“…The average Fe(2)ÀO distance, 2.072 Å (Table 9), also provides evidence that Fe(2) is occupied by a mixture of ferrous and ferric iron in an approximate ratio of 1:1. According to Baur (1981) The relatively short Fe(1)ÀFe(2) distance in the face-sharing dimer, 2.924(1) Å , makes it understandable that only this dimer accepts Fe 2+ , but not the other, edge-and corner-sharing dimers: if it would host only Fe 3+ cations, electrostatic cation repulsion across the shared face would be much stronger and could lead to severe intrapolyhedral strain. In kidwellite, which contains only Fe 3+ ions in an otherwise very similar face-sharing dimer, the Fe(1)ÀFe(2) distance is considerably longer, 2.967(2) Å , as would be expected from a stronger repulsion across the shared face.…”