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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 24 | Copyright
Atmos. Chem. Phys., 17, 15137-15150, 2017
https://doi.org/10.5194/acp-17-15137-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 21 Dec 2017

Research article | 21 Dec 2017

Temperature-dependent rate coefficients for the reactions of the hydroxyl radical with the atmospheric biogenics isoprene, alpha-pinene and delta-3-carene

Terry J. Dillon1,a, Katrin Dulitz1,b, Christoph B. M. Groß1, and John N. Crowley1 Terry J. Dillon et al.
  • 1Department of Air Chemistry, Max Planck Institute for Chemistry, 55128 Mainz, Germany
  • anow at: Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, YO10 5DD, York, UK
  • bnow at: Physikalisches Institut, University of Freiburg, Hermann-Herder Str. 3, 79104 Freiburg, Germany

Abstract. Pulsed laser methods for OH generation and detection were used to study atmospheric degradation reactions for three important biogenic gases: OH+isoprene (Reaction R1), OH+α-pinene (Reaction R2) and OH+Δ-3-carene (Reaction R3). Gas-phase rate coefficients were characterized by non-Arrhenius kinetics for all three reactions. For (R1), k1 (241–356K) = (1.93±0.08) × 10−11exp{(466±12)∕T}cm3molecule−1s−1 was determined, with a room temperature value of k1 (297K) = (9.3±0.4) × 10−11cm3molecule−1s−1, independent of bath-gas pressure (5–200Torr) and composition (M = N2 or air). Accuracy and precision were enhanced by online optical monitoring of isoprene, with absolute concentrations obtained via an absorption cross section, σisoprene = (1.28±0.06) × 10−17cm2molecule−1 at λ = 184.95nm, determined in this work. These results indicate that significant discrepancies between previous absolute and relative-rate determinations of k1 result in part from σ values used to derive the isoprene concentration in high-precision absolute determinations.

Similar methods were used to determine rate coefficients (in 10−11cm3molecule−1s−1) for (R2)–(R3): k2 (238–357K) = (1.83±0.04) × exp{(330±6)∕T} and k3 (235–357K) = (2.48±0.14) × exp{(357±17)∕T}. This is the first temperature-dependent dataset for (R3) and enables the calculation of reliable atmospheric lifetimes with respect to OH removal for e.g. boreal forest springtime conditions. Room temperature values of k2 (296K) = (5.4±0.2) × 10−11cm3molecule−1s−1 and k3 (297K) = (8.1±0.3) × 10−11cm3molecule−1s−1 were independent of bath-gas pressure (7–200Torr, N2 or air) and in good agreement with previously reported values. In the course of this work, 184.95nm absorption cross sections were determined: σ = (1.54±0.08) × 10−17cm2molecule−1 for α-pinene and (2.40±0.12) × 10−17cm2molecule−1 for Δ-3-carene.

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A great quantity and variety of organic compounds is released to the atmosphere annually. These compounds greatly impact air chemistry, quality and climate. Laser-based experiments were used to study the atmospheric breakdown of three organics: isoprene, alpha-pinene, and delta-3-carene. Results provided important missing information for low-temperature atmospheric conditions, resolved discrepancies from previous work, and allowed estimation of lifetimes of a few hours for each compound.
A great quantity and variety of organic compounds is released to the atmosphere annually. These...
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