<?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%">Tang, M. J.</style></author><author><style face="normal" font="default" size="100%">Huang, X.</style></author><author><style face="normal" font="default" size="100%">Lu, K. D.</style></author><author><style face="normal" font="default" size="100%">Ge, M. F.</style></author><author><style face="normal" font="default" size="100%">Li, Y. J.</style></author><author><style face="normal" font="default" size="100%">Cheng, P.</style></author><author><style face="normal" font="default" size="100%">T. Zhu</style></author><author><style face="normal" font="default" size="100%">Ding, A. J.</style></author><author><style face="normal" font="default" size="100%">Zhang, Y. H.</style></author><author><style face="normal" font="default" size="100%">Gligorovski, S.</style></author><author><style face="normal" font="default" size="100%">Song, W.</style></author><author><style face="normal" font="default" size="100%">X Ding</style></author><author><style face="normal" font="default" size="100%">Bi, X. H.</style></author><author><style face="normal" font="default" size="100%">XM Wang</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Heterogeneous reactions of mineral dust aerosol: implications for tropospheric oxidation capacity</style></title><secondary-title><style face="normal" font="default" size="100%">Atmospheric Chemistry and PhysicsAtmospheric Chemistry and PhysicsAtmospheric Chemistry and Physics</style></secondary-title><alt-title><style face="normal" font="default" size="100%">Atmos Chem Phys</style></alt-title><short-title><style face="normal" font="default" size="100%">Atmos Chem PhysAtmos Chem Phys</style></short-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">arizona test dust</style></keyword><keyword><style  face="normal" font="default" size="100%">calcium-carbonate particles</style></keyword><keyword><style  face="normal" font="default" size="100%">gas-particle interactions</style></keyword><keyword><style  face="normal" font="default" size="100%">gaseous-hydrogen peroxide</style></keyword><keyword><style  face="normal" font="default" size="100%">individual atmospheric particles</style></keyword><keyword><style  face="normal" font="default" size="100%">knudsen cell reactor</style></keyword><keyword><style  face="normal" font="default" size="100%">pearl river delta</style></keyword><keyword><style  face="normal" font="default" size="100%">phase diffusion-coefficients</style></keyword><keyword><style  face="normal" font="default" size="100%">total oh reactivity</style></keyword><keyword><style  face="normal" font="default" size="100%">volatile organic-compounds</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%">Oct 5</style></date></pub-dates></dates><number><style face="normal" font="default" size="100%">19</style></number><volume><style face="normal" font="default" size="100%">17</style></volume><pages><style face="normal" font="default" size="100%">11727-11777</style></pages><isbn><style face="normal" font="default" size="100%">1680-7316</style></isbn><language><style face="normal" font="default" size="100%">English</style></language><abstract><style face="normal" font="default" size="100%">Heterogeneous reactions of mineral dust aerosol with trace gases in the atmosphere could directly and indirectly affect tropospheric oxidation capacity, in addition to aerosol composition and physicochemical properties. In this article we provide a comprehensive and critical review of laboratory studies of heterogeneous uptake of OH, NO3, O-3, and their directly related species as well (including HO2, H2O2, HCHO, HONO, and N2O5) by mineral dust particles. The atmospheric importance of heterogeneous uptake as sinks for these species is assessed (i) by comparing their lifetimes with respect to heterogeneous reactions with mineral dust to lifetimes with respect to other major loss processes and (ii) by discussing relevant field and modeling studies. We have also outlined major open questions and challenges in laboratory studies of heterogeneous uptake by mineral dust and discussed research strategies to address them in order to better understand the effects of heterogeneous reactions with mineral dust on tropospheric oxidation capacity.</style></abstract><accession-num><style face="normal" font="default" size="100%">WOS:000412394100002</style></accession-num><notes><style face="normal" font="default" size="100%">Fj0jcTimes Cited:0Cited References Count:368</style></notes><auth-address><style face="normal" font="default" size="100%">Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou, Guangdong, Peoples R ChinaChinese Acad Sci, Guangzhou Inst Geochem, Guangdong Key Lab Environm Protect &amp; Resources Ut, Guangzhou, Guangdong, Peoples R ChinaNanjing Univ, Sch Atmospher Sci, Joint Int Res Lab Atmospher &amp; Earth Syst Sci JirL, Nanjing, Jiangsu, Peoples R ChinaPeking Univ, Coll Environm Sci &amp; Engn, State Key Joint Lab Environm Simulat &amp; Pollut Con, Beijing, Peoples R ChinaChinese Acad Sci, Inst Chem, State Key Lab Struct Chem Unstable &amp; Stable Speci, Beijing Natl Lab Mol Sci, Beijing, Peoples R ChinaUniv Macau, Fac Sci &amp; Technol, Dept Civil &amp; Environm Engn, Ave Univ, Taipa, Macau, Peoples R ChinaJinan Univ, Inst Mass Spectrometer &amp; Atmospher Environm, Guangzhou, Guangdong, Peoples R ChinaChinese Acad Sci, Inst Urban Environm, Ctr Excellence Reg Atmospher Environm, Xiamen 361021, Peoples R China</style></auth-address></record></records></xml>