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Sinkendes Niveau: Der kubische Perowskit BaFeO3 (siehe Bild; Ba blau, Fe braun, O weiß), erhältlich durch eine Oxidation mit Ozon bei tiefer Temperatur, ist ferromagnetisch, mit einem recht großen Moment von 3.5 μB pro Fe‐Ion oberhalb eines kleinen kritischen Felds von ca. 0.3 T. Dieser spezifische Ferromagnetismus wird mit der Verstärkung des O→Fe‐Ladungstransfers erklärt, die vom Absenken der Fe...
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