will present a seminar titled:
“New insights into the atmospheric chemistry of nitrogen oxide reservoir species”
Abstract:
The oxides of nitrogen (NOx = NO + NO2) are important trace gas constituents of the troposphere. During daytime, NOx catalyzes the photochemical production of ozone (O3), which is of interest to regional air quality and human health. The lifetime of NOx is on the order of days; its main sink is conversion to nitric acid (HNO3), which deposits. NOx can be stored in so-called reservoir species, whose lifetimes are longer than that of NOx and whose decomposition, usually after long-range transport to remote regions, regenerates NOx. Peroxycarboxylic nitric anhydrides (PANs, RC(O)O2NO2) and alkyl nitrates (ANs, RONO2) are important NOx reservoir species formed during daytime. At night, a significant fraction of NOx can be converted to the nocturnal reservoir species dinitrogen pentoxide (N2O5) and nitryl chloride (ClNO2). While the atmospheric chemistry of PANs and N2O5 in ambient air is relatively well established, considerable uncertainty remains about the atmospheric chemistry of ANs and ClNO2, mainly due to a lack of analytical techniques to measure these species in ambient abundance.
In this presentation, two novel analytical methods to quantify the mixing ratios of NOx reservoir species with high sensitivity and accuracy are presented and their advantages and limitations discussed. In the first method, thermal dissociation cavity ring-down spectroscopy (TD-CRDS) is used to quantify the mixing ratios of SPAN, SAN, ClNO2, or N2O5 in laboratory-generated samples with detection limits on the order of tens of parts-per-trillion by volume (pptv). In the second method, chemical ionization mass spectrometry (CIMS), calibrated against TD-CRDS, is used to quantify the mixing ratios of ClNO2, the major PAN species, nitric, and nitrous acid. The new methods were applied in laboratory experiments and field measurements. In the lab, the gaseous nitrogen oxides generated during the photolysis of nitrate anion in ice were characterized. The photochemical generation of NOx from nitrate photolysis was observed to be dependent on acidity. Using CIMS, two new species, peroxynitric (HO2NO2) and peroxynitrous (HO2NO) acid, were observed as photochemical products in the gas phase, which suggests that these molecules may be important but overlooked intermediates. Preliminary results from field measurements of ClNO2 in Calgary, AB, and Pasadena, CA, are presented.
Friday, January 27, 2012 at 3:00 p.m. in ICT 121
Department Contact: Dr. Kevin Thurbide.