The atmospheric chemistry of isoprene- and other multifunctional-nitrates

Formation of alkyl and multifunctional nitrates significantly reduces ozone production rates in their source regions, their transport and subsequent chemistry can impact secondary organic aerosol formation and NOy removal rates and they may lead to the re-release of NOx in regions far-removed from the original source. In this dissertation, the atmospheric chemistry of alkyl and multifunctional nitrates is investigated through a combination of laboratory and field measurements. In contrast to many previous studies that have focused on observations of specific individual nitrate compounds, the work described here uses a technique (Thermal Dissociation-Laser Induced Fluorescence or TD-LIF) that allows for measurements of the sum of all alkyl and multifunctional nitrates. These observations show that alkyl and multifunctional nitrates are a significant fraction of NOy in a number of different chemical regimes representing diverse hydrocarbon mixtures. In what follows, I show that their formation impacts both ozone 1 formation and NOy transport in ways that are not accounted for by currently accepted chemical mechanisms. Aircraft measurements are used to constrain nitrate yields following isoprene oxidation by OH, the atmospheric lifetimes of these nitrates, and the retention rate of the nitrate functional group upon oxidation of the initial isoprene nitrates. It is found that nitrate functionality is maintained upon further oxidation at least 75% of the time indicating that the lifetime of isoprene nitrates as a pool of compounds is considerably longer than the lifetime of the individual isoprene nitrates with respect to reaction with OH. We examine the products of NO3-initiated oxidation of isoprene in a smog-chamber, propose a detailed reaction scheme, and find that nitrates are produced with a yield of 65+/-12%, the majority of which are carbonyl nitrates. We investigate the role of alkyl and multifunctional nitrates in the Mexico City plume where they are observed to be more abundant than expected given currently accepted chemical mechanisms. We investigate several possible explanations for the unexpectedly high abundances and calculate that their formation depresses ozone production in the near-field of Mexico City by as much as 30%.