کد مقاله کد نشریه سال انتشار مقاله انگلیسی نسخه تمام متن
4699343 1637640 2012 18 صفحه PDF دانلود رایگان
عنوان انگلیسی مقاله ISI
The dissolution mechanism of sulphur in hydrous silicate melts. II: Solubility and speciation of sulphur in hydrous silicate melts as a function of fO2
موضوعات مرتبط
مهندسی و علوم پایه علوم زمین و سیارات ژئوشیمی و پترولوژی
پیش نمایش صفحه اول مقاله
The dissolution mechanism of sulphur in hydrous silicate melts. II: Solubility and speciation of sulphur in hydrous silicate melts as a function of fO2
چکیده انگلیسی

Raman and X-ray absorption spectroscopy (XANES) measurements on a series of experimentally synthesised, sulphur (S)-bearing, hydrous silicate glasses were used to determine the S-speciation and S-oxidation state as a function of glass composition and oxygen fugacity (fO2) and to decipher the dissolution mechanism of S in silicate melts. Synthesised glasses include soda-lime (SLG), K2Si4O9 (KSG), albite and trondhjemite (TROND) compositions. A series of SLG and KSG glasses, doped with small quantities of Fe, was also studied in order to determine the effect of Fe/S on the S solubility. The experiments were performed in internally heated (IHPV) and cold seal (CSPV) pressure vessels at 200 MPa, 1000 and 850 °C and a range of fO2 from log fO2 = QFM − 2.35 to QFM + 4 (QFM is quartz–fayalite–magnetite oxygen buffer).The systematic correlation of features in Raman and XANES spectra allows the identification of at least four different S-species in the glasses depending on fO2 and Fe/S of the system. In XANES spectra of Fe-free glasses SH−, H2S and SO42 − are visible as peaks at 2466, 2471.8 and 2482 eV, respectively. In Raman spectra peaks at 2574 and 990 cm− 1 indicate the presence of HS bonds and SO42 −, respectively, but SH− and H2S can not be distinguished using a Raman spectroscopy. In Fe-bearing glasses FeS bonding is identified at 2469 eV in the case of XANES and at 298, 372 and 420 cm− 1 in the case of Raman spectra. The intensities of peaks related to SH bonding systematically decrease and the intensities of peaks related to FeS bonding systematically increase with increasing Fe/S in both the XANES and the Raman spectra indicating that in the presence of Fe, FeS bonding is preferred over SH bonding. The total S solubility at sulphur saturation in the Fe-free melts is a function of the degree of melt polymerisation and it increases with increasing NBO/T (from 0.03 to 1.91 wt.% S). The S2 − species are more soluble than the S6 + species in contrast to previously studied Fe-bearing “natural” compositions.The change from S2 − to S6 + is observed at log fO2 = QFM − 1 to QFM + 1 which is ~ 1.5 log unit lower than the range of fO2 previously reported for Fe-rich compositions indicating that Fe influences not only the speciation but also the oxidation state of S in silicate melts at given redox conditions. The natural implications are that S6 + in Fe-poor magmas can be stable at lower fO2 than previously predicted and, hence, S6 + may act as an oxidising agent in the mantle wedge by successively oxidising Fe2 + to Fe3 + via the reaction H2SO4 + 9FeO = FeS + 4Fe2O3 + H2O. For the silicate melt generated in the mantle wedge and containing about 10 wt.% total FeO, the change in the Fe3 +/ΣFe ratio from 0.1 to 0.2 will correspond to an increase in the log fO2 from QFM − 0.5 to QFM + 1.5 and will require only 1000–3000 ppm S extracted from subducted slab.


► We have determined S dissolution mechanism in silicate melts.
► In Fe-free melts the S6 +/S2 − equilibrium is at lower fO2 than in natural melts.
► In Fe-free systems S2 − is more soluble than S6 +.
► S6 + may act as an oxidising agent in arc mantle.

ناشر
Database: Elsevier - ScienceDirect (ساینس دایرکت)
Journal: Chemical Geology - Volumes 322–323, 5 September 2012, Pages 250–267
نویسندگان
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