Abstract
CaFeO2Cl is a unique exception in the family of the iron oxyhalides. Its crystal structure is not related to the Ruddlesden-Popper phases as known for the other members, but contains layers of edge-sharing FeO2/2O3/3 pyramids without Fe-Cl contacts. The iron atoms form a distorted honeycomb substructure. Magnetization measurements on single crystals show an unexpected weak anisotropy and indicate antiferromagnetic ordering of the iron magnetic moments already at room temperature. Fe-57 Mossbauer spectra confirm the trivalent oxidation state of iron and the presence of magnetic order. DFT calculations using the LDA + U approach support a Mott-insulating antiferromagnetic ground state and indicate a Neel-type ordered antiferromagnetic state in the honeycomb layer. The band gap from optical measurements is 1.3 eV and agrees with the red-brown colour as well as with the theoretical calculations.
| Dokumententyp: | Zeitschriftenartikel | 
|---|---|
| Fakultät: | Chemie und Pharmazie > Department Chemie | 
| Themengebiete: | 500 Naturwissenschaften und Mathematik > 540 Chemie | 
| ISSN: | 0932-0776 | 
| Sprache: | Englisch | 
| Dokumenten ID: | 90061 | 
| Datum der Veröffentlichung auf Open Access LMU: | 25. Jan. 2022 09:33 | 
| Letzte Änderungen: | 25. Jan. 2022 09:33 | 
		
	