A low content of chromium (≤5 mol %) has been incorporated into a SnO cassiterite by a coprecipitation route in a basic medium, followed by an annealing step under an O flow at = 800 °C and = 1000 °C. Accurate UV-vis and EPR spectroscopy investigations show the coexistence of isolated Cr and Cr ions as well as ferromagnetic Cr-Cr and antiferromagnetic Cr-Cr interactions. The strong purple hue is related to the isolated Cr ions stabilized in a distorted octahedral site. This is thanks to the second-order Jahn-Teller (SOJT) effect with a crystal field splitting 10 value around 2.4 eV, whereas the 10 value is around 2 eV for isotropic Cr ions, partially substituted for Sn ions in cassiterite. Just after the coprecipitation process, only Cr species are stabilized in this rutile network with a poor crystallinity. The isolated Cr content remains high after annealing at 800 °C for 2 days especially for the highest Cr rate (2 and 5 mol %), leading to a darker purple color, but unfortunately the Cr content also increases for a higher Cr concentration. A lighter purple hue can be reached after calcination at a higher temperature ( = 1000 °C) for a shorter time (4 h) but with a lower Cr content to avoid Cr clusters. This is due to stabilizing a high content of isolated Cr species and limiting the Cr-Cr ferromagnetic interactions, which are optimal for a 2% Cr content and also cause the color to darken. The key roles of the Cr rate and the Cr-Cr clusters create local defects whose concentration strongly varies with a total Cr content, which have then been demonstrated to strongly influence the optical and magnetic properties.
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http://dx.doi.org/10.1021/acs.inorgchem.9b02943 | DOI Listing |
Inorg Chem
January 2020
CNRS, Université de Bordeaux, Bordeaux INP, ICMCB, UMR 5026 , F-33600 Pessac , France.
A low content of chromium (≤5 mol %) has been incorporated into a SnO cassiterite by a coprecipitation route in a basic medium, followed by an annealing step under an O flow at = 800 °C and = 1000 °C. Accurate UV-vis and EPR spectroscopy investigations show the coexistence of isolated Cr and Cr ions as well as ferromagnetic Cr-Cr and antiferromagnetic Cr-Cr interactions. The strong purple hue is related to the isolated Cr ions stabilized in a distorted octahedral site.
View Article and Find Full Text PDFEnviron Geochem Health
April 2012
GEOBIOTEC, University of Aveiro, Campus de Santiago, 3810-193, Aveiro, Portugal.
The Marrancos gold mineralisation has a chemical assemblage of Fe-As-Se-Bi-Au-Ag-Te-(Cu-Pb-Zn-Sn-W). The -200 mesh of 144 topsoil samples was analysed by ICP-MS to determine total contents of 53 elements that include potentially harmful elements like Cd, As and Pb. The soil geochemistry shows that some trace elements occur in considerably high concentrations.
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