HCl Yield from OH + ClO: Stratospheric Model Sensitivities and Elementary Rate Theory Calculations
| Autor: | Mark P. McGrath, Manvendra K. Dubey, Gregory P. Smith, F. Sherwood Rowland |
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| Rok vydání: | 1998 |
| Předmět: | |
| Zdroj: | The Journal of Physical Chemistry A. 102:3127-3133 |
| ISSN: | 1520-5215 1089-5639 |
| Popis: | Compared to measurements, atmospheric models have overestimated [ClO]/[HCl] and [ClONO2]/[HCl] in the upper and middle stratosphere, respectively, and consequently have predicted lower [O3] than observed. It is believed that a minor branch that produces HCl from the OH + ClO reaction can account for these discrepancies. Recent laboratory studies have indicated a 5 ( 2% yield for this channel. 1 By performing box model sensitivity analysis calculations using the output from the LLNL-2D diurnally averaged stratospheric model, we quantitatively confirm that this reaction is the most prominent contributor to the model [ClO]/ [HCl] and [ClONO2]/[HCl] uncertainties in the upper stratosphere and that it is most effective in increasing [O3] at higher latitudes during winter. Using theoretical methods, we examine the OH + ClO reaction mechanism, in which an initially energized HOOCl* complex is formed that can dissociate to HO2 + Cl (major) or HCl + O2( 1 ¢) (minor) products, redissociate to reactants, or be collisionally stabilized. Multichannel RRKM calculations guided by ab initio electronic structure calculations and the available kinetic data are presented. We show that the four-center transition state (TS3) for HCl production must lie at least 2 kcal/ mol below the reactants for the HCl yield to exceed 5%. Our ab initio relative energy of -2.3 ( 3 kcal/mol for TS3 demonstrates that this minor HCl channel is mechanistically feasible. We also predict small pressure, temperature, and H/D isotopic dependencies for the minor channel yield and insignificant rates of complex stabilization under atmospheric conditions. |
| Databáze: | OpenAIRE |
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