Dolomite is a refractory raw material with the ideal composition of CaCO//3-MgCO//3. It is usually found associated with varying amounts of accessory oxides. Four high purity dolomites of different origin were densified by the calsintering process. The intrinsic sinterability is most affected by the iron oxide content and porosity, whereas the densification of the Fe//2O//3 doped dolomites are primarily affected by the aggregate size.
|Original language||English (US)|
|Number of pages||4|
|Specialist publication||American Ceramic Society Bulletin|
|State||Published - 1984|
All Science Journal Classification (ASJC) codes
- Ceramics and Composites