Pseudobrookite-based ceramics with low thermal conductivity prepared from Fe-Ti-rich heavy mineral sand concentrate
- 1Jozef Stefan Institute, Low and Medium Energy Physics, Ljubljana, Slovenia (darko.hanzel@ijs.si)
- 2Jozef Stefan Institute, Advanced Materials, Ljubljana, Slovenia
- 3Jozef Stefan Institute, Nanostructured Materials, Ljubljana, Slovenia
- 4National Institute of Chemistry, Materials Chemistry, Ljubljana, Slovenia
- 5Cinkarna Celje, d.d. Inc., Celje, Slovenia
- 6Department of Geology, University of Ljubljana, Faculty of Natural Sciences and Engineering, Ljubljana, Slovenia
- 7CRISMAT, CNRS, Normandie Univ, ENSICAEN, UNICAEN, Caen, France
The potential of using natural Fe-Ti-rich heavy mineral sand, as an abundant, inexpensive, and ecologically acceptable raw material for the processing of pseudobrookite-based ceramics for thermoelectric applications is presented. The as-received raw powder was used in untreated form or after pre-oxidation at 600°C, 700°C, and 800°C for 1h in an air. The starting powders were consolidated into dense compacts via conventional solid-state sintering or spark plasma sintering. The phase composition, ferrous:ferric ratio and microstructural characteristics of the powders and sintered compacts were investigated by XRD, Mössbauer spectroscopy and SEM. The samples with a higher fraction of pseudobrookite exhibit relatively low thermal conductivity ranging between 2 and 3 W m-1 K-1, which is promising for practical thermoelectric applications. The Seebeck coefficient depends on the ferrous:ferric ratio and is rather low, leading to low power factor values for all the samples which will have to be improved for practical applications.
How to cite: Hanžel, D., Daneu, N., Radoševič, T., Bernik, S., Mazaj, M., Maček Kržmanc, M., Verhovšek, D., Kocjan, A., Vrabec, M., Spreitzer, M., and Guilmeau, E.: Pseudobrookite-based ceramics with low thermal conductivity prepared from Fe-Ti-rich heavy mineral sand concentrate, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-19755, https://doi.org/10.5194/egusphere-egu24-19755, 2024.