Artist's impression of the S3- molecule in a diamond anvil cell.
Sulfur is the sixth most abundant element on Earth and plays a key role in many geological and biological processes. A French-German team including CNRS1 and the Université Paul Sabatier has identified, on the basis of laboratory measurements, a novel form of sulfur present in geological fluids: the S3- ion. The discovery calls existing theories about the geological transport of sulfur into question, and could provide ways of identifying new deposits of precious metals such as gold and copper.
These findings are published in the Feb. 25, 2011 issue of the journal Science.
Until now, geochemists believed that inside Earth, only two forms of molecules contained sulfur: sulfides (based on H2S or S2-) and sulfates (based on H2SO4 or SO42-). Yet they had no way of directly plunging a probe into the hydrothermal fluids2 that flow through rocks to verify this theory. To get round this problem and test their hypothesis, the French-German team first created fluids similar to those in Earth's crust and mantle, i.e. aqueous solutions containing elementary sulfur (S) and thiosulfates (molecules containing the S2O32− ion). They then used a diamond anvil cell to bring the fluids to the temperatures and pressures found at depths of several kilometers (several hundred degrees and tens of thousands of atmospheres).
The researchers used an optical method known as Raman spectroscopy to identify the chemical species, and they were astounded to discover not two, but three forms of sulfur, the third being the trisulfur ion S3-. This was a double surprise: although S3- was already known to chemists (it is found in sulfur-containing silicate glass and ultramarine pigments for instance), it had never been observed in an aqueous solution.
The detection of S3- during these experiments means that sulfur must be considerably more mobile in hydrothermal fluids in Earth's crust than was previously thought. ...
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