Chemical and microstructural characterization of ash from the Ubinas and Sabancaya volcanoes in Peru

Abstract In this study, volcanic ash from Ubinas and Sabancaya volcanoes in Peru were characterized by particle size, scanning electron microscopy coupled with energy dispersive X-ray spectrometry (SEM/EDX), ICP MASS spectrometer, X-ray diffraction and specific gravity. The combined application of those techniques for the analysis provided complementary information, i.e., their elemental compositions and morphology. The results showed that the volcanic ashes (VA) have a particle size lower than 600 μm with a dominant size over 100 μm. Their mineralogical characteristics involve silica polymorp... Mehr ...

Verfasser: Tupayachy-Quispe, Danny
Apaza, Fredy
Churata, Rossibel
Almirón, Jonathan
Hermoza-Gutiérrez, Marián
Velasco, Francisco
Torres-Carrasco, Manuel
Dokumenttyp: Artikel
Erscheinungsdatum: 2021
Reihe/Periodikum: IOP Conference Series: Materials Science and Engineering ; volume 1150, issue 1, page 012010 ; ISSN 1757-8981 1757-899X
Verlag/Hrsg.: IOP Publishing
Sprache: unknown
Permalink: https://search.fid-benelux.de/Record/base-26890650
Datenquelle: BASE; Originalkatalog
Powered By: BASE
Link(s) : http://dx.doi.org/10.1088/1757-899x/1150/1/012010

Abstract In this study, volcanic ash from Ubinas and Sabancaya volcanoes in Peru were characterized by particle size, scanning electron microscopy coupled with energy dispersive X-ray spectrometry (SEM/EDX), ICP MASS spectrometer, X-ray diffraction and specific gravity. The combined application of those techniques for the analysis provided complementary information, i.e., their elemental compositions and morphology. The results showed that the volcanic ashes (VA) have a particle size lower than 600 μm with a dominant size over 100 μm. Their mineralogical characteristics involve silica polymorphs, vitreous nature of silica and silicate particles, showing chemical heterogeneity within the micrometer sized particles and diverse morphology. The chemical composition of the ash is mainly SiO 2 , Al 2 O 3 , Na 2 O and CaO, with a high content of silica ranging from 57.78 to 66.14% and alumina ranges from 13.81 to 17.56%. The concentration of potential pollutant elements determined in products from Ubinas and Sabancaya volcanoes, namely As, Ba, Co, Cr, Cs, Fe, K, Mn, Mo, Sb, Sc, Sr, Th, Ti, U, V, and Zn, are reported. The different mineralogical characteristics among the studied volcanic samples would be related to their association with different volcanic eruptions. The chemical compositions and microstructure indicate that ashes have an origin and formation of andesitic and dacitic type.