@article{
 title = {Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth},
 type = {article},
 year = {2008},
 keywords = {aerosol,events,mass-spectrometry,nuclei,particle formation,rates,scales,secondary,size distributions},
 pages = {L04808},
 volume = {35},
 websites = {http://doi.wiley.com/10.1029/2007GL032523},
 month = {2},
 day = {22},
 id = {2af0f305-929f-32ac-a196-77bc8dd3fc52},
 created = {2023-01-31T22:46:06.376Z},
 file_attached = {false},
 profile_id = {2e2b0bf1-6573-3fd8-8628-55d1dc39fe31},
 last_modified = {2023-01-31T22:46:06.376Z},
 read = {false},
 starred = {false},
 authored = {true},
 confirmed = {true},
 hidden = {false},
 citation_key = {Smith2008a},
 source_type = {Journal Article},
 language = {English},
 notes = {<b>From Duplicate 1 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, Jim N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/><b>From Duplicate 1 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, J. N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/>267TD<br/>Times Cited:87<br/>Cited References Count:26<br/><br/><b>From Duplicate 2 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, Jim N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/>Cited References Count:26|AMER GEOPHYSICAL UNION|2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA|ISI Document Delivery No.:267TD<br/><br/><b>From Duplicate 2 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, J. N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/>267TD<br/>Times Cited:87<br/>Cited References Count:26},
 private_publication = {false},
 abstract = {We report Thermal Desorption Chemical Ionization Mass Spectrometer (TDCIMS) measurements of the composition of ambient 10-33 nm diameter particles formed from nucleation on 16 March 2006 in Tecamac, Mexico during the Megacity Initiative: Local and Global Research Observations (MILAGRO) field study. On this day, nucleated particles contained far more organics than sulfates: average ion molar ratios with measurement uncertainties for nitrate, organics and sulfur species were 6±2%, 84±5%, and 10±1%, respectively. The measured organic species include nitrogen-containing organic compounds, organic acids, and hydroxy organic acids. Independent calculations show that sulfuric acid condensation could have accounted for only 10±2% of the growth that was observed on this day, which is consistent with the TDCIMS measurements of composition. It follows that organic compounds play a dominant role the high growth rates that were observed. Copyright 2008 by the American Geophysical Union.},
 bibtype = {article},
 author = {Smith, Jim N. and Dunn, M. J. and VanReken, T. M. and Iida, K. and Stolzenburg, M. R. and McMurry, P. H. and Huey, L. G.},
 doi = {10.1029/2007GL032523},
 journal = {Geophysical Research Letters},
 number = {4}
}

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J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/><b>From Duplicate 1 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, J. N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/>267TD<br/>Times Cited:87<br/>Cited References Count:26<br/><br/><b>From Duplicate 2 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, Jim N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/>Cited References Count:26|AMER GEOPHYSICAL UNION|2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA|ISI Document Delivery No.:267TD<br/><br/><b>From Duplicate 2 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, J. N.; Dunn, M. J.; VanReken, T. M.; Iida, K.; Stolzenburg, M. R.; McMurry, P. H.; Huey, L. G.)<br/></b><br/>267TD<br/>Times Cited:87<br/>Cited References Count:26","private_publication":false,"abstract":"We report Thermal Desorption Chemical Ionization Mass Spectrometer (TDCIMS) measurements of the composition of ambient 10-33 nm diameter particles formed from nucleation on 16 March 2006 in Tecamac, Mexico during the Megacity Initiative: Local and Global Research Observations (MILAGRO) field study. On this day, nucleated particles contained far more organics than sulfates: average ion molar ratios with measurement uncertainties for nitrate, organics and sulfur species were 6±2%, 84±5%, and 10±1%, respectively. The measured organic species include nitrogen-containing organic compounds, organic acids, and hydroxy organic acids. Independent calculations show that sulfuric acid condensation could have accounted for only 10±2% of the growth that was observed on this day, which is consistent with the TDCIMS measurements of composition. It follows that organic compounds play a dominant role the high growth rates that were observed. Copyright 2008 by the American Geophysical Union.","bibtype":"article","author":"Smith, Jim N. and Dunn, M. J. and VanReken, T. M. and Iida, K. and Stolzenburg, M. R. and McMurry, P. H. and Huey, L. G.","doi":"10.1029/2007GL032523","journal":"Geophysical Research Letters","number":"4","bibtex":"@article{\n title = {Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth},\n type = {article},\n year = {2008},\n keywords = {aerosol,events,mass-spectrometry,nuclei,particle formation,rates,scales,secondary,size distributions},\n pages = {L04808},\n volume = {35},\n websites = {http://doi.wiley.com/10.1029/2007GL032523},\n month = {2},\n day = {22},\n id = {2af0f305-929f-32ac-a196-77bc8dd3fc52},\n created = {2023-01-31T22:46:06.376Z},\n file_attached = {false},\n profile_id = {2e2b0bf1-6573-3fd8-8628-55d1dc39fe31},\n last_modified = {2023-01-31T22:46:06.376Z},\n read = {false},\n starred = {false},\n authored = {true},\n confirmed = {true},\n hidden = {false},\n citation_key = {Smith2008a},\n source_type = {Journal Article},\n language = {English},\n notes = {<b>From Duplicate 1 (<i>Chemical composition of atmospheric nanoparticles formed from nucleation in Tecamac, Mexico: Evidence for an important role for organic species in nanoparticle growth</i> - Smith, Jim N.; Dunn, M. 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