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Enhanced modern carbon and biogenic organic tracers in Northeast Asian aerosols during spring/summer

机译:春季/夏季东北亚气溶胶中增强的现代碳和生物有机示踪剂

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To better understand the organic aerosol (OA) sources and formation processes in Northeast Asia, we studied atmospheric aerosol (total suspended particulate matter (TSP)) samples collected from Sapporo, northern Japan over 1 year period for the measurement of radiocarbon (~(14)C) in aerosol total carbon (TC) and water-soluble organic carbon (WSOC). We also measured various organic tracers and carbonaceous components: organic carbon (OC), WSOC, and elemental carbon (EC). We found that the percent modern carbon (pMC) in TC and WSOC increased during spring/summer with maximum (85% and 117%, respectively) in May. The temporal variations of pMC in WSOC and TC showed a good agreement with changes in the contributions of biogenic OA tracers to OC and WSOC. We also found that emissions of pollen in spring and fungal spores from soil in summer/autumn as well as secondary OA formation from biogenic VOCs (BVOCs) in summer/autumn are responsible for the enhanced pMC. Although emissions from biomass burning are significant in winter, enhanced fossil fuel combustion lowers the pMC in WSOC and TC. Throughout the year, modern carbon is more enriched in WSOC fraction than in TC, indicating that WSOC is more associated with biological activity. This study warrants a need to reconcile the atmospheric models, considering seasonal differences in BVOC emissions, particularly in temperate regions, in estimating secondary OA budget and its climatic impacts.
机译:为了更好地了解东北亚的有机气溶胶(OA)来源和形成过程,我们研究了在1年时间内从日本北部札幌收集的大气气溶胶(总悬浮颗粒物(TSP))样品,以测量放射性碳(〜(14 )C)中的气溶胶总碳(TC)和水溶性有机碳(WSOC)。我们还测量了各种有机示踪剂和碳质成分:有机碳(OC),WSOC和元素碳(EC)。我们发现春季和夏季,TC和WSOC中的现代碳百分比(pMC)有所增加,5月份最高(分别为85%和117%)。 WSOC和TC中pMC的时间变化与生物成因OA示踪剂对OC和WSOC的贡献变化显示出很好的一致性。我们还发现,夏季/秋季土壤中的春季花粉和真菌孢子排放以及夏季/秋季土壤中生物源性VOC(BVOC)的次生OA形成是造成pMC增强的原因。尽管冬季生物质燃烧的排放量很大,但增强化石燃料燃烧会降低WSOC和TC中的pMC。全年中,现代碳的WSOC含量要比TC富集得多,这表明WSOC与生物活性更加相关。这项研究保证有必要调和大气模型,考虑到BVOC排放的季节性差异,尤其是在温带地区,以便估算次要OA预算及其对气候的影响。

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