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Chemical Fingerprints for PM2.5 in the Ambient Air near a Raw Material Storage Site for Iron Ore, Coal, Limestone, and Sinter

机译:PM2.5的化学指纹在靠近铁矿石,煤炭,石灰石和烧结的原料储存部位附近的环境空气中的PM2.5

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To understand the contributions of a raw material storage site for iron ore, coal, limestone, and sinter to ambient air fine particulate matter (PM2.5), the concentrations and chemical fingerprints for resuspended and ambient air PM2.5 were compared. Investigations were done for 15 piles of raw materials, including 5 iron piles, 5 coal piles, 3 stone piles, and a single pile each for coke and sinter. Additionally, four sites, including A, B, C, and D, in the storage site surroundings were chosen to investigate the ambient air PM2.5 concentrations. The concentrations, compositions, and i and j values for PM2.5 varied significantly by season in the four sites under investigation. The chemical fingerprints of the PM2.5 showed that water-soluble ions were the most important component in all sites. Specifically, SO42– and NO3– were the predominant water-soluble ions in winter and summer, respectively. The most dominant components in the iron ore, coal, limestone, coke, and sinter piles were iron, carbon, Ca2+ and carbon, carbon and SO42–, and Fe and Ca2+, respectively. During the summer, PM2.5 concentrations ranged from 13.7–18.0 μg m–3, where the chemical composition of water-soluble ions, metals, carbon accounted for 54.2%, 5.7%, and 23.7% respectively. During winter, the concentrations ranged from 44.7–48.0 μg m–3, where the water-soluble ions, metals, carbon components accounted for 49.2%, 8.1%, and 17.4% respectively. From the chemical mass balance, the main sources of PM2.5 in sites B, C, and D were stationary sources, mobile sources, and secondary organic aerosols. To effectively address the air pollution threat associated with the surroundings of a raw material storage site, the environmental protection agency should formulate measures to effectively reduce the contribution of resuspended dust and other pollution sources to ambient air PM2.5.
机译:要了解铁矿石,煤,石灰石和烧结到环境空气细颗粒物质(PM2.5)的贡献,比较了重悬的浓度和化学指纹和环境空气PM2.5。为15堆原料进行调查,包括5个铁桩,5个煤桩,3个石头桩,每个用于焦炭和烧结的单一桩。另外,选择四个站点,包括A,B,C和D,在储存地点周围的环境中,以研究环境空气PM2.5浓度。 PM2.5的浓度,组合物和I和j值在调查下的四个地点季节在季节上变化显着变化。 PM2.5的化学指纹显示水溶性离子是所有位点中最重要的组分。具体而言,SO42和NO3分别是冬季和夏季的主要水溶性离子。铁矿石,煤,石灰石,焦炭和烧结桩中最占优势的成分分别是铁,碳,Ca2 +和碳,碳和SO 42-和Fe和Ca +。在夏季,PM2.5浓度范围为13.7-18.0μgm-3,其中水溶性离子,金属,碳的化学成分分别占54.2%,5.7%和23.7%。冬季,浓度范围为44.7-48.0μgm-3,其中水溶性离子,金属,碳成分分别占49.2%,8.1%和17.4%。从化学质量平衡中,B,C和D位点的PM2.5的主要来源是静止源,移动源和二级有机气溶胶。为了有效解决与原料储存地点的周围环境相关的空气污染威胁,环境保护署应制定措施,有效降低重建粉尘和其他污染源对环境空气PM2.5的贡献。

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