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[沈阳大气气溶胶中水溶性无机离子的特征]

[Characteristics of Water-soluble Inorganic Ions in Atmospheric Aerosols in Shenyang].

作者信息

Miao Hong-Yan, Wen Tian-Xue, Wang Lu, Xu Hui

机构信息

State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China.

China Meteorological Administration Training Center Liaoning Branch, Shenyang 110166, China.

出版信息

Huan Jing Ke Xue. 2016 Jun 8;37(6):2017-2024. doi: 10.13227/j.hjkx.2016.06.003.

Abstract

To investigate the levels and seasonal variation of water soluble inorganic components in ambient aerosol in Shenyang, 25 samples were collected with Andersen cascade sampler from Jun. 2012 to May. 2013 and nine water-soluble ions in samples were analyzed by IC. The different characteristics of aerosols between clean and pollution days in winter were discussed based on these samples. The results showed that the annual concentrations of total water soluble inorganic ions were 22.30 μg·m and 14.29 μg·m in fine and coarse particles, and SO and Ca were the most abundant ions, respectively. The ratio of mass concentration between SO and NO was 2.28 and the NH existed in the form of (NH)SO and NHNO in fine particles. The concentrations of total water soluble ions in fine particles were higher in winter and spring compared with those in summer and autumn, and they varied significantly between different seasons. The fossil fuel consumption led to the maximum values of secondary inorganic ions in fine particles during winter. The concentrations of total water soluble ions in coarse particles varied slightly though they were higher in autumn and lower in winter, and the wind-drifting sand was responsible for the higher concentration of Ca in autumn in coarse particles. The concentration of SO, NO, NH accounted for 80% of total water soluble inorganic ions during clean days and rose to 94% during pollution days. The ions were mostly concentrated in the size ranges of 0.43-0.65 μm and 0.43-2.1 μm respectively during clean and pollution days in fine mode. The peaks of SO, NO, NH in fine mode shifted from 0.43-0.65 μm to 1.1-2.1 μm, which meant these ions were transformed from condensing mode to droplets mode during pollution days. The air mass produced at Lake Baikal and transported through high altitude to the sampling point caused clean days, however the air mass transported through industrial areas might bring pollutions to the sampling point then caused pollution days.

摘要

为研究沈阳市大气气溶胶中水溶性无机成分的含量水平及季节变化特征,于2012年6月至2013年5月利用安德森分级采样器采集了25个样品,并采用离子色谱法分析了样品中的9种水溶性离子。基于这些样品讨论了冬季清洁日和污染日气溶胶的不同特征。结果表明,细颗粒和粗颗粒中水溶性无机离子的年平均浓度分别为22.30 μg·m³和14.29 μg·m³,其中SO₄²⁻和Ca²⁺分别是含量最高的离子。SO₄²⁻与NO₃⁻的质量浓度之比为2.28,细颗粒中NH₄⁺以(NH₄)₂SO₄和NH₄NO₃的形式存在。细颗粒中水溶性离子的总浓度在冬季和春季高于夏季和秋季,且不同季节间变化显著。冬季化石燃料燃烧导致细颗粒中二次无机离子浓度达到最大值。粗颗粒中水溶性离子的总浓度虽在秋季较高、冬季较低,但变化较小,秋季粗颗粒中较高的Ca²⁺浓度是由风沙造成的。清洁日期间,SO₄²⁻、NO₃⁻、NH₄⁺的浓度占水溶性无机离子总量的80%,污染日期间则升至94%。在细模态下,清洁日和污染日这些离子大多分别集中在0.43 - 0.65 μm和0.43 - 2.1 μm粒径范围内。细模态下SO₄²⁻、NO₃⁻、NH₄⁺的峰值从0.43 - 0.65 μm移至1.1 - 2.1 μm,这意味着污染日期间这些离子从凝结模态转变为液滴模态。贝加尔湖产生并经高空输送至采样点的气团导致了清洁日的出现,然而经工业区输送的气团可能给采样点带来污染从而导致污染日的出现。

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