The studies of polaronic centers in a homologous series of scheelite-type compounds
AWO4 (
A = Ca, Sr, Ba) were performed using the W L
-edge and Sr K-edge X-ray absorption spectroscopy combined with the reverse Monte Carlo simulations, X-ray photoelectron
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The studies of polaronic centers in a homologous series of scheelite-type compounds
AWO4 (
A = Ca, Sr, Ba) were performed using the W L
-edge and Sr K-edge X-ray absorption spectroscopy combined with the reverse Monte Carlo simulations, X-ray photoelectron spectroscopy (XPS), and first-principles calculations. Protonated scheelites Hx
A O4 were produced using acid electrolytes in a one-step route at ambient conditions. The underlying mechanism behind this phenomenon can be ascribed to the intercalation of H
+ into the crystal structure of tungstate, effectively resulting in the reduction of W
6+ to W
5+, i.e., the formation of polaronic centers, and giving rise to a characteristic dark blue-purple color. The emergence of the W
5+ was confirmed by XPS experiments. The relaxation of the local atomic structure around the W
5+ polaronic center was determined from the analysis of the extended X-ray absorption fine structures using the reverse Monte Carlo method. The results obtained suggest the displacement of the W
5+ ions from the center of [W
O
] tetrahedra in the structure of
AWO4 scheelite-type tungstates. This finding was also supported by the results of the first-principles calculations.
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