Abstract

We have developed a new system for measuring photochemical ozone production rates in the atmosphere. Specifically, the system measures the net photochemical oxidant (Ox: the sum of ozone (O3) and nitrogen dioxide (NO2)) production rates (P-L(Ox)). Measuring Ox avoids issues from perturbations to the photostationary states between nitrogen oxides (NOx) and O3. This system has "reaction" and "reference" chambers. Ambient air is introduced into both chambers, and Ox is photochemically produced in the reaction chamber and not generated in the reference chamber. Air from the chambers is alternately introduced into an NO-reaction (NO: nitric oxide) tube to convert O3 to NO2, and then the Ox concentration is measured as NO2 using a laser-induced fluorescence technique. P-L(Ox) was obtained by dividing the difference in Ox concentrations between air samples from the two chambers by the mean residence time of the air in the reaction chamber. In this study, the P-L(Ox) measurement system was characterized, and the current detection limit of P-L(Ox) was determined to be 0.54 ppbv h-1 with an integration time of 60 s (S/N = 2), assuming an ambient Ox concentration of 100 ppbv. Field measurements of P-L(Ox) were conducted using the system at a remote forest location.

Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.