Abstract
The pyrite () is a model material where the impact of electron filling on a half-filled band system can be separated from changes in the bandwidth, since the unit cell volume does not change with . This contrasts with the system where the size difference between and makes the bandwidth vary at constant band filling. Our magnetic measurements show that there exists a clear relation between the presence of the antiferromagnetic phase developing below and charge localization. With the addition of Cu in , the ground state evolves towards a metallic paramagnetic state. These findings are discussed with the scenario based on charge ordering at low temperature in the charge transfer insulator pyrite, and also considering possible conducting surface states at low temperatures. At 300 K, the thermal conductivity decreases by 2.5 as increases from 0.00 to 0.07, even though the latter is much more electrically conductive than the former. This considerably extends the range of values for the thermal conductivity of the pyrites, from the largest in to the lowest in the present samples.
1 More- Received 10 April 2019
- Revised 23 July 2019
DOI:https://doi.org/10.1103/PhysRevMaterials.3.115401
©2019 American Physical Society