Structural Phase Transitions on AgCuS Stromeyerite Mineral under Compression

The structural behavior of mineral Stromeyerite, AgCuS, has been studied by means of angle-dispersive X-ray diffraction measurements up to 13 GPa and ab initio total-energy calculations. Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (Au...

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Veröffentlicht in:Inorganic chemistry 2013-01, Vol.52 (1), p.355-361
Hauptverfasser: Santamaria-Perez, D, Morales-Garcia, A, Martinez-Garcia, D, Garcia-Domene, B, Mühle, C, Jansen, M
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container_end_page 361
container_issue 1
container_start_page 355
container_title Inorganic chemistry
container_volume 52
creator Santamaria-Perez, D
Morales-Garcia, A
Martinez-Garcia, D
Garcia-Domene, B
Mühle, C
Jansen, M
description The structural behavior of mineral Stromeyerite, AgCuS, has been studied by means of angle-dispersive X-ray diffraction measurements up to 13 GPa and ab initio total-energy calculations. Two high-pressure phase transitions are found at 1.4 and 5.7 GPa, from the initial distorted Ni2In-type phase (AuRbS-type, RP, space group Cmc21) through an anti-PbClF-type phase (HP1, space group P4/nmm) to a monoclinic distortion of this latter phase (HP2, space group P21/m). The collapse of the metal–metal interatomic distances at the RP–HP1 transition suggests a stronger metallic behavior of the high-pressure phase. The compressibility of the lattice parameters and the equation of state of the first pressure-induced phase have been experimentally determined. First-principles calculations present an overall agreement with the experimental results in terms of the high-pressure sequence and provide chemical insight into the AgCuS behavior under hydrostatic pressure.
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