Nelson Beth S, Bryant Daniel J, Alam Mohammed S, Sommariva Roberto, Bloss William J, Newland Mike J, Drysdale Will S, Vaughan Adam R, Acton W Joe F, Hewitt C Nicholas, Crilley Leigh R, Swift Stefan J, Edwards Pete M, Lewis Alastair C, Langford Ben, Nemitz Eiko, Gadi Ranu, Gurjar Bhola R, Heard Dwayne E, Whalley Lisa K, Şahin Ülkü A, Beddows David C S, Hopkins James R, Lee James D, Rickard Andrew R, Hamilton Jacqueline F
Wolfson Atmospheric Chemistry Laboratories, Department of Chemistry, University of York, Heslington, York YO10 5DD, U.K.
School of Biosciences, University of Nottingham, Sutton Bonington, Leicestershire LE12 5RD, U.K.
Environ Sci Technol Lett. 2023 May 3;10(6):520-527. doi: 10.1021/acs.estlett.3c00171. eCollection 2023 Jun 13.
Delhi, India, suffers from periods of very poor air quality, but little is known about the chemical production of secondary pollutants in this highly polluted environment. During the postmonsoon period in 2018, extremely high nighttime concentrations of NO (NO and NO) and volatile organic compounds (VOCs) were observed, with median NO mixing ratios of ∼200 ppbV (maximum of ∼700 ppbV). A detailed chemical box model constrained to a comprehensive suite of speciated VOC and NO measurements revealed very low nighttime concentrations of oxidants, NO, O, and OH, driven by high nighttime NO concentrations. This results in an atypical NO diel profile, not previously reported in other highly polluted urban environments, significantly perturbing nighttime radical oxidation chemistry. Low concentrations of oxidants and high nocturnal primary emissions coupled with a shallow boundary layer led to enhanced early morning photo-oxidation chemistry. This results in a temporal shift in peak O concentrations when compared to the premonsoon period (12:00 and 15:00 local time, respectively). This shift will likely have important implications on local air quality, and effective urban air quality management should consider the impacts of nighttime emission sources during the postmonsoon period.
印度德里空气质量极差的时期,但对于这个高度污染环境中二次污染物的化学生成情况却知之甚少。在2018年季风后期,观测到夜间一氧化氮(NO和NO)和挥发性有机化合物(VOCs)浓度极高,NO混合比中位数约为200 ppbV(最高约700 ppbV)。一个受一套全面的特定VOC和NO测量数据约束的详细化学箱模型显示,由于夜间NO浓度高,夜间氧化剂、NO、O和OH的浓度极低。这导致了一种非典型的NO日变化曲线,此前在其他高度污染的城市环境中未曾报道过,显著扰乱了夜间自由基氧化化学过程。低浓度的氧化剂和高夜间一次排放加上浅薄的边界层导致清晨光氧化化学过程增强。与季风前期相比,这导致了O浓度峰值的时间偏移(分别为当地时间12:00和15:00)。这种偏移可能会对当地空气质量产生重要影响,有效的城市空气质量管理应考虑季风后期夜间排放源的影响。