How does the hot core of a volcanic plume control the sulfur speciation in volcanic emission?

Geochemistry, Geophysics, Geosystems

Volumn 13, Issue 7, 2012, Pages

  Hoshyaripour, G ^a   Hort, M ^a   Langmann, B ^a  

^a UNIVERSITY OF HAMBURG   (Germany)

Author keywords

Explosive volcanism; Geochemical modeling; Thermodynamics; Volcanic gases

Indexed keywords

MIRRORS; OXIDATION; SULFUR; SULFUR DIOXIDE; TECTONICS; THERMODYNAMICS;

AMBIENT AIR; BOX MODELS; EXPLOSIVE VOLCANISM; GEOCHEMICAL MODELING; HOT SPOT; INITIAL OXIDATION; OXIDATION STATE; PLINIAN; SOURCE CONDITIONS; SULFUR SPECIATION; TECTONIC SETTINGS; TEMPERATURE RANGE; THERMODYNAMIC EQUILIBRIA; VOLCANIC CLOUDS; VOLCANIC EMISSION; VOLCANIC ERUPTIONS; VOLCANIC GAS; VOLCANIC PLUME; VOLCANIC SETTINGS;

VOLCANOES;

ATMOSPHERIC PLUME; CHEMICAL COMPOSITION; GEOCHEMISTRY; MAGMA; OXIDATION; SPECIATION (CHEMISTRY); SULFUR; TEMPERATURE; THERMODYNAMICS; VOLCANIC CLOUD; VOLCANIC ERUPTION; VOLCANIC GAS;

PLINIA;

EID: 84864046446     PISSN: None     EISSN: 15252027     Source Type: Journal    
DOI: 10.1029/2011GC004020     Document Type: Article

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