Mass spectrometric measurement of hydrogen isotope fractionation for the reactions of chloromethane with OH and Cl
Chloromethane (CHinline-formula3Cl) is an important provider of chlorine to the stratosphere but detailed knowledge of its budget is missing. Stable isotope analysis is a potentially powerful tool to constrain CHinline-formula3Cl flux estimates. The largest degree of isotope fractionation is expected to occur for deuterium in CHinline-formula3Cl in the hydrogen abstraction reactions with its main sink reactant tropospheric OH and its minor sink reactant Cl atoms. We determined the isotope fractionation by stable hydrogen isotope analysis of the fraction of CHinline-formula3Cl remaining after reaction with hydroxyl and chlorine radicals in a 3.5 minline-formula3 Teflon smog chamber at 293 inline-formula± 1 K. We measured the stable hydrogen isotope values of the unreacted CHinline-formula3Cl using compound-specific thermal conversion isotope ratio mass spectrometry. The isotope fractionations of CHinline-formula3Cl for the reactions with hydroxyl and chlorine radicals were found to be inline-formula
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