaction: An ab initio molecular orbital/statistical theory study

Authors
Citation
Ws. Xia et Mc. Lin, A multifacet mechanism for the OH+HNO3 reaction: An ab initio molecular orbital/statistical theory study, J CHEM PHYS, 114(10), 2001, pp. 4522-4532
Citations number
56
Categorie Soggetti
Physical Chemistry/Chemical Physics
Journal title
JOURNAL OF CHEMICAL PHYSICS
ISSN journal
00219606 → ACNP
Volume
114
Issue
10
Year of publication
2001
Pages
4522 - 4532
Database
ISI
SICI code
0021-9606(20010308)114:10<4522:AMMFTO>2.0.ZU;2-D
Abstract
The mechanism for the OH + HNO3 reaction has been studied by ab initio mole cular orbital calculations at the G2M(cc3) level of theory. Four complexes and four transition states have been found and confirmed by intrinsic react ion coordinate analyses. The commonly assumed six-membered ring complex for med by hydrogen bonding of the OH radical with HNO3, -ON(O)OH...OH-, was fo und to be stable by 8.1 kcal/mol; its decomposition producing NO3 + H2O was predicted to have a barrier of 11.6 kcal/mol. A five-membered ring complex , -ON(O)OH...O(H)-, with the H atom of the OH radical placed out of the rin g plane, was found to have a stability of 5.3 kcal/mol; it fragments to for m NO3 + H2O with a barrier of 6.6 kcal/mol. Two additional complexes, which are the mirror image of each other with a 7.4 kcal/mol binding energy, wer e found to be related to the OH exchange reaction with a 13.3 kcal/mol barr ier above the complexes. The direct abstraction process producing H2O2 and NO2 was predicted to have a large barrier of 24.4 kcal/mol, insignificant t o atmospheric chemistry. The rate constant has been calculated at 200-1500 K and 0-760 Torr. The results show that the reaction has strong pressure an d tunneling effects below room temperature. In addition, the rate constants for the decay of OH and OD (in OD + DNO3) evaluated by kinetic modeling co mpare reasonably well with experimental data below room temperature. The un usually pronounced kinetic isotope effect observed experimentally, k(H)/k(D ) greater than or equal to 10, could be accounted for by the combination of the greater tunneling rate in the H system and the large redissociation ra te of stabilized complexes in the D system. The rate constant predicted for the production of H2O and NO3 in the temperature range 750-1500 K can be e ffectively represented by the expression k = 1.45 x 10(-23) T-3.5 exp(+839/ T) cm(3)/s. (C) 2001 American Institute of Physics.