Abstract
The rapid reaction of the smallest Criegee intermediate, CH2OO, with water dimers is the dominant removal mechanism for CH2OO
in the Earth’s atmosphere, but its products are not well understood.
This reaction was recently suggested as a significant source of the most
abundant tropospheric organic acid, formic acid (HCOOH), which is
consistently underpredicted by atmospheric models. However, using
time-resolved measurements of reaction kinetics by UV absorption and
product analysis by photoionization mass spectrometry, we show that the
primary products of this reaction are formaldehyde and hydroxymethyl
hydroperoxide (HMHP), with direct HCOOH yields of less than 10%.
Incorporating our results into a global chemistry-transport model
further reduces HCOOH levels by 10 – 90%, relative to previous
assumptions, which indicates that the reaction CH2OO + water dimer by itself cannot resolve the discrepancy between the measured and predicted HCOOH levels.
Original language | English |
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Pages (from-to) | 21970-21979 |
Number of pages | 10 |
Journal | Physical Chemistry Chemical Physics |
Volume | 19 |
Issue number | 33 |
Early online date | 4 Aug 2017 |
DOIs | |
Publication status | Published - 7 Sep 2017 |
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Profiles
-
Professor Dudley E Shallcross
- School of Chemistry - Professor of Atmospheric Chemistry
- Cabot Institute for the Environment
- Spectroscopy and Dynamics
- Atmospheric and Global Change Chemistry
- Computational and Theoretical Chemistry
- Atmospheric Chemistry
Person: Academic , Member