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首页> 外文期刊>Environmental Pollution >Characterization of dicarboxylic acids, oxoacids, and α-dicarbonyls in PM2.5 within the urban boundary layer in southern China: Sources and formation pathways
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Characterization of dicarboxylic acids, oxoacids, and α-dicarbonyls in PM2.5 within the urban boundary layer in southern China: Sources and formation pathways

机译:中国南部城市边界层中PM2.5中二羧酸,氧代酸和α-二羰基的表征:来源和地层途径

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摘要

Low-molecular-weight dicarboxylic acids, which are important components of secondary organic aerosols, have been extensively studied in recent years. Many studies have focused on ground-level observations and literature reports on the vertical distribution of the organic aerosols within the urban boundary layer are limited. In this study, the vertical profiles of dicarboxylic acids and related organic compounds (DCRCs) in PM2.5 were investigated at altitudinal levels (ground level and 488 m above the ground level) at the Canton Tower in Guangzhou, southern China, to elucidate their primary sources and secondary formation processes. The concentrations of DCRCs at ground level were generally higher than those at 488 m. Oxalic acid (C-2) was the most abundant species, followed by succinic acid (C-4) and malonic acid (C-3) at both heights. The higher ratio of DCRCs-bound carbon to organic carbon (i.e., DCRCsC/OC) at 488 m (4.8 +/- 1.2%) relative to that at ground level (2.7 +/- 0.5%) indicated a higher degree of aerosol aging at 488 m. The abundance of C-2 was increased and the conversion of C-4 to C-3 was enhanced due to the photochemical oxidation of its homologues during long-range transport periods. The increase in C-2 was associated with in-cloud processes during pollution periods. Principal component analysis showed that DCRCs were mainly derived from atmospheric secondary processing and biomass burning was also an important source of long-chain carboxylic acids during autumn in Guangzhou. Our results illustrate that secondary processing and biomass burning play prominent roles in controlling the abundance of DCRCs. Furthermore, DCRCs are affected by air masses from regional areas, oxidation of their precursors via vertical transport and in-cloud processes. (C) 2021 Elsevier Ltd. All rights reserved.
机译:近年来,是二次有机气溶胶的重要组成部分的低分子量二羧酸已被广泛研究。许多研究专注于地面级别观察和文献报告,了城市边界层有机气溶胶的垂直分布是有限的。在该研究中,在广州南方广州广州广州塔的大陆水平(地面和地面488米以上的地面和488米以上)来研究二羧酸和相关有机化合物(DCRC)的垂直曲线,以阐明他们的主要来源和二级形成过程。地面水平的DCRC浓度通常高于488米的浓度。草酸(C-2)是最丰富的物种,其次在两个高度下是琥珀酸(C-4)和丙酸(C-3)。相对于地面水平(2.7 +/- 0.5%)的488 m(4.8 +/- 1.2%)的DCRCS-结合的碳与有机碳(即,DCRCSC / OC)的比例较高,表明了较高程度的气溶胶老化在488米处。由于在远程运输期间其同源物的光化学氧化,C-2的丰度增加了C-4至C-3的转化。 C-2的增加与污染期间的云内过程有关。主要成分分析表明,DCRC主要来自大气二次加工,生物量燃烧也是广州秋季长链羧酸的重要来源。我们的结果说明了二次处理和生物量燃烧在控制DCRC的丰富方面发挥着突出的作用。此外,DCRCS受到区域区域的气体影响,通过垂直运输和云流程氧化它们的前体。 (c)2021 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2021年第9期|117185.1-117185.12|共12页
  • 作者单位

    Jinan Univ Inst Environm & Climate Res Guangzhou 511443 Peoples R China|Guangdong Hongkong Macau Joint Lab Collaborat Inn Guangzhou 511443 Peoples R China;

    Sun Yat Sen Univ Sch Atmospher Sci Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Key Lab Climate Change & Nat Disas Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Field Observat & Res Stn Climate E Guangzhou 510275 Peoples R China|Southern Marine Sci & Engn Guangdong Lab Zhuhai Zhuhai 519082 Peoples R China;

    Tianjin Univ Sch Earth Syst Sci Inst Surface Earth Syst Sci Tianjin 300072 Peoples R China;

    Chubu Univ Chubu Inst Adv Studies Kasugai Aichi 4878501 Japan;

    Chinese Acad Sci Inst Atmospher Phys State Key Lab Atmospher Boundary Layer Phys & Atm Beijing 100029 Peoples R China;

    Jinan Univ Inst Environm & Climate Res Guangzhou 511443 Peoples R China|Guangdong Hongkong Macau Joint Lab Collaborat Inn Guangzhou 511443 Peoples R China;

    Jinan Univ Inst Environm & Climate Res Guangzhou 511443 Peoples R China|Guangdong Hongkong Macau Joint Lab Collaborat Inn Guangzhou 511443 Peoples R China;

    Jinan Univ Inst Environm & Climate Res Guangzhou 511443 Peoples R China|Guangdong Hongkong Macau Joint Lab Collaborat Inn Guangzhou 511443 Peoples R China;

    Jinan Univ Inst Environm & Climate Res Guangzhou 511443 Peoples R China|Guangdong Hongkong Macau Joint Lab Collaborat Inn Guangzhou 511443 Peoples R China;

    Sun Yat Sen Univ Sch Atmospher Sci Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Key Lab Climate Change & Nat Disas Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Field Observat & Res Stn Climate E Guangzhou 510275 Peoples R China|Southern Marine Sci & Engn Guangdong Lab Zhuhai Zhuhai 519082 Peoples R China;

    Sun Yat Sen Univ Sch Atmospher Sci Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Key Lab Climate Change & Nat Disas Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Field Observat & Res Stn Climate E Guangzhou 510275 Peoples R China|Southern Marine Sci & Engn Guangdong Lab Zhuhai Zhuhai 519082 Peoples R China;

    Sun Yat Sen Univ Sch Atmospher Sci Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Key Lab Climate Change & Nat Disas Guangzhou 510275 Peoples R China|Sun Yat Sen Univ Guangdong Prov Field Observat & Res Stn Climate E Guangzhou 510275 Peoples R China|Southern Marine Sci & Engn Guangdong Lab Zhuhai Zhuhai 519082 Peoples R China;

    Guangzhou Environm Monitoring Ctr Guangzhou 510030 Peoples R China;

    Guangzhou Environm Monitoring Ctr Guangzhou 510030 Peoples R China;

    Tianjin Univ Sch Earth Syst Sci Inst Surface Earth Syst Sci Tianjin 300072 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Vertical distribution; Organic aerosol; Dicarboxylic acids; Photochemical oxidation; In-cloud process; Sources;

    机译:垂直分布;有机气溶胶;二羧酸;光化学氧化;云流程;来源;

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