The gas-phase formation mechanism of iodic acid as an atmospheric aerosol source

被引:0
作者
Henning Finkenzeller
Siddharth Iyer
Xu-Cheng He
Mario Simon
Theodore K. Koenig
Christopher F. Lee
Rashid Valiev
Victoria Hofbauer
Antonio Amorim
Rima Baalbaki
Andrea Baccarini
Lisa Beck
David M. Bell
Lucía Caudillo
Dexian Chen
Randall Chiu
Biwu Chu
Lubna Dada
Jonathan Duplissy
Martin Heinritzi
Deniz Kemppainen
Changhyuk Kim
Jordan Krechmer
Andreas Kürten
Alexandr Kvashnin
Houssni Lamkaddam
Chuan Ping Lee
Katrianne Lehtipalo
Zijun Li
Vladimir Makhmutov
Hanna E. Manninen
Guillaume Marie
Ruby Marten
Roy L. Mauldin
Bernhard Mentler
Tatjana Müller
Tuukka Petäjä
Maxim Philippov
Ananth Ranjithkumar
Birte Rörup
Jiali Shen
Dominik Stolzenburg
Christian Tauber
Yee Jun Tham
António Tomé
Miguel Vazquez-Pufleau
Andrea C. Wagner
Dongyu S. Wang
Mingyi Wang
Yonghong Wang
机构
[1] University of Colorado Boulder,Department of Chemistry
[2] University of Colorado Boulder,Cooperative Institute for Research in Environmental Sciences
[3] Tampere University,Aerosol Physics Laboratory, Physics Unit, Faculty of Engineering and Natural Sciences
[4] University of Helsinki,Institute for Atmospheric and Earth System Research
[5] Goethe University Frankfurt,Institute for Atmospheric and Environmental Sciences
[6] Peking University,State Key Joint Laboratory of Environmental Simulation and Pollution Control, BIC
[7] University of Helsinki,ESAT and IJRC, College of Environmental Sciences and Engineering
[8] Carnegie Mellon University,Department of Chemistry
[9] CENTRA and Faculdade de Ciências da Universidade de Lisboa,Center for Atmospheric Particle Studies
[10] Paul Scherrer Institute,Laboratory of Atmospheric Chemistry
[11] École Polytechnique Fédérale de Lausanne,Extreme Environments Research Laboratory
[12] Chinese Academy of Science,Research Center for Eco
[13] University of Helsinki,Environmental Sciences
[14] Pusan National University,Helsinki Institute of Physics (HIP) / Physics, Faculty of Science
[15] California Institute of Technology,School of Civil and Environmental Engineering
[16] Aerodyne Research,Division of Chemistry and Chemical Engineering
[17] P.N. Lebedev Physical Institute of the Russian Academy of Sciences,Department of Applied Physics
[18] Finnish Meteorological Institute,Institute of Ion and Applied Physics
[19] University of Eastern Finland,School of Earth and Environment
[20] Moscow Institute of Physics and Technology (National Research University),Faculty of Physics
[21] CERN,School of Marine Sciences
[22] the European Organization for Nuclear Research,Joint International Research Laboratory of Atmospheric and Earth System Research, School of Atmospheric Sciences
[23] University of Innsbruck,LACy UMR8105
[24] University of Leeds,Aerosol and Haze Laboratory, Beijing Advanced Innovation Center for Soft Matter Sciences and Engineering
[25] University of Vienna,undefined
[26] Sun Yat-sen University,undefined
[27] IDL-Universidade da Beira Interior,undefined
[28] Nanjing University,undefined
[29] Université de la Réunion,undefined
[30] Beijing University of Chemical Technology (BUCT),undefined
来源
Nature Chemistry | 2023年 / 15卷
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摘要
Iodine is a reactive trace element in atmospheric chemistry that destroys ozone and nucleates particles. Iodine emissions have tripled since 1950 and are projected to keep increasing with rising O3 surface concentrations. Although iodic acid (HIO3) is widespread and forms particles more efficiently than sulfuric acid, its gas-phase formation mechanism remains unresolved. Here, in CLOUD atmospheric simulation chamber experiments that generate iodine radicals at atmospherically relevant rates, we show that iodooxy hypoiodite, IOIO, is efficiently converted into HIO3 via reactions (R1) IOIO + O3 → IOIO4 and (R2) IOIO4 + H2O → HIO3 + HOI + (1)O2. The laboratory-derived reaction rate coefficients are corroborated by theory and shown to explain field observations of daytime HIO3 in the remote lower free troposphere. The mechanism provides a missing link between iodine sources and particle formation. Because particulate iodate is readily reduced, recycling iodine back into the gas phase, our results suggest a catalytic role of iodine in aerosol formation.
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页码:129 / 135
页数:6
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共 116 条
  • [11] Sipilä M(1994)On the role of iodine in ozone depletion J. Geophys. Res. Atmos. 99 20491-20499
  • [12] He X-C(1981)Emission of iodine from the sea surface in the presence of ozone J. Geophys. Res. Ocean. 86 3183-3186
  • [13] He X-C(2013)Atmospheric iodine levels influenced by sea surface emissions of inorganic iodine Nat. Geosci. 6 108-111
  • [14] Solomon S(2020)Aircraft observations since the 1990s reveal increases of tropospheric ozone at multiple locations across the Northern Hemisphere Sci. Adv. 6 eaba8272-12141
  • [15] Garcia RR(2018)Alpine ice evidence of a three-fold increase in atmospheric iodine deposition since 1950 in Europe due to increasing oceanic emissions Proc. Natl Acad. Sci. USA 115 12136-12271
  • [16] Ravishankara AR(2018)Rapid increase in atmospheric iodine levels in the North Atlantic since the mid-20th century Nat. Commun. 9 1452-8714
  • [17] Garland JA(2016)Global impacts of tropospheric halogens (Cl, Br, I) on oxidants and composition in GEOS-Chem Atmos. Chem. Phys. 16 12239-1866
  • [18] Curtis H(2021)Marine iodine emissions in a changing world Proc. R. Soc. A Math. Phys. Eng. Sci. 477 20200824-2040
  • [19] Carpenter LJ(2019)Atmospheric iodine ( Environ. Sci. Technol. 53 8706-9286
  • [20] Gaudel A(2020)I and Proc. Natl Acad. Sci. USA 117 1860-1804