Resonance fluorescence method for kinetics of atomic reactions. Reactions of atomic hydrogen with olefins

1967 ◽  
Vol 44 ◽  
pp. 252 ◽  
Author(s):  
W. Braun ◽  
M. Lenzi
1988 ◽  
Vol 30 (12) ◽  
pp. 1637-1640 ◽  
Author(s):  
M M Larionov ◽  
L S Levin ◽  
Yu V Petrov ◽  
G T Razdobarin ◽  
V V Semenov ◽  
...  

2001 ◽  
Vol 1 (1) ◽  
pp. 1-7 ◽  
Author(s):  
S. A. Carl ◽  
J. N. Crowley

Abstract. The kinetics of the title reactions were investigated using the laser photolysis - resonance fluorescence method, employing the sequential two-photon dissociation of NO2 in the presence of H2  as the OH source. The 298 K rate constant for OH + C3H8 was found to be (1.15 ± 0.1) × 10-12 cm3 s-1, in excellent agreement with the literature recommendation, and with a separate determination using HNO3  photolysis at 248 nm as the OH source. The 298 K rate constants for OH + n - C3H7I and  i - C3H7I  were measured for the first time and found to be (1.47 ± 0.08) and (1.22 ± 0.06) × 10-12 cm3 s-1, respectively. The errors include an assessment of systematic error due to concentration measurement, which, for the propyl-iodides was minimised by on-line UV-absorption spectroscopy. These results show that reaction with OH is an important sink for  n - C3H7I and  i - C3H7I, which has implications for the reactive iodine budget of the marine boundary layer.


2001 ◽  
Vol 1 (1) ◽  
pp. 23-41 ◽  
Author(s):  
S. A. Carl ◽  
J. N. Crowley

Abstract. The kinetics of the title reactions were investigated using the laser photolysis - resonance fluorescence method, employing the sequential two-photon dissociation of NO2 in the presence of H2 as the OH source. The 298 K rate constant for OH + C3H8 was found to be (1.15±0.1) × 10-12 cm3 s-1, in excellent agreement with the literature recommendation, and with a separate determination using HNO3 photolysis at 248 nm as the OH source. The 298 K rate constants for OH + n-C3H7I and i-C3H7I were measured for the first time and found to be (1.47±0.08) and (1.22±0.06) × 10-12 cm3 s-1, respectively. The errors include an assessment of systematic error due to concentration measurement, which, for the propyl-iodides was minimised by on-line UV-absorption spectroscopy. The implications of these results for the reactive iodine budget of the marine boundary layer are discussed.


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