<?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%">Wang, H. C.</style></author><author><style face="normal" font="default" size="100%">Tang, M. J.</style></author><author><style face="normal" font="default" size="100%">Tan, Z. F.</style></author><author><style face="normal" font="default" size="100%">Peng, C.</style></author><author><style face="normal" font="default" size="100%">Lu, K. D.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Atmospheric Chemistry of Nitryl Chloride</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. Chem.</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">atmospheric oxidation</style></keyword><keyword><style  face="normal" font="default" size="100%">boundary-layer</style></keyword><keyword><style  face="normal" font="default" size="100%">chlorine chemistry</style></keyword><keyword><style  face="normal" font="default" size="100%">clno2 production</style></keyword><keyword><style  face="normal" font="default" size="100%">dinitrogen pentoxide</style></keyword><keyword><style  face="normal" font="default" size="100%">gaseous n2o5</style></keyword><keyword><style  face="normal" font="default" size="100%">heterogeneous n2o5 uptake</style></keyword><keyword><style  face="normal" font="default" size="100%">heterogeneous reaction</style></keyword><keyword><style  face="normal" font="default" size="100%">mass-spectrometer</style></keyword><keyword><style  face="normal" font="default" size="100%">nighttime reactive nitrogen chemistry</style></keyword><keyword><style  face="normal" font="default" size="100%">nitrate</style></keyword><keyword><style  face="normal" font="default" size="100%">nitrate formation</style></keyword><keyword><style  face="normal" font="default" size="100%">nitryl chloride</style></keyword><keyword><style  face="normal" font="default" size="100%">ozone</style></keyword><keyword><style  face="normal" font="default" size="100%">ozone production</style></keyword><keyword><style  face="normal" font="default" size="100%">power-plant</style></keyword><keyword><style  face="normal" font="default" size="100%">uptake coefficients</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2020</style></year><pub-dates><date><style  face="normal" font="default" size="100%">Oct 24</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">10</style></number><volume><style face="normal" font="default" size="100%">32</style></volume><pages><style face="normal" font="default" size="100%">1535-1546</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%">As an important reactive trace gases in the troposphere, nitryl chloride (ClNO2) has significant impacts on atmospheric oxidation capacity , the degradation of primary pollutants and the formation of secondary pollutants, and plays indispensable roles in global cycles of both nitrogen and chlorine. In this paper, we introduce basic properties of ClNO2 as well as its formation and removal mechanisms in the troposphere, and describe in brief techniques currently used in laboratory and field work to measure ClNO2. In addition , we review spatial and temporal distributions of tropospheric ClNO2 over the globe as reported in the last 10 similar to 20 years , discuss in a systematical manner chemical mechanisms and environmental factors which determine its heterogeneous formation in the atmosphere via critical analysis of important results from laboratory studies and field measurements, and summarize impacts of ClNO(2 )on chlorine radicals, atmospheric oxidation capacity as well as the formation of O-3 and nitrate aerosol. We emphasize that ClNO2 couples gas phase chemistry and heterogeneous chemistry , and also couples nocturnal atmospheric chemistry with daytime photochemistry , thus very likely playing an important role in the formation of air pollution complex in China. Important questions which remain to be answered to better understand atmospheric chemistry of ClNO2 are outlined at the end, and we also discuss in brief how these questions can be addressed in future work.</style></abstract><accession-num><style face="normal" font="default" size="100%">WOS:000596561300008</style></accession-num><notes><style face="normal" font="default" size="100%">&lt;p&gt;Pb8jrTimes Cited:0Cited References Count:75&lt;/p&gt;</style></notes><auth-address><style face="normal" font="default" size="100%">Peking Univ, Coll Environm Sci &amp;amp;amp; Engn, State Key Lab Environm Simulat &amp;amp;amp; Pollut Control, Beijing 100871, Peoples R ChinaChinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Peoples R ChinaChinese Acad Sci, Guangzhou Inst Geochem, Guangdong Key Lab Environm Protect &amp;amp;amp; Resources Ut, Guangzhou 510640, Peoples R ChinaForschungszentrum Julich, Inst Energy &amp;amp;amp; Climate Res, IEK 8 Troposphere, D-52425 Julich, Germany</style></auth-address></record></records></xml>