The acid ionization by which HBr transfers a proton to a water molecule is
studied for HBr in small water clusters as a first stage in a study of the
corresponding Arctic atmospheric process. Electronic structure calculations
, involving relatively large basis sets and including electron correlation
effects, indicate that HBr is acid-ionized in a cluster of four water molec
ules. The most stable structure in the general HBr(H2O)(4) system is a diam
ond-like (trigonal bipyramidal) structure in which the bromide and hydroniu
m ion species are bridged by three water molecules, and infrared spectral a
nd ionization potential characteristics potentially useful for experimental
study are provided. This structure is calculated to remain the thermodynam
ically most stable one up to about 180 K, where HBr + (H2O)(4) becomes more
stable. Aspects of the formation of the acid-ionized cluster from both HBr
+ (H2O)(4) and H2O + HBr(H2O)(3) are discussed. Possible implications for
HBr acid ionization at the surface of ice, believed to be important for Arc
tic atmosphere ozone depletion mechanisms, are briefly discussed.