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Autor:
J. R. Salazar, B. T. Cartledge, J. P. Haynes, R. York-Marini, A. L. Robinson, G. T. Drozd, A. H. Goldstein, S. C. Fakra, B. J. Majestic
Publikováno v:
Atmospheric Chemistry and Physics, Vol 20, Pp 1849-1860 (2020)
Iron is the most abundant transition element in airborne particulate matter (PM), primarily existing as Fe(II) or Fe(III). Generally, the fraction of water-soluble iron is greater in urban areas compared to areas dominated by crustal emissions. To be
Externí odkaz:
https://doaj.org/article/bf9884f360ac4e9b960df46c7d7d73c9
