The enrichment of some metals (Al, Mg, Na, K, Cu, Zn, Cd) in volcanic gases is measured by an emanation coefficient, ex, relating the amount of the element x in lavas and in aerosol. Concerning the most volatile species, it appears that practically all the volcanic aerosol are produced by evaporation followed by gas-to-particle conversion and the spattered fraction appears to be negligible

Fractionation of metals in volcanic emissions

Pennisi M;
1988

Abstract

The enrichment of some metals (Al, Mg, Na, K, Cu, Zn, Cd) in volcanic gases is measured by an emanation coefficient, ex, relating the amount of the element x in lavas and in aerosol. Concerning the most volatile species, it appears that practically all the volcanic aerosol are produced by evaporation followed by gas-to-particle conversion and the spattered fraction appears to be negligible
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/219802
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