Abstract
The magnetic properties of a synthetic bornite, Cu5FeS 4, and of a Mn-bearing synthetic bornite were investigated using Superconducting Quantum Interference Device (SQUID) magnetometry and room temperature X-band Electron Paramagnetic Resonance (EPR) spectroscopy. Samples were synthesised from the elements using conventional dry methods. Chemical and phase compositions of the samples were confirmed by means of Electron Probe Micro-Analysis (EPMA) and by powder X-Ray Diffraction (XRD). Experimental results, interpreted using spectral simulations, highlight the superexchange nature of ionic interactions between paramagnetic centres and the role played by partial intervalence charge transfer between the Fe(III) and Cu(I) species in natural and synthetic bornite. The cation distribution in synthetic samples was shown to be different from the natural sample, in spite of the close similarity in chemical composition and structure.
Original language | English |
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Pages (from-to) | 113-121 |
Number of pages | 8 |
Journal | Periodico di Mineralogia |
Volume | 80 |
Issue number | 1 |
DOIs | |
Publication status | Published - Apr 2011 |
Keywords
- Bornite
- EPMA
- EPR spectroscopy
- Intervalence charge transfer
- Mn(II)
- SQUID magnetometry