<?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%">Chen, X. R.</style></author><author><style face="normal" font="default" size="100%">Lu, K. D.</style></author><author><style face="normal" font="default" size="100%">Tan, Z. F.</style></author><author><style face="normal" font="default" size="100%">Ma, XF</style></author><author><style face="normal" font="default" size="100%">ZJ Wu</style></author><author><style face="normal" font="default" size="100%">X. Li</style></author><author><style face="normal" font="default" size="100%">Liu, Y. H.</style></author><author><style face="normal" font="default" size="100%">Shang, D. J.</style></author><author><style face="normal" font="default" size="100%">Y.S. Wu</style></author><author><style face="normal" font="default" size="100%">L.M. Zeng</style></author><author><style face="normal" font="default" size="100%">Hu, M.</style></author><author><style face="normal" font="default" size="100%">S. Schmitt</style></author><author><style face="normal" font="default" size="100%">Kiendler-Scharr, A.</style></author><author><style face="normal" font="default" size="100%">Wahner, A.</style></author><author><style face="normal" font="default" size="100%">Zhang, Y. H.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Wintertime N2O5 uptake coefficients over the North China Plain</style></title><secondary-title><style face="normal" font="default" size="100%">Science Bulletin</style></secondary-title><alt-title><style face="normal" font="default" size="100%">Sci Bull</style></alt-title><short-title><style face="normal" font="default" size="100%">Sci BullSci Bull</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">aerosol</style></keyword><keyword><style  face="normal" font="default" size="100%">ammonium-sulfate</style></keyword><keyword><style  face="normal" font="default" size="100%">clno2</style></keyword><keyword><style  face="normal" font="default" size="100%">gaseous n2o5</style></keyword><keyword><style  face="normal" font="default" size="100%">heterogeneous hydrolysis</style></keyword><keyword><style  face="normal" font="default" size="100%">liquid phase-separation</style></keyword><keyword><style  face="normal" font="default" size="100%">n2o5 uptake coefficient</style></keyword><keyword><style  face="normal" font="default" size="100%">nighttime chemistry</style></keyword><keyword><style  face="normal" font="default" size="100%">nitrate</style></keyword><keyword><style  face="normal" font="default" size="100%">nitrate pollution</style></keyword><keyword><style  face="normal" font="default" size="100%">particle-phase</style></keyword><keyword><style  face="normal" font="default" size="100%">reactive uptake</style></keyword><keyword><style  face="normal" font="default" size="100%">residual layer</style></keyword><keyword><style  face="normal" font="default" size="100%">winter air pollution</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%">May 15</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">9</style></number><volume><style face="normal" font="default" size="100%">65</style></volume><pages><style face="normal" font="default" size="100%">765-774</style></pages><isbn><style face="normal" font="default" size="100%">2095-9273</style></isbn><language><style face="normal" font="default" size="100%">English</style></language><abstract><style face="normal" font="default" size="100%">The heterogeneous hydrolysis of dinitrogen pentoxide (N2O5) plays an important role in regulating NOx. The N2O5 uptake coefficient, c(N2O5), was determined using an iterative box model that was constrained to observational data obtained in suburban Beijing from February to March 2016. The box model determined 2289 individual c(N2O5) values that varied from &amp;lt;0.001 to 0.02 with an average value of 0.0046 +/- 0.0039 (and a median value of 0.0032). We found the derived winter c(N2O5) values in Beijing were relatively low as compared to values reported in previous field studies conducted during winter in Hong Kong (average value of 0.014) and the eastern U.S. coast (median value of 0.0143). In our study, field evidence of the suppression of c(N2O5) values due to pNO3 content, organics and the enhancement by aerosol liquid water content (ALWC) is in line with previous laboratory study results. Low ALWC, high pNO3 content, and particle morphology (inorganic core with an organic shell) accounted for the low c (N2O5) values in the North China Plain (NCP) during wintertime. The field-derived c(N2O5) values are well reproduced by a revised parameterization method, which includes the aerosol size distribution, ALWC, nitrate and organic coating, suggesting the feasibility of comprehensive parameterization in the NCP during wintertime. (C) 2020 Science China Press. Published by Elsevier B.V. and Science China Press. All rights reserved.</style></abstract><accession-num><style face="normal" font="default" size="100%">WOS:000528833400012</style></accession-num><notes><style face="normal" font="default" size="100%">&lt;p&gt;Lh5odTimes Cited:0Cited References Count:59&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 ChinaForschungszentrum Julich, Inst Energy &amp;amp;amp;amp; Climate Res, IEK 8 Troposphere, D-52428 Julich, GermanyChinese Acad Sci, Ctr Excellence Reg Atmospher Environm, Xiamen 361021, Peoples R ChinaTSI GmbH, D-52068 Aachen, Germany</style></auth-address></record></records></xml>