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Source receptor modeling of airborne particles collected over the Great Lakes.

机译:大湖上收集的空气传播颗粒的源受体模型。

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High-volume air samplers were used to collect aerosol samples on Whatman 41 air filters at the Canadian air sampling stations Burnt Island, Egbert and Point Petre. Once collected, the samples were analyzed for trace elements by neutron activation analysis. Air concentrations of over thirty trace elements were determined. A special focus was made to utilize Compton suppression gamma-ray spectroscopy and epithermal irradiations to enhance the detection limits of neutron activation analysis. These vanguard techniques allowed for the determination of trace elements at very low levels. Advancements were also made for the determination of Br through short-lived irradiations.; After the air concentrations were determined for trace elements from the neutron activation analysis data, the trends, sources and origin of the atmospheric aerosols were investigated. Exploration of the seasonal trends revealed that elements from a salt source like Na, Cl and Br were highest in the winter while elements originating from crustal weathering like Al, Ca and Si were highest in the summer. Many elements of anthropogenic origin demonstrated no seasonal trend. Enrichment factor analysis revealed elements from non-crustal sources including the elements Ag, As, Br, Cl, I, In, Sb, Se, Sn and Zn. Factor analysis exhibited trends that indicate oil and coal combustion, mining, incineration, and smelting as anthropogenic sources to aerosols of the rural Great Lakes. Potential source contribution function analysis indicated that many of the anthropogenic atmospheric pollutants in the Great Lakes originate from industrial centers in the eastern and southeastern United States. Study of the trace metal dry deposition into Lakes Huron and Ontario indicated that the majority of the total deposition resulted from crustal materials. However, dry deposition is a significant pathway for many toxic anthropogenic trace metals into the Great Lakes.
机译:在加拿大Burnt Island,Egbert和Point Petre空气采样站的Whatman 41空气过滤器上,使用了大容量空气采样器来收集气溶胶样品。一旦收集,就通过中子活化分析来分析样品中的痕量元素。测定了三十种以上微量元素的空气浓度。一个特别的重点是利用康普顿抑制伽马射线光谱和超热辐射来提高中子活化分析的检测极限。这些先进技术可用于测定极低含量的痕量元素。通过短期照射测定溴的方法也取得了进展。从中子活化分析数据确定空气中的微量元素浓度后,研究了大气气溶胶的趋势,来源和起源。对季节趋势的探索表明,盐分元素(如Na,Cl和Br)在冬季最高,而地壳气候元素(如Al,Ca和Si)则在夏季最高。人为起源的许多要素均未显示出季节性趋势。富集因子分析揭示了来自非壳来源的元素,包括元素Ag,As,Br,Cl,I,In,Sb,Se,Sn和Zn。因子分析显示出趋势,这些趋势表明石油和煤炭的燃烧,采矿,焚化和冶炼是农村大湖区气溶胶的人为来源。潜在的源贡献函数分析表明,五大湖中许多人为的大气污染物都来自美国东部和东南部的工业中心。对进入休伦湖和安大略省的痕量金属干沉积的研究表明,总沉积的大部分来自地壳物质。但是,干沉降是许多有毒的人为微量金属进入五大湖的重要途径。

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