The Ag₈SnSe₆ argyrodite compound was synthesized by the direct melting of the elementary Ag, Sn and Se high purity grade stoichiometric mixture in a sealed silica ampoule. The prepared polycrystalline material was characterized by the X-ray diffraction (XRD), visible (VIS) and near-infrared (NIR) reflection and photoluminescence (PL) spectroscopy. XRD showed that the Ag₈SnSe₆ crystallizes in orthorhombic structure, Pmn2₁ space group with lattice parameters: ɑ = 7.89052(6) Ǻ, b = 7.78976(6) Ǻ, c = 11.02717(8) Ǻ. Photo-luminescence spectra of the Ag₈SnSe₆ polycrystalline wafer show two bands at 1675 nm and 1460 nm. Absorption edge position estimated from optical reflectance spectra is located in the 14131540 nm wavelength range.
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The structural origin of Cu+ ion conductivity in Cu6PS5I single crystals is described in terms of structural phase transitions studied by X-ray diffraction, polarized light microscopy and calorimetric measurements. Below the phase transition temperature at Tc = (144-169) K, Cu6PS5I belongs to the monoclinic, ferroelastic phase, with the space group Cc. Above Tc, the crystal changes its symmetry to a cubic superstructure, with the space group F43c (a' = 19.528); finally, at 274 K, the disordering of Cu+ ions increases to the symmetry F43m (a = 9.794). The phase transition at 274 K coincides well with a strong anomaly in electrical conductivity observed on the Arrhenius plot. Diffusion paths for Cu+ ions are evidenced by means of atomic displacement factors and a split model. The influence of copper stoichiometry on Tc is also discu
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