Answers are grounded in this paper and cite their sources.
Temperature-dependent near-IR photodissociation spectra were obtained for several vibrational overtone transitions of peroxynitric acid (HNO 4 ) with a tunable OPO photolysis/OH laser-induced-fluorescence system. Band-integrated photodissociation cross-sections ( ∫σ diss ), determined relative to that for the 3ν 1 OH stretching overtone, were measured for three dissociative bands. Assuming unit quantum efficiency for photodissociation of 3ν 1 we find 2ν 1 + ν 3 (8242 cm -1 ) = (1.21 × 10 -20 ) (independent of temperature), 2ν 1 (6900 cm -1 ) = 4.09 × 10 -18 * e (-826.5/ T ) (295 K > T > 224 K), and ν 1 + 2ν 3 (6252 cm -1 ) = 1.87 × 10 -19 * e (-1410.7/ T ) (278 K > T > 240 K) cm 2 molecule -1 cm -1 . The photodissociation cross-sections are independent of pressure over the range 2 to 40 Torr. Temperature-dependent quantum yields (φ) for these transitions were obtained using integrated absorption cross-sections (∫σ abs ) of HNO 4 overtone vibrations measured with a FTIR spectrometer. In the atmosphere, photodissociation in the infrared is dominated by excitation of the first overtone of the OH stretching vibration (2ν 1 ). Inclusion of all dissociative HNO 4 overtone and combination transitions yields a daytime IR photolysis rate of approximately 1 × 10 -5 s -1 . This process significantly shortens the estimated lifetime of HNO 4 in the upper troposphere and lower stratosphere.
No takes yet. Share an insight, caveat, or question.
Roehl et al. (2002) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: