Abstract
Iron cation distribution in magnetite may be determined by thermoelectric power measurements in which values are monitored as a factor of temperatures. Data on cation distribution are given over a temperature range from 600 to 1500C.
Original language | English |
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Pages (from-to) | 520-522 |
Number of pages | 3 |
Journal | Journal of the American Ceramic Society |
Volume | 64 |
Issue number | 9 |
Publication status | Published - Sep 1981 |
ASJC Scopus subject areas
- Ceramics and Composites