<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Gu, F. T.</style></author><author><style face="normal" font="default" size="100%">Min* Hu</style></author><author><style face="normal" font="default" size="100%">Zheng, J.</style></author><author><style face="normal" font="default" size="100%">Guo, S.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Research Progress on Particulate Organonitrates</style></title><secondary-title><style face="normal" font="default" size="100%">Progress in Chemistry</style></secondary-title><alt-title><style face="normal" font="default" size="100%">Prog Chem</style></alt-title><short-title><style face="normal" font="default" size="100%">Prog ChemProg Chem</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">ams</style></keyword><keyword><style  face="normal" font="default" size="100%">aromatic-hydrocarbons</style></keyword><keyword><style  face="normal" font="default" size="100%">cims</style></keyword><keyword><style  face="normal" font="default" size="100%">field measurements</style></keyword><keyword><style  face="normal" font="default" size="100%">henrys law constants</style></keyword><keyword><style  face="normal" font="default" size="100%">hydroxy alkyl nitrates</style></keyword><keyword><style  face="normal" font="default" size="100%">mass-spectrometry</style></keyword><keyword><style  face="normal" font="default" size="100%">n-alkanes</style></keyword><keyword><style  face="normal" font="default" size="100%">nox-air photooxidations</style></keyword><keyword><style  face="normal" font="default" size="100%">organonitrates</style></keyword><keyword><style  face="normal" font="default" size="100%">radical-initiated reactions</style></keyword><keyword><style  face="normal" font="default" size="100%">secondary organic aerosol</style></keyword><keyword><style  face="normal" font="default" size="100%">secondary organic aerosols</style></keyword><keyword><style  face="normal" font="default" size="100%">soa formation</style></keyword><keyword><style  face="normal" font="default" size="100%">southeastern united-states</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2017</style></year><pub-dates><date><style  face="normal" font="default" size="100%">Sep</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">9</style></number><volume><style face="normal" font="default" size="100%">29</style></volume><pages><style face="normal" font="default" size="100%">962-969</style></pages><isbn><style face="normal" font="default" size="100%">1005-281X</style></isbn><language><style face="normal" font="default" size="100%">Chinese</style></language><abstract><style face="normal" font="default" size="100%">Particulate organonitrates are formed from volatile organic compounds (VOCs) oxidation by radicals. A portion of semi-volatile gas-phase organonitrates can be incorporate into aerosol by oxidation reactions or portioning, and has been an important component of secondary organic aerosol (SOA). Particulate organonitrates study has become one of the important aspects of atmospheric chemistry. Given the large number and variability of chemical constituents, and possible chemical transformations of organonitrates, such characterization presents a key problem for research. Based on recent research progress on particulate organonitrates, this paper summarizes the formation mechanism and quantification method of particulate organonitrates. Profiting from the application of high time resolution techniques, field measurements has become the major approach of particulate organonitrates study. Thermal dissociation-laser induced fluorescence (TD-LIF) and aerosol mass spectrometers (AMS) have been used to quantify and provide the evolution processes of particulate organonirates. Meanwhile, chemical ionization mass spectrometer(CIMS)allows for the determination of molecular ion composition of organonitrates, promising to become the important direction of study of particulate organonirates in future field measurements. To have a deep insight on precursor and atmospheric chemistry processes of particulate organonirates, future research should focus on the combination of field measurement, modeling simulation and laboratory simulation, and these will also lead to a more comprehensive understanding of formation mechanism of particulate organonirates</style></abstract><accession-num><style face="normal" font="default" size="100%">ISI:000416303500005</style></accession-num><notes><style face="normal" font="default" size="100%">&lt;p&gt;Fn8viTimes Cited:0Cited References Count:58&lt;/p&gt;</style></notes><auth-address><style face="normal" font="default" size="100%">Peking Univ, Coll Environm Sci &amp;amp;amp;amp; Engn, State Key Joint Lab Environm Simulat &amp;amp;amp;amp; Pollut Con, Beijing 100871, Peoples R China</style></auth-address></record></records></xml>