Back to Search Start Over

Sulfur oxidation state and solubility in silicate melts.

Authors :
Boulliung, Julien
Wood, Bernard J.
Source :
Contributions to Mineralogy & Petrology; Aug2023, Vol. 178 Issue 8, p1-15, 15p
Publication Year :
2023

Abstract

We have determined the solubility of sulfur (S) as sulfide (S<superscript>2–</superscript>) for 13 different natural melt compositions at temperatures of 1473–1773 K under controlled conditions of oxygen and sulfur fugacities (fO<subscript>2</subscript> and fS<subscript>2</subscript>, respectively). The S and major element contents of the quenched glasses were determined by electron microprobe. The sulfide capacity parameter (C<subscript>S2–</subscript>) was used to express S<superscript>2–</superscript> solubility as a function of the oxygen and sulfur fugacities according to the equation: log C S 2 - = log S melt w t % + 0.5 log f O 2 f S 2 . 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 log C S 2 - = 0.225 + 25237 X FeO + 5214 X CaO + 12705 X MnO + 19829 X K 2 O - 1109 X S i 0.5 O - 8879 / T . X<subscript>MO</subscript> 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 (C<subscript>S6+</subscript>) 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 (S<superscript>6+</superscript>/S<superscript>2–</superscript> ratio) as a function of melt composition, temperature and oxygen fugacity. Results obtained are in good agreement with earlier measurements of S<superscript>6+</superscript>/S<superscript>2–</superscript> for basaltic and andesitic compositions. We observe a significant increase, however, relative to FMQ of the oxygen fugacity of the S<superscript>2–</superscript> to S<superscript>6+</superscript> 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 fO<subscript>2</subscript> 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. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
00107999
Volume :
178
Issue :
8
Database :
Complementary Index
Journal :
Contributions to Mineralogy & Petrology
Publication Type :
Academic Journal
Accession number :
170406076
Full Text :
https://doi.org/10.1007/s00410-023-02033-9