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Hamilton JF, Bryant DJ, Edwards PM, Ouyang B, Bannan TJ, Mehra A, Mayhew AW, Hopkins JR, Dunmore RE, Squires FA, Lee JD, Newland MJ, Worrall SD, Bacak A, Coe H, Percival C, Whalley LK, Heard DE, Slater EJ, Jones RL, Cui T, Surratt JD, Reeves CE, Mills GP, Grimmond S, Sun Y, Xu W, Shi Z, Rickard AR. Key Role of NO 3 Radicals in the Production of Isoprene Nitrates and Nitrooxyorganosulfates in Beijing. ENVIRONMENTAL SCIENCE & TECHNOLOGY 2021; 55:842-853. [PMID: 33410677 DOI: 10.1021/acs.est.0c05689] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/12/2023]
Abstract
The formation of isoprene nitrates (IsN) can lead to significant secondary organic aerosol (SOA) production and they can act as reservoirs of atmospheric nitrogen oxides. In this work, we estimate the rate of production of IsN from the reactions of isoprene with OH and NO3 radicals during the summertime in Beijing. While OH dominates the loss of isoprene during the day, NO3 plays an increasingly important role in the production of IsN from the early afternoon onwards. Unusually low NO concentrations during the afternoon resulted in NO3 mixing ratios of ca. 2 pptv at approximately 15:00, which we estimate to account for around a third of the total IsN production in the gas phase. Heterogeneous uptake of IsN produces nitrooxyorganosulfates (NOS). Two mono-nitrated NOS were correlated with particulate sulfate concentrations and appear to be formed from sequential NO3 and OH oxidation. Di- and tri-nitrated isoprene-related NOS, formed from multiple NO3 oxidation steps, peaked during the night. This work highlights that NO3 chemistry can play a key role in driving biogenic-anthropogenic interactive chemistry in Beijing with respect to the formation of IsN during both the day and night.
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Affiliation(s)
- Jacqueline F Hamilton
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - Daniel J Bryant
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - Peter M Edwards
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - Bin Ouyang
- Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, U.K
| | - Thomas J Bannan
- School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, U.K
| | - Archit Mehra
- School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, U.K
| | - Alfred W Mayhew
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - James R Hopkins
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
- National Centre for Atmospheric Science, University of York, York YO10 5DD, U.K
| | - Rachel E Dunmore
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - Freya A Squires
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - James D Lee
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
- National Centre for Atmospheric Science, University of York, York YO10 5DD, U.K
| | - Mike J Newland
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
| | - Stephen D Worrall
- School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, U.K
| | - Asan Bacak
- School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, U.K
| | - Hugh Coe
- School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, U.K
| | - Carl Percival
- School of Earth and Environmental Sciences, University of Manchester, Manchester M13 9PL, U.K
| | - Lisa K Whalley
- School of Chemistry, University of Leeds, Leeds LS2 9JT, U.K
| | - Dwayne E Heard
- School of Chemistry, University of Leeds, Leeds LS2 9JT, U.K
| | - Eloise J Slater
- School of Chemistry, University of Leeds, Leeds LS2 9JT, U.K
| | - Roderic L Jones
- Department of Chemistry, University of Cambridge, Cambridge CB2 1EW, U.K
| | - Tianqu Cui
- Department of Environmental Sciences and Engineering, Gillings School of Global and Public Health, University of North Carolina, Chapel Hill, North Carolina 27599, United States
| | - Jason D Surratt
- Department of Environmental Sciences and Engineering, Gillings School of Global and Public Health, University of North Carolina, Chapel Hill, North Carolina 27599, United States
| | - Claire E Reeves
- Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, U.K
| | - Graham P Mills
- Centre for Ocean and Atmospheric Sciences, School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, U.K
| | - Sue Grimmond
- Department of Meteorology, University of Reading, Reading RG6 6ET, U.K
| | - Yele Sun
- Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, People's Republic of China
| | - Weiqi Xu
- Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, People's Republic of China
| | - Zongbo Shi
- School of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham B15 2TT, U.K
| | - Andrew R Rickard
- Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, York YO10 5DD, U.K
- National Centre for Atmospheric Science, University of York, York YO10 5DD, U.K
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Carslaw N, Fletcher L, Heard D, Ingham T, Walker H. Significant OH production under surface cleaning and air cleaning conditions: Impact on indoor air quality. INDOOR AIR 2017; 27:1091-1100. [PMID: 28493625 DOI: 10.1111/ina.12394] [Citation(s) in RCA: 46] [Impact Index Per Article: 5.8] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 09/08/2016] [Accepted: 05/03/2017] [Indexed: 05/25/2023]
Abstract
We report measurements of hydroxyl (OH) and hydroperoxy (HO2 ) radicals made by laser-induced fluorescence spectroscopy in a computer classroom (i) in the absence of indoor activities (ii) during desk cleaning with a limonene-containing cleaner (iii) during operation of a commercially available "air cleaning" device. In the unmanipulated environment, the one-minute averaged OH concentration remained close to or below the limit of detection (6.5×105 molecule cm-3 ), whilst that of HO2 was 1.3×107 molecule cm-3 . These concentrations increased to ~4×106 and 4×108 molecule cm-3 , respectively during desk cleaning. During operation of the air cleaning device, OH and HO2 concentrations reached ~2×107 and ~6×108 molecule cm-3 respectively. The potential of these OH concentrations to initiate chemical processing is explored using a detailed chemical model for indoor air (the INDCM). The model can reproduce the measured OH and HO2 concentrations to within 50% and often within a few % and demonstrates that the resulting secondary chemistry varies with the cleaning activity. Whilst terpene reaction products dominate the product composition following surface cleaning, those from aromatics and other VOCs are much more important during the use of the air cleaning device.
