A31F-06
Quantification of Alkyl Nitrates in Ambient Air by Thermal Dissociation Cavity Ring-Down Spectroscopy with Preconcentration

Wednesday, 16 December 2015: 09:15
3004 (Moscone West)
Hans Dieter Osthoff, Connie Ziying Ye, Youssef M Taha, Jason K Pak and Matthew T Saowapon, University of Calgary, Chemistry, Calgary, AB, Canada
Abstract:
Alkyl nitrates (AN, molecular formula RONO2) play a crucial role in the troposphere as temporary reservoirs of nitrogen oxides (NOx =NO +NO2) and by acting as chain terminators in the photochemical production of ozone. Mixing ratios of AN in ambient air are commonly quantified by gas chromatography with electron capture or mass spectrometric detection (GC-ECD or GC-MS) coupled to purge-and-trap preconcentration, usually on Tenax sorbent, to improve the detection limits. The analysis, however, is quite laborious as there are many alkyl nitrates that are low in individual abundance (often less than 1 parts-per-trillion by volume, pptv) and that exhibit different instrumental response factors. An alternative method is to determine alkyl nitrates as a sum (ΣAN) by thermal dissociation (TD) to a common fragment (NO2), which can then be quantified with a uniform response factor by optical absorption, for example by cavity ring-down spectroscopy (CRDS). However, the determination of ΣAN by TD-CRDS is hampered by its relatively high detection limits (several 100 pptv) and secondary chemistry following TD that results in both negative and positive interferences and depends on the composition of the ambient air sampled.

In this work, a TD-CRDS equipped with a Tenax preconcentration unit is described. Matrix effects are minimized by desorbing the samples from the Tenax in a background of nitrogen. The performance of the instrument, in particular the recovery from the Tenax sorbent, was evaluated by sampling laboratory-generated mixtures of alkyl and peroxyacyl nitrates. Field data from a coastal site collected during the Ozone-depleting reactions in a coastal atmosphere (ORCA) campaign, which took place at the Amphitrite Point Observatory in Ucluelet, BC, from July 6 - 31, 2015, are presented. Advantages and disadvantages of the new method are discussed.