Stable carbon isotope ratios of ambient aromatic volatile organic compounds

Measurements of mixing ratios and stable carbon isotope ratios of aromatic volatile organic compounds (VOC) in the atmosphere were made in Toronto (Canada) in 2009 and 2010. Consistent with the kinetic isotope effect for reactions of aromatic VOC with the OH radical the observed stable carbon is...

Full description

Bibliographic Details
Main Authors: A. Kornilova, L. Huang, M. Saccon, J. Rudolph
Format: Article
Language:English
Published: Copernicus Publications 2016-09-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/11755/2016/acp-16-11755-2016.pdf
id doaj-0f6139a156564cf4a6a85fe5b5dc75a5
record_format Article
spelling doaj-0f6139a156564cf4a6a85fe5b5dc75a52020-11-25T00:04:51ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-09-0116117551177210.5194/acp-16-11755-2016Stable carbon isotope ratios of ambient aromatic volatile organic compoundsA. Kornilova0L. Huang1M. Saccon2J. Rudolph3Centre for Atmospheric Chemistry, York University, Toronto, ON, M3J 1P3, CanadaEnvironment Canada, Toronto, ON, M3H 5T4, CanadaCentre for Atmospheric Chemistry, York University, Toronto, ON, M3J 1P3, CanadaCentre for Atmospheric Chemistry, York University, Toronto, ON, M3J 1P3, CanadaMeasurements of mixing ratios and stable carbon isotope ratios of aromatic volatile organic compounds (VOC) in the atmosphere were made in Toronto (Canada) in 2009 and 2010. Consistent with the kinetic isotope effect for reactions of aromatic VOC with the OH radical the observed stable carbon isotope ratios are on average significantly heavier than the isotope ratios of their emissions. The change of carbon isotope ratio between emission and observation is used to determine the extent of photochemical processing (photochemical age,  <mo form="infix">∫</mo> [OH]d<i>t</i>) of the different VOC. It is found that  <mo form="infix">∫</mo> [OH]d<i>t</i> of different VOC depends strongly on the VOC reactivity. This demonstrates that for this set of observations the assumption of a uniform  <mo form="infix">∫</mo> [OH]d<i>t</i> for VOC with different reactivity is not justified and that the observed values for  <mo form="infix">∫</mo> [OH]d<i>t</i> are the result of mixing of VOC from air masses with different values for  <mo form="infix">∫</mo> [OH]d<i>t</i>. Based on comparison between carbon isotope ratios and VOC concentration ratios it is also found that the varying influence of sources with different VOC emission ratios has a larger impact on VOC concentration ratios than photochemical processing. It is concluded that for this data set the use of VOC concentration ratios to determine  <mo form="infix">∫</mo> [OH]d<i>t</i> would result in values for  <mo form="infix">∫</mo> [OH]d<i>t</i> inconsistent with carbon isotope ratios and that the concept of a uniform  <mo form="infix">∫</mo> [OH]d<i>t</i> for an air mass has to be replaced by the concept of individual values of an average  <mo form="infix">∫</mo> [OH]d<i>t</i> for VOC with different reactivity.</p>https://www.atmos-chem-phys.net/16/11755/2016/acp-16-11755-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Kornilova
L. Huang
M. Saccon
J. Rudolph
spellingShingle A. Kornilova
L. Huang
M. Saccon
J. Rudolph
Stable carbon isotope ratios of ambient aromatic volatile organic compounds
Atmospheric Chemistry and Physics
author_facet A. Kornilova
L. Huang
M. Saccon
J. Rudolph
author_sort A. Kornilova
title Stable carbon isotope ratios of ambient aromatic volatile organic compounds
title_short Stable carbon isotope ratios of ambient aromatic volatile organic compounds
title_full Stable carbon isotope ratios of ambient aromatic volatile organic compounds
title_fullStr Stable carbon isotope ratios of ambient aromatic volatile organic compounds
title_full_unstemmed Stable carbon isotope ratios of ambient aromatic volatile organic compounds
title_sort stable carbon isotope ratios of ambient aromatic volatile organic compounds
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-09-01
description Measurements of mixing ratios and stable carbon isotope ratios of aromatic volatile organic compounds (VOC) in the atmosphere were made in Toronto (Canada) in 2009 and 2010. Consistent with the kinetic isotope effect for reactions of aromatic VOC with the OH radical the observed stable carbon isotope ratios are on average significantly heavier than the isotope ratios of their emissions. The change of carbon isotope ratio between emission and observation is used to determine the extent of photochemical processing (photochemical age,  <mo form="infix">∫</mo> [OH]d<i>t</i>) of the different VOC. It is found that  <mo form="infix">∫</mo> [OH]d<i>t</i> of different VOC depends strongly on the VOC reactivity. This demonstrates that for this set of observations the assumption of a uniform  <mo form="infix">∫</mo> [OH]d<i>t</i> for VOC with different reactivity is not justified and that the observed values for  <mo form="infix">∫</mo> [OH]d<i>t</i> are the result of mixing of VOC from air masses with different values for  <mo form="infix">∫</mo> [OH]d<i>t</i>. Based on comparison between carbon isotope ratios and VOC concentration ratios it is also found that the varying influence of sources with different VOC emission ratios has a larger impact on VOC concentration ratios than photochemical processing. It is concluded that for this data set the use of VOC concentration ratios to determine  <mo form="infix">∫</mo> [OH]d<i>t</i> would result in values for  <mo form="infix">∫</mo> [OH]d<i>t</i> inconsistent with carbon isotope ratios and that the concept of a uniform  <mo form="infix">∫</mo> [OH]d<i>t</i> for an air mass has to be replaced by the concept of individual values of an average  <mo form="infix">∫</mo> [OH]d<i>t</i> for VOC with different reactivity.</p>
url https://www.atmos-chem-phys.net/16/11755/2016/acp-16-11755-2016.pdf
work_keys_str_mv AT akornilova stablecarbonisotoperatiosofambientaromaticvolatileorganiccompounds
AT lhuang stablecarbonisotoperatiosofambientaromaticvolatileorganiccompounds
AT msaccon stablecarbonisotoperatiosofambientaromaticvolatileorganiccompounds
AT jrudolph stablecarbonisotoperatiosofambientaromaticvolatileorganiccompounds
_version_ 1725427645309517824