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Aerosol characterization over the southeastern United States using high-resolution aerosol mass spectrometry: spatial and seasonal variation of aerosol composition and sources with a focus on organic nitrates

机译:使用高分辨率气溶胶质谱仪对美国东南部的气溶胶进行表征:以有机硝酸盐为重点的气溶胶成分和来源的时空变化

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摘要

We deployed a High-Resolution Time-of-Flight Aerosol Mass Spectrometer(HR-ToF-AMS) and an Aerosol Chemical Speciation Monitor (ACSM) tocharacterize the chemical composition of submicron non-refractory particulate matter(NR-PM$_{1}$) in the southeastern USA. Measurements were performed in bothrural and urban sites in the greater Atlanta area, Georgia (GA), andCentreville, Alabama (AL), for approximately 1 year as part ofSoutheastern Center for Air Pollution and Epidemiology study (SCAPE) andSouthern Oxidant and Aerosol Study (SOAS). Organic aerosol (OA) accounts formore than half of NR-PM mass concentration regardless of samplingsites and seasons. Positive matrix factorization (PMF) analysis ofHR-ToF-AMS measurements identified various OA sources, depending on locationand season. Hydrocarbon-like OA (HOA) and cooking OA (COA) have important,but not dominant, contributions to total OA in urban sites (i.e., 21–38 %of total OA depending on site and season). Biomass burning OA (BBOA)concentration shows a distinct seasonal variation with a larger enhancementin winter than summer. We find a good correlation between BBOA and browncarbon, indicating biomass burning is an important source for brown carbon,although an additional, unidentified brown carbon source is likely presentat the rural Yorkville site. Isoprene-derived OA factor (isoprene-OA) is onlydeconvolved in warmer months and contributes 18–36 % of total OA. Thepresence of isoprene-OA factor in urban sites is more likely from localproduction in the presence of NO than transport from rural sites.More-oxidized and less-oxidized oxygenated organic aerosol (MO-OOA andLO-OOA, respectively) are dominant fractions (47–79 %) of OA in all sites.MO-OOA correlates well with ozone in summer but not in winter, indicatingMO-OOA sources may vary with seasons. LO-OOA, which reaches a daily maximumat night, correlates better with estimated nitrate functionality fromorganic nitrates than total nitrates.Based on the HR-ToF-AMS measurements, we estimate that the nitratefunctionality from organic nitrates contributes 63–100 % to the totalmeasured nitrates in summer. Furthermore, the contribution of organic nitratesto total OA is estimated to be 5–12 % in summer, suggesting that organicnitrates are important components in the ambient aerosol in the southeasternUSA. The spatial distribution of OA is investigated by comparing simultaneousHR-ToF-AMS measurements with ACSM measurements at two different samplingsites. OA is found to be spatially homogeneous in summer due possibly tostagnant air mass and a dominant amount of regional secondary organicaerosol (SOA) in the southeastern USA. The homogeneity is less in winter,which is likely due to spatial variation of primary emissions.We observe that the seasonality of OA concentration shows a clearurban/rural contrast. While OA exhibits weak seasonal variation in the urbansites, its concentration is higher in summer than winter for rural sites.This observation from our year-long measurements is consistent with 14 yearsof organic carbon (OC) data from the SouthEastern Aerosol Research andCharacterization (SEARCH) network. The comparison between short-termmeasurements with advanced instruments and long-term measurements of basicair quality indicators not only tests the robustness of the short-termmeasurements but also provides insights in interpreting long-termmeasurements. We find that OA factors resolved from PMF analysis onHR-ToF-AMS measurements have distinctly different diurnal variations. Thecompensation of OA factors with different diurnal trends is one possiblereason for the repeatedly observed, relatively flat OA diurnal profile inthe southeastern USA. In addition, analysis of long-term measurements showsthat the correlation between OC and sulfate is substantially stronger insummer than winter. This seasonality could be partly due to the effects ofsulfate on isoprene SOA formation as revealed by the short-term intensivemeasurements.
机译:我们部署了高分辨飞行时间气溶胶质谱仪(HR-ToF-AMS)和气溶胶化学形态监测器(ACSM)来表征亚微米非难熔颗粒物的化学成分(NR-PM $ _ {1} $)在美国东南部。作为东南部空气污染和流行病学研究中心(SCAPE)和南部氧化剂和气溶胶研究中心(SOAS)的一部分,在佐治亚州大亚特兰大地区(GA)和阿拉巴马州中部维尔市(AL)的农村和城市站点中进行了大约1年的测量。 )。不论采样地点和季节如何,有机气溶胶(OA)占NR-PM质量浓度的一半以上。对HR-ToF-AMS测量结果进行正矩阵分解(PMF)分析,根据位置和季节确定了各种OA来源。类碳氢化合物(HOA)和蒸煮OA(COA)对城市场所的总OA有重要但不是主要的贡献(即占场所和季节的总OA的21–38%)。冬季比夏季,生物质燃烧OA(BBOA)的浓度表现出明显的季节性变化,冬季增强更大。我们发现BBOA与褐碳之间有良好的相关性,这表明生物质燃烧是褐碳的重要来源,尽管在约克维尔乡村地区可能还会出现其他未确定的褐碳来源。异戊二烯衍生的OA因子(异戊二烯OA)仅在较温暖的月份解卷积,占总OA的18–36%。在没有NO的情况下,城市生产中异戊二烯-OA因子的存在更有可能来自农村地区,而不是农村地区的运输。高氧化和低氧化的含氧有机气溶胶(分别为MO-OOA和LO-OOA)是主要成分(47所有地点的OA中约有–79%。MO-OOA与臭氧的相关性很好,但在冬季却不然,这表明MO-OOA的来源可能随季节而变化。 LO-OOA每天晚上都达到最大值,与有机硝酸盐估计的硝酸盐官能度比总硝酸盐更好地相关。基于HR-ToF-AMS测量,我们估计有机硝酸盐的硝酸盐官能度对总硝酸盐的贡献为63-100%在夏天。此外,夏季估计有机硝酸盐对总OA的贡献为5-12%,这表明有机硝酸盐是美国东南部环境气溶胶中的重要成分。通过比较同时在两个不同采样点进行的HR-ToF-AMS测量与ACSM测量来研究OA的空间分布。发现OA在夏季在空间上是均匀的,这可能是由于美国东南部的空气质量停滞和主要的区域性次级有机气溶胶(SOA)含量。冬季的均一性较低,这很可能是由于一次排放的空间变化所致。我们观察到,OA浓度的季节性呈现出明显的城乡对比。虽然OA在城市地区表现出较弱的季节性变化,但农村地区的夏季浓度高于冬季,这与我们一年来的观测结果一致,与东南气溶胶研究和表征(SEARCH)的14年有机碳(OC)数据一致网络。使用高级仪器进行的短期测量与基本空气质量指标的长期测量之间的比较,不仅测试了短期测量的鲁棒性,而且还为解释长期测量提供了见识。我们发现,从PMF分析得出的HR-ToF-AMS测量结果得出的OA因素具有明显不同的昼夜变化。在美国东南部反复观察到的相对平坦的OA昼夜剖​​面时,具有不同昼夜趋势的OA因子补偿是一种可能的原因。此外,对长期测量值的分析表明,夏季的OC和硫酸盐之间的相关性强于冬季。这种短期变化可能部分是由于短期密集测量所揭示的,硫酸盐对异戊二烯SOA形成的影响。

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