Observations of total RONOsub2/sub over the boreal forest: NOsubx/sub sinks and HNOsub3/sub sources

摘要

pstrongAbstract./strong In contrast with the textbook view of remote chemistry where HNOsub3/sub formation is the primary sink of nitrogen oxides, recent theoretical analyses show that formation of RONOsub2/sub (ΣANs) from isoprene and other terpene precursors is the primary net chemical loss of nitrogen oxides over the remote continents where the concentration of nitrogen oxides is low. This then increases the prominence of questions concerning the chemical lifetime and ultimate fate of ΣANs. We present observations of nitrogen oxides and organic molecules collected over the Canadian boreal forest during the summer which show that ΣANs account for ~20% of total oxidized nitrogen and that their instantaneous production rate is larger than that of HNOsub3/sub. This confirms the primary role of reactions producing ΣANs as a control over the lifetime of NOsubx/sub (NOsubx/sub = NO + NOsub2/sub) in remote, continental environments. However, HNOsub3/sub is generally present in larger concentrations than ΣANs indicating that the atmospheric lifetime of ΣANs is shorter than the HNOsub3/sub lifetime. We investigate a range of proposed loss mechanisms that would explain the inferred lifetime of ΣANs finding that in combination with deposition, two processes are consistent with the observations (1) rapid ozonolysis of isoprene nitrates where at least ~40% of the ozonolysis products release NOsubx/sub from the carbon backbone and/or (2) hydrolysis of particulate organic nitrates with HNOsub3/sub as a product. Implications of these ideas for our understanding of NOsubx/sub and NOsuby/sub budget in remote and rural locations are discussed./p.