Silver binding in argentiferous manganese oxide minerals investigated by synchrotron radiation X-ray absorption spectroscopy

The knowledge of the nature of silver occurrence and sites in argentiferous manganese oxides is significant for developing better process to extract silver from manganese-silver ores. Synchrotron radiation has been used to collect Ag K-edge X-ray absorption spectroscopy of three natural and five synthetic samples of silver-containing manganese oxide, basically in the phases of tunnel-type cryptomelane or todorokite and layer-type birnessite or chalcophanite. Data were also gathered on five standards including Ag foil, Ag2O, Ag2SO4, Ag2CO3, and AgNO3 to compare the local environments of Ag atoms with the samples. Ag K-edge XANES studies show that Ag is present in most of the samples in Ag+ oxidation state, except in the Ag-Tod sample through annealing step in the form of Ag0 nanoparticles which are also identified by TEM. The natural samples from Xiangguang manganese-silver ores exhibit similar coordination distances as the corresponding tunnel or layer structured synthetic samples. In the argentiferous cryptomelanes, silver cations do not occupy the tunnel centers like K+, but rather place on the common face sites of the cubic cage formed by MnO6 octahedra, coordinated with about four oxygen anions at ~ 2.4 A bond distances proved by the EXAFS results. In the silver-exchanged birnessites or natural argentiferous chalcophanite, silver cations probably occupy a tetrahedral coordination to interlayer O atoms and a position located above or below the vacant cavities in the Mn octahedra layers.