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High concentrations of N2O5 and NO3 observed in daytime with a TD-CIMS: chemical interference or a real atmospheric phenomenon?

Authors :
Wang, X.
Wang, T.
Yan, C.
Tham, Y. J.
Xue, L.
Xu, Z.
Zha, Q.
Source :
Atmospheric Measurement Techniques Discussions; 2013, Vol. 6 Issue 4, p7473-7504, 32p
Publication Year :
2013

Abstract

Dinitrogen pentoxide (N<subscript>2</subscript>O<subscript>5</subscript>) and the nitrate radical (NO<subscript>3</subscript>) play important roles in atmospheric chemistry, yet accurate measurements of their concentrations remain challenging. A thermal dissociation chemical ionization mass spectrometer (TD-CIMS) was deployed to an urban site in Hong Kong to measure the sum of N<subscript>2</subscript>O<subscript>5</subscript> and NO<subscript>3</subscript> in autumn 2010. To our surprise, very high concentrations of N<subscript>2</subscript>O<subscript>5</subscript> +NO<subscript>3</subscript> were frequently observed in daytime, with mixing ratios in the range of 200–1000 pptv. To investigate this unusual phenomenon, various interference tests and measurements with different instrument configuration were conducted. It was found that peroxy acetyl nitrate (PAN) contributed to measurable signals at 62 amu, and more importantly, this interference increased significantly with co-existence of NO<subscript>2</subscript>. Nitric acid (HNO<subscript>3</subscript>), on the other hand, had little interference to the detection of N<subscript>2</subscript>O<subscript>5</subscript>/NO<subscript>3</subscript> via the NO<subscript>3</subscript><superscript>−</superscript> ion in our TD-CIMS. According to the test results, the interference from PAN and NO<subscript>2</subscript> could have contributed to 30–50% of the average daytime (12:00–16:00 LT) N<subscript>2</subscript>O<subscript>5</subscript> +NO<subscript>3</subscript> signal at our site. However, evidence exists for the presence of elevated daytime N<subscript>2</subscript>O<subscript>5</subscript>, in addition to the daytime signal at 62amu. This includes: (1) daytime N<subscript>2</subscript>O<subscript>5</subscript> measured via the I(N<subscript>2</subscript>O<subscript>5</subscript>)<superscript>−</superscript> cluster ion with an unheated inlet, which subjects to minimum interferences, and (2) observation of elevated daytime ClNO<subscript>2</subscript> (a product of N<subscript>2</subscript>O<subscript>5</subscript> hydrolysis) during a follow-up study. In view of the difficulty in accurately quantifying the contribution from the interferences of PAN and NO<subscript>2</subscript> and un-tested potential interfering chemicals in the real atmosphere, we caution the use of 62amu in the TD-CIMS for measuring ambient N<subscript>2</subscript>O<subscript>5</subscript> in a high NO<subscript>x</subscript> environment like Hong Kong. Additional studies are needed to re-examine the daytime issue using other measurement techniques. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
18678610
Volume :
6
Issue :
4
Database :
Complementary Index
Journal :
Atmospheric Measurement Techniques Discussions
Publication Type :
Academic Journal
Accession number :
91631158
Full Text :
https://doi.org/10.5194/amtd-6-7473-2013