首页> 外文期刊>Atmospheric Chemistry and Physics Discussions >Source apportionment and dynamic changes of carbonaceous aerosols during the haze bloom-decay process in China based on radiocarbon and organic molecular tracers
【24h】

Source apportionment and dynamic changes of carbonaceous aerosols during the haze bloom-decay process in China based on radiocarbon and organic molecular tracers

机译:基于无线碳和有机分子示踪剂的中国雾霾盛开过程中碳质气溶胶源分摊和动态变化

获取原文
           

摘要

Fine carbonaceous aerosols (CAs) is the key factor influencing the currently filthy air in megacities in China, yet few studies simultaneously focus on the origins of different CAs species using specific and powerful source tracers. Here, we present a detailed source apportionment for various CAs fractions, including organic carbon (OC), water-soluble OC (WSOC), water-insoluble OC (WIOC), elemental carbon (EC) and secondary OC (SOC) in the largest cities of North (Beijing, BJ) and South China (Guangzhou, GZ), using the measurements of radiocarbon and anhydrosugars. Results show that non-fossil fuel sources such as biomass burning and biogenic emission make a significant contribution to the total CAs in Chinese megacities: 56?±?4 in BJ and 46?±?5?% in GZ, respectively. The relative contributions of primary fossil carbon from coal and liquid petroleum combustions, primary non-fossil carbon and secondary organic carbon (SOC) to total carbon are 19, 28 and 54?% in BJ, and 40, 15 and 46?% in GZ, respectively. Non-fossil fuel sources account for 52 in BJ and 71?% in GZ of SOC, respectively. These results suggest that biomass burning has a greater influence on regional particulate air pollution in North China than in South China. We observed an unabridged haze bloom-decay process in South China, which illustrates that both primary and secondary matter from fossil sources played a key role in the blooming phase of the pollution episode, while haze phase is predominantly driven by fossil-derived secondary organic matter and nitrate.
机译:细碳素气溶胶(CAS)是影响中国目前肮脏的空气的关键因素,但很少有几次研究使用特定和强大的源示踪剂同时关注不同CAS种类的起源。在这里,我们为各种CAS分数提供了详细的源分配,包括最大的有机碳(OC),水溶性OC(WIOC),水不溶性oc(WioC),水不溶性oc(WioC)和中学碳(EC)和中学北北(北京,BJ)和华南(广州,GZ)的城市使用RadioCarbon和Anhydrozars的测量。结果表明,生物量燃烧和生物发射等非化石燃料源对中国巨发的总CA产生了重大贡献:BJ和46°(46°(46)中分别为46±5?5?%。原发性化石碳来自煤和液体石油燃烧,初级非化石碳和二次有机碳(SoC)至总碳的相对贡献是BJ的19,28和54℃,40,15和46℃。 , 分别。非化石燃料源分别占BJ的52,分别在SOC的GZ中分别为71?%。这些结果表明生物量燃烧对华北地区颗粒状空气污染的影响而不是华南地区。我们观察到南方的一个未制造的阴霾绽放衰变过程,这表明来自化石源的初级和二次物质在污染发作的盛开阶段发挥了关键作用,而阴霾阶段主要由化石衍生的二次有机物驱动和硝酸盐。

著录项

获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号