Ery C. Hughes, Lee Saper, Philippa Liggins, Hugh St.C. O'Neill, Edward M. Stolper
{"title":"The sulfur solubility minimum and maximum in silicate melt","authors":"Ery C. Hughes, Lee Saper, Philippa Liggins, Hugh St.C. O'Neill, Edward M. Stolper","doi":"10.1144/jgs2021-125","DOIUrl":null,"url":null,"abstract":"The behaviour of sulfur in magmas is complex because it dissolves as both sulfide (S 2− ) and sulfate (S 6+ ) in silicate melt. Interesting aspects of the behaviour of sulfur are the solubility minimum (SS min ) and maxima (SS max ) observed with varying oxygen fugacity ( <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">O</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> ). We use a simple ternary model (silicate–S 2 –O 2 ) to explore the varying <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">O</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> paths where these phenomena occur. Both SS min and SS max occur when S 2− and S 6+ are present in the silicate melt in similar quantities owing to the differing solubility mechanisms of melt species containing these oxidation states of sulfur. At constant T , a minimum in dissolved total S content in vapour-saturated silicate melt ( <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msubsup> <mml:mi>w</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">S</mml:mi> </mml:mrow> <mml:mrow> <mml:mi mathvariant=\"normal\">T</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> <mml:mi>m</mml:mi> </mml:msubsup> </mml:math> ) occurs along paths of increasing <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">O</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> and either constant <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">S</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> or constant P . For paths on which <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msubsup> <mml:mi>w</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">S</mml:mi> </mml:mrow> <mml:mrow> <mml:mi mathvariant=\"normal\">T</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> <mml:mi>m</mml:mi> </mml:msubsup> </mml:math> is held constant with increasing <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">O</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> , the SS min is expressed as a maximum in P . The SS min occurs when the fraction of S 6+ in the melt ([S 6+ /S T ] m ) is 0.25 for constant <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">S</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> and [S 6+ /S T ] m <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:mo>≈</mml:mo> </mml:math> 0.75 for constant <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msubsup> <mml:mi>w</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">S</mml:mi> </mml:mrow> <mml:mrow> <mml:mi mathvariant=\"normal\">T</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> <mml:mi>m</mml:mi> </mml:msubsup> </mml:math> and P . A minimum in <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msubsup> <mml:mi>w</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">S</mml:mi> </mml:mrow> <mml:mrow> <mml:mi mathvariant=\"normal\">T</mml:mi> </mml:mrow> </mml:msub> </mml:mrow> <mml:mi>m</mml:mi> </mml:msubsup> </mml:math> is not encountered during closed- or open-system depressurization in the simple system we modelled. However, the SS min marks a change from reduction to oxidation during degassing. Various SS max occur when the silicate melt is multiply saturated with at least two phases: vapour, sulfide melt, and/or anhydrite. The SS min and SS max are potentially important features of magmatic process involving S, such as mantle melting, magma mixing, and degassing. These concepts influence calculations of the pressures of vapour-saturation, <mml:math xmlns:mml=\"http://www.w3.org/1998/Math/MathML\" overflow=\"scroll\"> <mml:msub> <mml:mi>f</mml:mi> <mml:mrow> <mml:msub> <mml:mrow> <mml:mi mathvariant=\"normal\">O</mml:mi> </mml:mrow> <mml:mn>2</mml:mn> </mml:msub> </mml:mrow> </mml:msub> </mml:math> , and SO 2 emissions using melt inclusions. Supplementary material: Additional information and data used to create the figures are available at https://doi.org/10.6084/m9.figshare.c.6274527 Thematic collection: This article is part of the Sulfur in the Earth system collection available at: https://www.lyellcollection.org/topic/collections/sulfur-in-the-earth-system","PeriodicalId":17320,"journal":{"name":"Journal of the Geological Society","volume":"24 1","pages":"0"},"PeriodicalIF":2.6000,"publicationDate":"2023-05-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"2","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of the Geological Society","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1144/jgs2021-125","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 2
Abstract
The behaviour of sulfur in magmas is complex because it dissolves as both sulfide (S 2− ) and sulfate (S 6+ ) in silicate melt. Interesting aspects of the behaviour of sulfur are the solubility minimum (SS min ) and maxima (SS max ) observed with varying oxygen fugacity ( fO2 ). We use a simple ternary model (silicate–S 2 –O 2 ) to explore the varying fO2 paths where these phenomena occur. Both SS min and SS max occur when S 2− and S 6+ are present in the silicate melt in similar quantities owing to the differing solubility mechanisms of melt species containing these oxidation states of sulfur. At constant T , a minimum in dissolved total S content in vapour-saturated silicate melt ( wSTm ) occurs along paths of increasing fO2 and either constant fS2 or constant P . For paths on which wSTm is held constant with increasing fO2 , the SS min is expressed as a maximum in P . The SS min occurs when the fraction of S 6+ in the melt ([S 6+ /S T ] m ) is 0.25 for constant fS2 and [S 6+ /S T ] m ≈ 0.75 for constant wSTm and P . A minimum in wSTm is not encountered during closed- or open-system depressurization in the simple system we modelled. However, the SS min marks a change from reduction to oxidation during degassing. Various SS max occur when the silicate melt is multiply saturated with at least two phases: vapour, sulfide melt, and/or anhydrite. The SS min and SS max are potentially important features of magmatic process involving S, such as mantle melting, magma mixing, and degassing. These concepts influence calculations of the pressures of vapour-saturation, fO2 , and SO 2 emissions using melt inclusions. Supplementary material: Additional information and data used to create the figures are available at https://doi.org/10.6084/m9.figshare.c.6274527 Thematic collection: This article is part of the Sulfur in the Earth system collection available at: https://www.lyellcollection.org/topic/collections/sulfur-in-the-earth-system
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Journal of the Geological Society (JGS) is owned and published by the Geological Society of London.
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