文摘
Production of O(3PJ, J = 2, 1, 0) atoms from the 295-320 nm photodissociation of NO3- adsorbed on waterpolycrystalline ice films at 100 K was directly confirmed using the resonance-enhanced multiphoton ionizationtechnique. Detection of the O atom signals required an induction period after deposition of HNO3 onto theice film held at 130 K due to the slow ionization rate of HNO3 to H+ and NO3- with a rate constant of k =(5.3 ± 0.2) × 10-3 s-1. Translational energy distributions of the O atoms were represented by a combinationof two Maxwell-Boltzmann energy distributions with translational temperatures of 2000 and 100 K. Directdetection of NO from the secondary photodissociation process was also successful. On the atmosphericimplications, the influence of the direct release of the oxygen atoms into the air from NO3- adsorbed on thenatural snowpack was included in an atmospheric model calculation on the mixing ratios of ozone and nitricoxide at the South Pole, and the results compared favorably with the field data.