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Rate constants for reactions between atmospheric reservoir species. 1. HCL

Journal Article · · Journal of Physical Chemistry; (USA)
DOI:https://doi.org/10.1021/j100352a026· OSTI ID:6985889
; ;  [1]
  1. California Institute of Technology, Pasadena (USA)
The kinetics of the reactions of HCl with ClONO{sub 2}, N{sub 2}O{sub 5}, O{sub 3}, and HO{sub 2}NO{sub 2} have been investigated by using a large-volume static reactor and a Fourier transform spectrometer (FTIR) at 296 K. The upper limits for the homogeneous gas-phase reaction rates of the ClONO{sub 2} + HCl, N{sub 2}O{sub 5} + HCl, O{sub 3} + HCl, and HO{sub 2}NO{sub 2} + HCl reactions were found to be 8.4 {times} 10{sup {minus}21}, 8.4 {times} 10{sup {minus}21}, 4.7 {times} 10{sup {minus}24}, and 9.0 {times} 10{sup {minus}22} (all in unit of cm{sup 3} s{sup {minus}1}), respectively. The heterogeneous nature of the ClONO{sub 2} + CHl and N{sub 2}O{sub 5} + HCl reactions are characterized in terms of the Langmuir-Rideal mechanism. The yields of HNO{sub 3} were observed to be 0.94 {plus minus} 0.14 and 1.10 {plus minus} 0.12 for the ClONO{sub 2} + HCl and N{sub 2}O{sub 5} + HCl reactions, respectively, and the yield of ClNO{sub 2} was found to be 0.84 {plus minus} 0.10 for the N{sub 2}O{sub 5} + HCl reaction. The quoted errors represent one standard deviation of the measurement. In addition, an upper limit of 1.6 {times} 10{sup {minus}19} cm{sup 3} s{sup {minus}1} at 296 K for the reaction of NO{sub 3} with HCl was also obtained in this study. These results may be important in the elucidation of the role played by heterogeneous reactions in the development of the springtime Antarctic ozone depletion over the past decade.
OSTI ID:
6985889
Journal Information:
Journal of Physical Chemistry; (USA), Journal Name: Journal of Physical Chemistry; (USA) Vol. 93:15; ISSN 0022-3654; ISSN JPCHA
Country of Publication:
United States
Language:
English