Variations of Ag bonding distances in the AgBr 1− xI x solid-solution with rock-salt type structure by X-ray and EXAFS analyses

Abstract

The local structure of the AgBr 1−xI x rock-salt type solid-solution (0≤×≤0.4) was investigated by both EXAFS and single crystal X-ray diffraction. The first nearest neighbor distances from Br to Ag, and those from Ag to Br in the solid-solution can be determined from EXAFS method. Because Ag + surrounded by both Br − and I − ions is locally attracted to Br −, which has larger effective negative charge than I −, the Ag-Br distances gradually decrease with AgI content. There are observed systematic changes in both Br K- and Ag K-edge XANES spectra with increasing AgI content in connection with the change of the local structure in the solid-solution. The Br and I ions are distributed at random over the 4( a) sites of space group Fm3m without forming clusters. Both cation and anion are displaced from the lattice site because the Ag-Br and Ag-I distances in the solid-solution are close, respectively, to the distances in the pure rock-salt type AgBr and a hypothetical rock-salt type AgI. The particular increase in temperature factors by X-ray diffraction results from the static displacements of both cations and anions from the normal octahedral site. A large enhancement of ionic conductivity in AgI rich region will be ascribed to an increase in the concentration of the Frenkel defect caused by changes in local structures in an equilibrium state.