Abstrakt
The phase transitions and structural behaviour in natural bornite sample were investigated after heat treatment in air in a temperature range of (180÷500) ◦ C using high-resolution Faraday, X-ray diffraction and 5 7Fe Mössbauer spectroscopy studies. X-ray diffraction and the Mössbauer spectroscopy results show that polymorph phases can exist only at high temperatures, and at a temperature of 220 ◦ C a process of decomposition of bornite structure starts. Hematite is a main Fe-bearing phase and Cu is located mainly in cooper oxides present in the sample after annealing at 500 ◦ C.
| Język oryginału | angielski |
|---|---|
| Strony (od–do) | 1044-1047 |
| Liczba stron | 4 |
| Czasopismo | Acta Physica Polonica A |
| Tom | 134 |
| Numer wydania | 5 |
| Identyfikatory DOI | |
| Status publikacji | Opublikowano - 2018 |
Obszary tematyczne ASJC Scopus
- Ogólna fizyka i astronomia
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