% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Keel:835141,
      author       = {Keßel, Stephan and Cabrera-Perez, David and Horowitz,
                      Abraham and Veres, Patrick R. and Sander, Rolf and
                      Taraborrelli, Domenico and Tucceri, Maria and Crowley, John
                      N. and Pozzer, Andrea and Stönner, Christof and Vereecken,
                      Luc and Lelieveld, Jos and Williams, Jonathan},
      title        = {{A}tmospheric chemistry, sources and sinks of carbon
                      suboxide, {C}3{O}2},
      journal      = {Atmospheric chemistry and physics},
      volume       = {17},
      number       = {14},
      issn         = {1680-7324},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {FZJ-2017-05009},
      pages        = {8789 - 8804},
      year         = {2017},
      abstract     = {Carbon suboxide,
                      O  =  C  =  C  =  C  =  O,
                      has been detected in ambient air samples and has the
                      potential to be a noxious pollutant and oxidant precursor;
                      however, its lifetime and fate in the atmosphere are largely
                      unknown. In this work, we collect an extensive set of
                      studies on the atmospheric chemistry of C3O2. Rate
                      coefficients for the reactions of C3O2 with OH radicals and
                      ozone were determined as
                      kOH =  (2.6 ± 0.5)  ×  10−12 cm3 molecule−1 s−1
                      at 295 K (independent of pressure between  ∼  25
                      and 1000 mbar) and
                      kO3  <  1.5  ×  10−21 cm3 molecule−1 s−1
                      at 295 K. A theoretical study on the mechanisms of these
                      reactions indicates that the sole products are CO and CO2,
                      as observed experimentally. The UV absorption spectrum and
                      the interaction of C3O2 with water (Henry's law solubility
                      and hydrolysis rate constant) were also investigated,
                      enabling its photodissociation lifetime and hydrolysis
                      rates, respectively, to be assessed.},
      cin          = {IEK-8},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-8-20101013},
      pnm          = {243 - Tropospheric trace substances and their
                      transformation processes (POF3-243)},
      pid          = {G:(DE-HGF)POF3-243},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000405864000001},
      doi          = {10.5194/acp-17-8789-2017},
      url          = {https://juser.fz-juelich.de/record/835141},
}