@article{
 title = {Hydrolysis and gas-particle partitioning of organic nitrates formed from the oxidation of α-pinene in environmental chamber experiments},
 type = {article},
 year = {2015},
 identifiers = {[object Object]},
 pages = {20629-20653},
 volume = {15},
 websites = {http://www.atmos-chem-phys-discuss.net/15/20629/2015/},
 id = {bd06f690-24ed-35a0-8e12-4420c6dc6879},
 created = {2016-10-05T03:31:12.000Z},
 file_attached = {false},
 profile_id = {81af7548-db00-3f00-bfa0-1774347c59e1},
 group_id = {63e349d6-2c70-3938-9e67-2f6483f6cbab},
 last_modified = {2016-10-05T03:31:12.000Z},
 read = {false},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 abstract = {<p>Gas-particle partitioning and hydrolysis of organic nitrates (ON) influences their role as sinks and sources of NO<sub><i>x</i></sub> and their effects on the formation of tropospheric ozone and organic aerosol (OA). Organic nitrates were formed from the photo-oxidation of α-pinene in environmental chamber experiments under varying conditions. A hydrolysis rate of 2 day<sup>&minus;1</sup> was found for particle-phase ONs at a relative humidity of 22 % or higher; no significant ON hydrolysis was observed at lower relative humidity. The ON gas-particle partitioning is dependent on total OA concentration and temperature, consistent with absorptive partitioning theory. In a volatility basis set the ON partitioning is consistent with mass fractions of [0 0.19 0.29 0.52] at saturations mass concentrations (<i>C</i><sup>*</sup>) of [1 10 100 1000] &mu;g m<sup>&minus;3</sup>.</p>},
 bibtype = {article},
 author = {Bean, J. K. and Hildebrandt Ruiz, L.},
 journal = {Atmospheric Chemistry and Physics Discussions},
 number = {14}
}

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