基于元素含量和锶同位素特征的堪萨斯州东北部大气沉淀中自然与人为污染物的区分

N. Clauer, S. Chaudhuri, I. Techer, R. Boutin
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摘要

本研究旨在通过分析主要污染物的元素和Sr同位素组成,确定并可能评估在堪萨斯州东北部康扎草原保护遗址附近收集的不同大气降水(雨、雪和冰雹)中主要污染物的变化。潜在的污染物,如当地的土壤和粘土材料,以及附近燃煤电厂的粉煤灰也进行了分析。与分析的沉淀中钾含量正相关,沉淀中的Na含量表明有肥料和/或天然植物有机物的供应。结合沉淀物的四种污染物,即土壤,粉煤灰,肥料和植物,可以评估它们在单一降水事件中的变化贡献。降雨事件的持续时间也监测了已确定污染物的变化贡献。稀土元素分布模式的变化证实了持续事件中沉淀87Sr/86Sr比值的变化。事实上,土壤矿物质在降水事件开始时起主要作用,并逐渐被工业粉煤灰所取代,而工业粉煤灰在降水事件结束时占主导地位,这取决于持续时间和风向。最后,通过元素贡献、稀土元素分布模式和87Sr/86Sr比值的变化可以识别出不同的污染物。它们在湿溶质中的变化可以被跟踪,但由于自然和人为贡献者之间的元素和同位素相互联系,无法提供严格的定量。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Distinction between Natural and Anthropogenic Contaminants of Atmospheric Precipitates from Northeastern Kansas Based on Their Elemental Contents and Strontium Isotopic Signatures
This study was designed to identify and possibly evaluate the changing occurrence of major pollutants in different atmospheric precipitates (rain, snow and hail) that were collected in northeastern Kansas next to the Konza Prairie Preservation site by analyzing their elemental and Sr isotope compositions. Potential pollutants like the local soils and their clay material, as well as the fly ash of a nearby coal-burning power plant were also analyzed. Positively correlated with K in the analyzed precipitates, the Na contents of the precipitates suggest a supply of fertilizers and/or natural plant organics. Combining the four identified pollutants of the precipitates that is to say the soils, the fly ash, the fertilizers and the plants allows evaluation of their changing contribution during a single precipitation event. The duration of the rain events monitors also the changing contribution of the identified pollutants. Variations of the 87Sr/86Sr ratio from precipitates during lasting events are confirmed by changing distribution patterns of the REEs. In fact, soil minerals contribute mostly at the beginning of the precipitation events and are replaced progressively by the industrial fly ash that becomes dominant towards the end of the precipitation events, depending on the duration and wind directions. At last not least, the different contaminants are recognizable by changing elemental contributions, REE distribution patterns and 87Sr/86Sr ratios. Their variable occurrence can be followed in the wet solutes, but a strict quantification cannot be provided due to elemental and isotopic interconnections between the natural and the anthropogenic contributors.
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