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Identification and characterization of individual airborne volcanic ash particles by Raman microspectroscopy

机译:通过拉曼光谱法鉴定和表征单个机载火山灰颗粒

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We present for the first time the Raman microspectroscopic identification and characterization of individual airborne volcanic ash (VA) particles. The particles were collected in April/May 2010 during research aircraft flights, which were performed by Deutsches Zentrum für Luft- und Raumfahrt in the airspace near the Eyjafjallaj?kull volcano eruption and over Europe (between Iceland and Southern Germany). In addition, aerosol particles were sampled by an Electrical Low Pressure Impactor in Munich, Germany. As references for the Raman analysis, we used the spectra of VA collected at the ground near the place of eruption, of mineral basaltic rock, and of different minerals from a database. We found significant differences in the spectra of VA and other aerosol particles (e.g., soot, nitrates, sulfates, and clay minerals), which allowed us to identify VA among other atmospheric particulate matter. Furthermore, while the airborne VA shows a characteristic Raman pattern (with broad band from ca. 200 to ca. 700 cm~(-1) typical for SiO_2 glasses and additional bands of ferric minerals), the differences between the spectra of aged and fresh particles were observed, suggesting differences in their chemical composition and/or structure. We also analyzed similarities between Eyjafjallaj?kull VA particles collected at different sampling sites and compared the particles with a large variety of glassy and crystalline minerals. This was done by applying cluster analysis, in order to get information on the composition and structure of volcanic ash. [Figure not available: see fulltext.]
机译:我们首次展示了单个机载火山灰(VA)颗粒的拉曼显微鉴定和表征。这些颗粒是在2010年4月/ 5月的研究飞机飞行中收集的,由德意志联邦航空与航天公司在德国埃亚菲亚德拉冰峰喷发附近的空域以及整个欧洲(冰岛与德国南部之间)进行。另外,气溶胶颗粒由德国慕尼黑的电子低压冲击器采样。作为拉曼分析的参考,我们使用了在火山爆发地点附近地面收集的VA光谱,矿物玄武岩以及数据库中不同矿物的光谱。我们发现VA和其他气溶胶颗粒(例如烟灰,硝酸盐,硫酸盐和粘土矿物)的光谱存在明显差异,这使我们能够在其他大气颗粒物中识别VA。此外,尽管机载VA显示出特征性的拉曼图案(SiO_2玻璃通常具有约200至约700 cm〜(-1)的宽带以及铁矿物质的附加带),但老化和新鲜光谱之间的差异观察到颗粒,表明它们的化学组成和/或结构不同。我们还分析了在不同采样点收集的艾亚菲亚德拉冰壶VA颗粒之间的相似性,并将这些颗粒与各种玻璃状和结晶性矿物进行了比较。这是通过应用聚类分析来完成的,以便获得有关火山灰成分和结构的信息。 [图不可用:请参见全文。]

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