Secondary formation of nitrophenols in an oil and gas production region: insights from observations during the Uintah Basin Winter Ozone Study (UBWOS) 2014

Bin Yuan1,2, John Liggio3, Jeremy J B Wentzell4, Shao-Meng Li4, Harald Stark5, Hans Dieter Osthoff6, Dr. James Roberts, PhD7, Jessica Gilman7, Brian M Lerner8, Rui Li9, Amy Leithead4, Patrick R Veres10, Carsten Warneke9, Robert J Wild11, Steven S Brown12 and Joost A de Gouw13, (1)NOAA Earth System Research Lab, Boulder, CO, United States, (2)Cooperative Institute for Research in Environmental Sciences, Boulder, CO, United States, (3)Air Quality Research Division, Toronto, ON, Canada, (4)Environment and Climate Change Canada, Air Quality Research Division, Toronto, ON, Canada, (5)University of Colorado at Boulder, Cooperative Institute for Research in Environmental Sciences (CIRES) and Department of Chemistry, Boulder, United States, (6)University of Calgary, Chemistry, Calgary, AB, Canada, (7)NOAA Chemical Sciences Laboratory, Boulder, United States, (8)Aerodyne Research, Inc., Billerica, MA, United States, (9)NOAA Boulder, Boulder, CO, United States, (10)NOAA Boulder, Boulder, United States, (11)Colorado University/NOAA/ESRL, Boulder, CO, United States, (12)NOAA, Earth System Research Laboratory, Boulder, CO, United States, (13)University of Colorado Boulder, Department of Chemistry, Boulder, United States
Abstract:
Nitrophenols play important roles in the atmosphere, for example as light-absorbing organic matter, phytotoxins, precursors of secondary organic aerosol (SOA) and HONO. Besides emissions from primary sources, nitrophenols are important secondary products from the oxidation of aromatics in the atmosphere. Nitrophenols were measured along with many other organic acids using an acetate ion (CH3COO-) time of flight chemical ionization mass spectrometer (TOF-CIMS) at a site in an oil and gas producing region during Uintah Basin Winter Ozone Study (UBWOS) in 2014. Nitrophenol and methyl-substituted nitrophenols exhibited distinct diurnal profiles, with high concentrations at night and a minimum observed during the daytime. This is consistent with photolysis being the dominant sink of these species. For this study, nitrophenols are most likely formed in situ, while primary emissions (e.g. biomass burning, oil and gas emissions) are negligible during this campaign. We will quantify the contributions of gas phase reactions of phenols with OH and NO3 radicals to form nitrophenols. The importance of heterogeneous reactions resulting for nitrophenol formation, including N2O5 chemistry on surfaces and photolysis of nitrate in the snow will be also explored using vertical gradient measurements at two different heights (1.0 m and 18.5 m). In contrast with mono-nitrophenols, dinitrophenol showed a daytime maximum, indicating that the formation of dinitrophenol is driven by photochemistry in the atmosphere. The results of this study will be helpful to improving our understanding the budget of nitrophenols and oxidation mechanisms of aromatics in the atmosphere.