The S3- ion is stable in geological fluids at elevated temperatures and pressures

Science

Volumn 331, Issue 6020, 2011, Pages 1052-1054

  Pokrovski, Gleb S ^a   Dubrovinsky, Leonid S ^b  

^a CNRS   (France)

^b UNIVERSITÄT BAYREUTH   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

GOLD; HYDROGEN SULFIDE; SULFATE; SULFIDE; SULFUR; TRISULFUR ION; UNCLASSIFIED DRUG;

AQUEOUS SOLUTION; GEOLOGICAL SURVEY; ISOTOPIC FRACTIONATION; METAMORPHIC FACIES; PRESSURE GRADIENT; RAMAN SPECTROSCOPY; SPECIATION (CHEMISTRY); SUBDUCTION ZONE; SULFUR; TEMPERATURE EFFECT;

ACIDITY; ARTICLE; ATMOSPHERIC PRESSURE; CHEMICAL REACTION; CHEMICAL STRUCTURE; COMPLEX FORMATION; FRACTIONATION; GEOCHEMISTRY; OXIDATION REDUCTION REACTION; PRIORITY JOURNAL; RAMAN SPECTROMETRY; SPECIES DIFFERENTIATION; TEMPERATURE SENSITIVITY; THERMOSTABILITY;

EID: 79952050236     PISSN: 00368075     EISSN: 10959203     Source Type: Journal    
DOI: 10.1126/science.1199911     Document Type: Article

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31. This work was supported by Institut National des Sciences de l'Univers-CNRS grants 3F, SOUMET, and CO2MET; a transnational access grant to the European High-Pressure Facility of Bayerisches Geoinstitut; and a Deutscher Akademischer Austausch Dienst-Partenariat Hubert Curien linkage grant PROCOPE. We thank L. Kison-Herzing, S. Linhardt, S. Übelhack, D. Krauße, and C. Cavaré-Hester for technical and logistical support and J. Schott, A. Borisova, N. Dubrovinskaia, Y. Shvarov, and H. Keppler for advice. The article benefited from comments of three anonymous reviewers.