Chemical composition and hydrolysis of organic nitrate aerosol formed from hydroxyl and nitrate radical oxidation of <i>α</i>-pinene and <i>β</i>-pinene
<p>Atmospheric organic nitrate (ON) is thought to play a crucial role in the formation potential of ozone and aerosol, which are the leading air pollutants of concern across the world. Limited fundamental knowledge and understanding of the life cycles of ON currently hinder the ability to quan...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-10-01
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| Series: | Atmospheric Chemistry and Physics |
| Online Access: | https://www.atmos-chem-phys.net/19/12749/2019/acp-19-12749-2019.pdf |
| Summary: | <p>Atmospheric organic nitrate (ON) is thought to play a crucial role in the
formation potential of ozone and aerosol, which are the leading air
pollutants of concern across the world. Limited fundamental knowledge and
understanding of the life cycles of ON currently hinder the ability to
quantitatively assess its impacts on the formation of these pollutants.
Although hydrolysis is currently considered an important loss mechanism
of ON based on prior field measurement studies, this process for
atmospherically relevant ON has not been well constrained by fundamental
laboratory studies. In this comprehensive study, we investigated the
chemical composition and hydrolysis process of particulate ON (<span class="inline-formula"><sub>p</sub>ON</span>)
formed from the oxidation of <span class="inline-formula"><i>α</i></span>-pinene and <span class="inline-formula"><i>β</i></span>-pinene by
hydroxyl (<span class="inline-formula">OH<span class="Radical">⚫</span></span>) and nitrate radicals (<span class="inline-formula">NO<sub>3</sub><span class="Radical">⚫</span></span>). For
<span class="inline-formula"><sub>p</sub>ON</span> that undergoes hydrolysis, the hydrolysis lifetime is determined to
be no more than 30 <span class="inline-formula">min</span> for all systems explored. This is significantly
shorter than those reported in previous chamber studies (i.e., 3–6 <span class="inline-formula">h</span>) but is
consistent with the reported lifetime from bulk solution measurement studies
(i.e., 0.02–8.8 <span class="inline-formula">h</span>). The discrepancy appears to stem from the choice of proxy
used to estimate the hydrolysis lifetime. The measured hydrolyzable
fractions of <span class="inline-formula"><sub>p</sub>ON</span> (<span class="inline-formula"><i>F</i><sub>H</sub></span>) in the <span class="inline-formula"><i>α</i></span>-pinene <span class="inline-formula">+</span> <span class="inline-formula">OH<span class="Radical">⚫</span></span>,
<span class="inline-formula"><i>β</i></span>-pinene <span class="inline-formula">+</span> <span class="inline-formula">OH<span class="Radical">⚫</span></span>, <span class="inline-formula"><i>α</i></span>-pinene <span class="inline-formula">+</span> <span class="inline-formula">NO<sub>3</sub><span class="Radical">⚫</span></span>,
and <span class="inline-formula"><i>β</i></span>-pinene <span class="inline-formula">+</span> <span class="inline-formula">NO<sub>3</sub><span class="Radical">⚫</span></span> systems are 23 %–32 %, 27 %–34 %, 9 %–17 %,
and 9 %–15 %, respectively. While a very low <span class="inline-formula"><i>F</i><sub>H</sub></span> for the
<span class="inline-formula">NO<sub>3</sub><span class="Radical">⚫</span></span> oxidation system is expected based on prior studies,
<span class="inline-formula"><i>F</i><sub>H</sub></span> for the <span class="inline-formula">OH<span class="Radical">⚫</span></span> oxidation system is surprisingly lower than
predicted in past studies. Overall, the hydrolysis lifetime as well as
<span class="inline-formula"><i>F</i><sub>H</sub></span> obtained in this study serve as experimentally constrained
parameters that are required in regional and global chemical transport
models to accurately evaluate the impacts of ON on nitrogen budget and
formation of ozone and aerosol.</p> |
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| ISSN: | 1680-7316 1680-7324 |