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@ARTICLE{Wildt:28375,
      author       = {Wildt, J. and Kobel, K. and Schuh-Thomas, G. and Heiden, A.
                      C.},
      title        = {{E}missions of oxygenated volatile organic compounds from
                      plants {II} : emissions of saturated aldehydes},
      journal      = {Journal of atmospheric chemistry},
      volume       = {45},
      issn         = {0167-7764},
      address      = {Dordrecht [u.a.]},
      publisher    = {Springer Science + Business Media B.V},
      reportid     = {PreJuSER-28375},
      pages        = {173 - 196},
      year         = {2003},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {Emissions of hexanal, heptanal, octanal, nonanal, and
                      decanal from 6 different plant species were measured in
                      continuously stirred tank reactors when the plants were
                      exposed to ozone. Pathogen- and insect attack on plants also
                      led to these emissions. The emission rates of individual
                      aldehydes were related to each other implying a common
                      mechanism for the emissions of these aldehydes. Furthermore,
                      the emission pattern was similar in all cases indicating a
                      similar emission mechanism for different plant species and
                      different elicitors. Measurements with ozone exposed Scots
                      pine plants (Pinus sylvestris L.) showed that the emission
                      rates were dependent on temperature as well as on the ozone
                      flux into the plants. The diurnal variation of aldehyde
                      emissions from ozone exposed Scots pine were described quite
                      well using a formalism including temperature and ozone flux
                      as variables. Assuming the aldehyde emissions to be general
                      for plants exposed to ozone, the global emissions were
                      estimated to be in the range between 7 and 22 Tg/a. Because
                      these emissions can be induced by other factors than ozone
                      uptake alone this estimate may be a lower limit.},
      keywords     = {J (WoSType)},
      cin          = {ICG-II / ICG-III},
      ddc          = {540},
      cid          = {I:(DE-Juel1)VDB48 / I:(DE-Juel1)VDB49},
      pnm          = {Chemie und Dynamik der Geo-Biosphäre},
      pid          = {G:(DE-Juel1)FUEK257},
      shelfmark    = {Environmental Sciences / Meteorology $\&$ Atmospheric
                      Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000183325400003},
      doi          = {10.1023/A:1024030821349},
      url          = {https://juser.fz-juelich.de/record/28375},
}