Articles | Volume 10, issue 3
Atmos. Chem. Phys., 10, 1441–1459, 2010
https://doi.org/10.5194/acp-10-1441-2010
Atmos. Chem. Phys., 10, 1441–1459, 2010
https://doi.org/10.5194/acp-10-1441-2010

  10 Feb 2010

10 Feb 2010

Measurements of OH and HO2 yields from the gas phase ozonolysis of isoprene

T. L. Malkin et al.

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Subject: Gases | Research Activity: Laboratory Studies | Altitude Range: Troposphere | Science Focus: Chemistry (chemical composition and reactions)
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Cited articles

Arneth, A., Monson, R. K., Schurgers, G., Niinemets, Ü., and Palmer, P. I.: Why are estimates of global terrestrial isoprene emissions so similar (and why is this not so for monoterpenes)?, Atmos. Chem. Phys., 8, 4605–4620, 2008.
Asatryan, R. and Bozzelli, J. W.: Formation of a Criegee intermediate in the low-temperature oxidation of dimethyl sulfoxide, Phys. Chem. Chem. Phys., 10, 1769–1780, 2008.
Aschmann, S. M and Atkinson, R.: Formation yields of methyl vinyl ketone and methacrolein from the gas-phase reaction of O3 with isoprene, Environ. Sci. Technol., 28(8), 1539–1542, 1994.
Aschmann, S. M., Arey, J., and Atkinson, R.: OH radical formation from the gas-phase reactions of O3 with methacrolein and methyl vinyl ketone, Atmos. Environ., 30, 2939–2943, 1996.
Atkinson, R. and Aschmann, S. M.: Rate constants for the gas-phase reactions of the OH radical with a series of aromatic hydrocarbons at 296±2 K, Int. J. Chem. Kinet., 21, 355–365, 1989.
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