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Long-term air concentrations, wet deposition, and scavenging ratios of inorganic ions, HNO3, and SO2 and assessment of aerosol and precipitation acidity at Canadian rural locations

机译:加拿大农村地区的长期空气浓度,湿沉降和无机离子,HNO3和SO2的清除率以及气溶胶和沉淀酸度的评估

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摘要

This study analyzed long-term air concentrations and annual wetdeposition of inorganic ions and aerosol and precipitation acidity at 31 Canadian sites from 1983 to 2011. Scavenging ratios of inorganic ions andrelative contributions of particulate- and gas-phase species toNH, NO, and SO wet deposition weredetermined. Geographical patterns of atmospheric Ca, Na,Cl, NH, NO, and SO were similarto wet deposition and attributed to anthropogenic sources, sea-saltemissions, and agricultural emissions. Decreasing trends in atmosphericNH (1994–2010) and SO (1983–2010) were prevalent.Atmospheric NO increased prior to 2001 and then declinedafterwards. These results are consistent with SO, NO andNH emission trends in Canada and the USA. Widespread declines inannual NO and SO wet deposition ranged from0.07 to 1.0 kg ha a (1984–2011). Acidic aerosols andprecipitation impacted southern and eastern Canada more than western Canada;however, both trends have been decreasing since 1994. Scavenging ratios ofparticulate NH, SO and NO differedfrom literature values by 22 %, 44 %, and a factor of 6, respectively,because of the exclusion of gas scavenging in previous studies. Average gasand particle scavenging contributions to total wet deposition were estimatedto be 72 % for HNO and 28 % for particulate NO,37 % for SO and 63 % for particulate SO, and 30 %for NH and 70 % for particulate NH.
机译:这项研究分析了1983年至2011年加拿大31个站点的长期空气浓度和无机离子与气溶胶的年湿沉降和沉淀酸度。无机离子的清除率以及颗粒物和气相物类对NH,NO和SO湿润的相对贡献确定沉积。大气中Ca,Na,Cl,NH,NO和SO的地理分布与湿沉降相似,并归因于人为来源,海盐排放和农业排放。大气NH(1994–2010)和SO(1983–2010)呈下降趋势。2001年之前,大气NO呈上升趋势,然后呈下降趋势。这些结果与加拿大和美国的SO,NO和NH排放趋势一致。 NO和SO湿沉降的年平均下降幅度为0.07至1.0 kgkgha a(1984-2011)。酸性气溶胶和降水对加拿大南部和东部的影响大于加拿大西部;但是,这两种趋势自1994年以来一直呈下降趋势。NH,SO和NO颗粒的清除率与文献值相差22%,44%和6倍,因为在以前的研究中排除气体清除的原因。据估计,对总湿沉降的平均气体和颗粒清除率分别为:HNO为72%,颗粒NO为28%,SO为37%,SO为63%,NH为30%和NH为70%。

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  • 作者

    Cheng Irene; Zhang Leiming;

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  • 年度 2017
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  • 原文格式 PDF
  • 正文语种 eng
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