Highly time resolved measurements of nitrate in ambient aerosols were conducted by an Aerodyne Quadrupole Aerosol Mass Spectrometer (Q‐AMS or simply AMS) and a particle‐into‐liquid sampler (PILS) coupled to ion chromatography from field intensives at two sites: an urban site in New York City (Queens College; QC) for wintertime (22 January to 5 February 2004) and a rural site in southwestern New York state (Pinnacle State Park; PSP) for summertime (18 July to 6 August 2004). In this study, we report that in rural atmospheres the inorganic nitrate signal from Q‐AMS may contain significant interferences from organic signals. Analysis of the QC data indicates a good agreement between the PILS‐nitrate and AMS‐nitrate measurements ( R 2 = 0.94; linear regression slope = 1.05). In addition, the m / z 30 and m / z 46 (two dominant ion fragments in nitrate mass spectrum) signals tightly correlate at QC ( R 2 = 0.98) and have an average ratio similar to that determined in the laboratory for NH 4 NO 3 ( m / z 30/ m / z 46 = 2.4). In contrast, at the PSP site the correlation between PILS‐ and AMS‐nitrate was poor ( R 2 = 0.34), the AMS reported nitrate values were substantially higher, and the m / z 30 to m / z 46 ratios were generally much larger than 2.4. These observations, together with evaluations by aerosol phase ion balance, indicate that the AMS m / z 30 signals at PSP have been strongly influenced by organic compounds that also produce signals at m / z 30, e.g., organic nitrates (NO + ), oxygenated organics (CH 2 O + ), hydrocarbon‐like organics (C 2 H 6 + ), and nitrogen‐containing organic compounds (CH 4 N + ).
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Bae et al. (2007) studied this question.
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