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Evidence of the existence of the As.sub.4S.sub.6 molecule produced by light exposure of alacranite, As.sub.8S.sub.9

The As.sub.4 S.sub.6 molecule, although theoretically predicted and supposed to occur in amorphous arsenic sulfides, was missing in the reported structures of crystalline As chalcogenides; the thermodynamic stable phase for this stoichiometry, in fact, is that of the mineral orpiment, which shows a...

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Published in:European journal of mineralogy (Stuttgart) 2024-08, Vol.36 (4), p.615
Main Authors: Bindi, Luca, Bonazzi, Paola, Chelazzi, Laura, Franceschini, Matteo M. N, Lepore, Giovanni O, Morana, Marta, Pratesi, Giovanni, Taddei, Alice, Zoppi, Matteo, Menchetti, Silvio
Format: Article
Language:English
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Summary:The As.sub.4 S.sub.6 molecule, although theoretically predicted and supposed to occur in amorphous arsenic sulfides, was missing in the reported structures of crystalline As chalcogenides; the thermodynamic stable phase for this stoichiometry, in fact, is that of the mineral orpiment, which shows a layered structural arrangement based on trigonal AsS.sub.3 pyramids. Here we report the first possible occurrence of the As.sub.4 S.sub.6 molecule together with the other known As.sub.4 S.sub.n (n=3, 4, 5) molecules randomly replacing each other in the crystalline structure of a new monoclinic product obtained by the light-induced alteration of the mineral alacranite, As.sub.8 S.sub.9 . Our findings are based on single-crystal X-ray diffraction experiments. The fact that As.sub.4 S.sub.6 formed in a crystalline light-induced alteration product could indicate a heretofore unknown role of this molecule in the photoinduced changes of the physico-chemical properties of both bulk glasses and thin films in the As-S system, widely studied in optics and optoelectronics.
ISSN:0935-1221