Laser-heated melts based on the 43CaO–57Fe
2
O
3−
x
eutectic, close to the calcium ferrite (CF) composition, were measured with high-energy X-ray diffraction using aerodynamic levitation over a range of redox states controlled by CO/CO
2
gas atmospheres. The iron–oxygen coordination number was found to rise from 4.4 ± 0.3 at 15% Fe
3+
to 5.3 ± 0.3 at 87% Fe
3+
. Empirical potential structure refinement modelling was used to obtain the ferric and ferrous partial pair distribution functions. It was found that the Fe
2+
iron–oxygen coordination number is consistently approximately 10% higher in CF than in pure iron oxide, while Fe
3+
is essentially identical in all but the most oxygen-rich environments (where it is higher in CF compared with FeO
x
). The model also shows calcium octahedra to be the dominant species across all redox environments, although the population of CaO
7
increases with the availability of oxygen at the expense of CaO
4
and CaO
5
.
This article is part of the theme issue ‘Exploring the length scales, timescales and chemistry of challenging materials (Part 1)’.