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Pollution characteristics and source difference of gaseous elemental mercury between haze and non-haze days in winter

机译:冬季阴霾日与非阴霾日之间气态元素汞的污染特征及来源差异

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摘要

The distribution characteristics and sources of gaseous elemental mercury (GEM) on haze and non-haze days are still not clear. During the winter heating period in 2017, the GEM concentrations in Qingdao were studied for their differences, sources, and pollution characteristics on haze and non-haze days. The GEM concentration on haze days (2.81 +/- 2.23 ng/m(3)) was higher than that on non-haze days (1.90 +/- 121 ng/m(3)) and the difference was significant (p 0.01) during the period of artificial heating. The average concentration of GEM was 2.27 ng/m(3) in the heating period, but lower than that before heating (3.30 ng/m(3)). However, the mercury to carbon monoxide ratio (GEM/CO) on haze days was lower than that on non-haze days. The ratio of GEM/CO in this study was lower than that in other studies reported from China. There was a positive correlation between the GEM/CO ratio and the air temperature (p 0.01), suggesting that the mercury released from the Earth's surface was important. The environmental policies of China also contributed to decrease of the GEM/CO ratio. Similar diurnal patterns appeared on both haze and non-haze days, with one GEM peak at 14:00-15:00. This pattern was different from the bimodal pattern of other atmospheric pollutants in the morning and evening rush hours and was controlled by GEM from the Earth's surface (mostly re-emission of legacy Hg) whether on haze or non-haze days. Principal component analysis showed that the contribution of GEM directly from anthropogenic sources was relatively small. The main influencing factor on haze days was air temperature. GEM concentrations showed large spatial differences in air masses from different places. The GEM concentration in air masses from southern and the western Shandong Province was higher than from the north on haze days. (C) 2019 Elsevier B.V. All rights reserved.
机译:雾天和非雾天的气态元素汞(GEM)的分布特征和来源仍不清楚。在2017年冬季取暖期间,研究了青岛市GEM浓度的差异,来源和霾天和非霾天的污染特征。霾日的GEM浓度(2.81 +/- 2.23 ng / m(3))高于非霾日的GEM浓度(1.90 +/- 121 ng / m(3)),差异显着(p <0.01 )在人工加热期间。加热期间GEM的平均浓度为2.27 ng / m(3),但低于加热前的平均浓度(3.30 ng / m(3))。然而,雾霾天的汞与一氧化碳之比(GEM / CO)低于非雾霾天。在这项研究中,GEM / CO的比率低于中国报道的其他研究。 GEM / CO比与气温之间存在正相关关系(p <0.01),这表明从地球表面释放的汞很重要。中国的环境政策也导致了GEM / CO比率的下降。在阴霾天和非阴霾天都出现类似的昼夜模式,在14:00-15:00出现一个GEM高峰。这种模式不同于早晨和傍晚高峰时间其他大气污染物的双峰模式,并且无论是在霾天还是非霾天,都是由GEM从地球表面控制的(主要是遗留的汞再排放)。主成分分析表明,人为因素直接对创业板的贡献相对较小。雾霾天的主要影响因素是气温。 GEM浓度显示来自不同地方的空气质量存在较大的空间差异。烟霾天,山东南部和西部的空气质量中的GEM浓度高于北部。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第15期|671-680|共10页
  • 作者单位

    Ocean Univ China, Minist Educ, Key Lab Marine Environm Sci & Ecol, Qingdao 266100, Shandong, Peoples R China|Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Shandong, Peoples R China;

    Ocean Univ China, Minist Educ, Key Lab Marine Environm Sci & Ecol, Qingdao 266100, Shandong, Peoples R China|Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Shandong, Peoples R China;

    Ocean Univ China, Minist Educ, Key Lab Marine Environm Sci & Ecol, Qingdao 266100, Shandong, Peoples R China|Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Shandong, Peoples R China;

    Ocean Univ China, Minist Educ, Key Lab Marine Environm Sci & Ecol, Qingdao 266100, Shandong, Peoples R China|Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Shandong, Peoples R China;

    Qingdao Environm Monitoring Ctr, Qingdao 266000, Shandong, Peoples R China;

    Ocean Univ China, Minist Educ, Key Lab Marine Environm Sci & Ecol, Qingdao 266100, Shandong, Peoples R China|Ocean Univ China, Coll Environm Sci & Engn, Qingdao 266100, Shandong, Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Gaseous elemental mercury; Heating period; Source; Air mass; Haze days; GEM/CO;

    机译:气态元素汞加热时间来源空气质量阴霾天GEM / CO;

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