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Sulfur oxidation state and solubility in silicate melts
by
Wood, Bernard J
, Boulliung, Julien
in
Composition
/ Controlled conditions
/ Degassing
/ Electron probes
/ Fugacity
/ Lava
/ Magma
/ Melts
/ Mineralogy
/ Oxidation
/ Oxygen
/ Petrology
/ Silicates
/ Solubility
/ Sulfides
/ Sulfur
/ Sulphides
/ Sulphur
/ Temperature
/ Valence
2023
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Sulfur oxidation state and solubility in silicate melts
by
Wood, Bernard J
, Boulliung, Julien
in
Composition
/ Controlled conditions
/ Degassing
/ Electron probes
/ Fugacity
/ Lava
/ Magma
/ Melts
/ Mineralogy
/ Oxidation
/ Oxygen
/ Petrology
/ Silicates
/ Solubility
/ Sulfides
/ Sulfur
/ Sulphides
/ Sulphur
/ Temperature
/ Valence
2023
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Sulfur oxidation state and solubility in silicate melts
by
Wood, Bernard J
, Boulliung, Julien
in
Composition
/ Controlled conditions
/ Degassing
/ Electron probes
/ Fugacity
/ Lava
/ Magma
/ Melts
/ Mineralogy
/ Oxidation
/ Oxygen
/ Petrology
/ Silicates
/ Solubility
/ Sulfides
/ Sulfur
/ Sulphides
/ Sulphur
/ Temperature
/ Valence
2023
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Journal Article
Sulfur oxidation state and solubility in silicate melts
2023
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Overview
We have determined the solubility of sulfur (S) as sulfide (S2–) for 13 different natural melt compositions at temperatures of 1473–1773 K under controlled conditions of oxygen and sulfur fugacities (fO2 and fS2, respectively). The S and major element contents of the quenched glasses were determined by electron microprobe. The sulfide capacity parameter (CS2–) was used to express S2– solubility as a function of the oxygen and sulfur fugacities according to the equation: logCS2-=logSmeltwt%+0.5logfO2fS2. Sulfide capacities of silicate melts were found to increase with temperature and the FeO content of the melt. We combined our sulfide data at 1473–1773 K with (O’Neill and Mavrogenes, J Petrol 43:1049–1087, 2002) results at 1673 K, and obtained by stepwise linear regression the following equation for sulfide capacity logCS2-=0.225+25237XFeO+5214XCaO+12705XMnO+19829XK2O-1109XSi0.5O-8879/T. XMO is the mole fraction of the oxide of M on a single-oxygen basis, and T is in Kelvin. The sulfide capacity equation was combined with sulfate capacity (CS6+) data for similar compositions and at the same temperatures (Boulliung and Wood, Geochim Cosmochim Acta 336:150–164, 2022), to estimate the S redox state (S6+/S2– ratio) as a function of melt composition, temperature and oxygen fugacity. Results obtained are in good agreement with earlier measurements of S6+/S2– for basaltic and andesitic compositions. We observe a significant increase, however, relative to FMQ of the oxygen fugacity of the S2– to S6+ transition as temperature is lowered from 1773 to 1473 K. We used our results to simulate sulfur-degassing paths for basaltic compositions under various redox conditions (FMQ –2 log fO2 units to FMQ + 2). The calculations indicate that, given an initial concentration of 0.12 wt% S in an ascending melt at 250 MPa, most of the S (> 80%) will be degassed before the magma reaches 100 MPa pressure.
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