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Affiliation(s)
- N Carslaw
- Environment Department, University of York, York, UK
| | - L Fletcher
- Institute of Public health and Environmental Engineering (iPHEE), School of Civil Engineering, University of Leeds, Leeds, UK
| | - D Heard
- School of Chemistry, University of Leeds, Leeds, UK
- National Centre for Atmospheric Science, University of Leeds, Leeds, UK
| | - T Ingham
- School of Chemistry, University of Leeds, Leeds, UK
- National Centre for Atmospheric Science, University of Leeds, Leeds, UK
| | - H Walker
- School of Chemistry, University of Leeds, Leeds, UK
- Now at the Institute of Climate and Academic Science, School of Earth and Environment, University of Leeds, Leeds, UK
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Dunmore RE, Whalley LK, Sherwen T, Evans MJ, Heard DE, Hopkins JR, Lee JD, Lewis AC, Lidster RT, Rickard AR, Hamilton JF. Atmospheric ethanol in London and the potential impacts of future fuel formulations. Faraday Discuss 2016; 189:105-20. [DOI: 10.1039/c5fd00190k] [Citation(s) in RCA: 10] [Impact Index Per Article: 1.1] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/21/2022]
Abstract
There is growing global consumption of non-fossil fuels such as ethanol made from renewable biomass. Previous studies have shown that one of the main air quality disadvantages of using ethanol blended fuels is a significant increase in the production of acetaldehyde, an unregulated and toxic pollutant. Most studies on the impacts of ethanol blended gasoline have been carried out in the US and Brazil, with much less focus on the UK and Europe. We report time resolved measurements of ethanol in London during the winter and summer of 2012. In both seasons the mean mixing ratio of ethanol was around 5 ppb, with maximum values over 30 ppb, making ethanol currently the most abundant VOC in London air. We identify a road transport related source, with ‘rush-hour’ peaks observed. Ethanol is strongly correlated with other road transport-related emissions, such as small aromatics and light alkanes, and has no relationship to summer biogenic emissions. To determine the impact of road transport-related ethanol emission on secondary species (i.e. acetaldehyde and ozone), we use both a chemically detailed box model (incorporating the Master Chemical Mechanism, MCM) and a global and nested regional scale chemical transport model (GEOS-Chem), on various processing time scales. Using the MCM model, only 16% of the modelled acetaldehyde was formed from ethanol oxidation. However, the model significantly underpredicts the total levels of acetaldehyde, indicating a missing primary emission source, that appears to be traffic-related. Further support for a primary emission source comes from the regional scale model simulations, where the observed concentrations of ethanol and acetaldehyde can only be reconciled with the inclusion of large primary emissions. Although only constrained by one set of observations, the regional modelling suggests a European ethanol source similar in magnitude to that of ethane (∼60 Gg per year) and greater than that of acetaldehyde (∼10 Gg per year). The increased concentrations of ethanol and acetaldehyde from primary emissions impacts both radical and NOx cycling over Europe, resulting in significant regional impacts on NOy speciation and O3 concentrations, with potential changes to human exposure to air pollutants.
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Affiliation(s)
| | - Lisa K. Whalley
- School of Chemistry
- University of Leeds
- Leeds
- UK
- National Centre for Atmospheric Science
| | - Tomás Sherwen
- Wolfson Atmospheric Chemistry Laboratory
- University of York
- York
- UK
| | - Mathew J. Evans
- Wolfson Atmospheric Chemistry Laboratory
- University of York
- York
- UK
- National Centre for Atmospheric Science
| | - Dwayne E. Heard
- School of Chemistry
- University of Leeds
- Leeds
- UK
- National Centre for Atmospheric Science
| | - James R. Hopkins
- Wolfson Atmospheric Chemistry Laboratory
- University of York
- York
- UK
- National Centre for Atmospheric Science
| | - James D. Lee
- Wolfson Atmospheric Chemistry Laboratory
- University of York
- York
- UK
- National Centre for Atmospheric Science
| | - Alastair C. Lewis
- Wolfson Atmospheric Chemistry Laboratory
- University of York
- York
- UK
- National Centre for Atmospheric Science
| | | | - Andrew R. Rickard
- Wolfson Atmospheric Chemistry Laboratory
- University of York
- York
- UK
- National Centre for Atmospheric Science
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