“…The low-temperature fluorination used to prepare such systems generally involves a simple F insertion into interstitial sites (such as O vacancy sites), a substitution of F for O, or both . For manganese, fluorination of the oxygen-deficient phases Sr 2 Mn 2 O 5 and Sr 2 MnGaO 5 using XeF 2 as a fluorinating agent results in Sr 2 Mn 2 O 5– x F 1+ x and Sr 2 MnGaO 4.78 F 1.22 containing Mn 3+ /Mn 4+ valence states through the filling of the O vacancy sites with F and the partial substitution of F for O, as shown in Figure a. , Manganese oxides with the Ruddlesden–Popper (RP)-type layered structure having the general formula (AO)(AMnO 3 ) n , LaSrMnO 4 ( n = 1) and Ln 1.2 Sr 1.8 Mn 2 O 7 ( n = 2), accommodate F in the interstitial sites of the (La/Sr)O rock-salt layers, not in the anion sites of the perovskite block layers, giving LaSrMnO 4 F y ( y = 1, 1.7, 2) and Ln 1.2 Sr 1.8 Mn 2 O 7 F y ( y = 1, 2; Ln = La, Pr, Nd, Sm, Eu, Gd), − as shown in Figure b. Conversely, the oxygen-deficient phase Sr 3 Mn 2 O 6 , which contains pseudosquare and pseudohexagonal tunnels composed of corner-sharing MnO 5 square pyramids, exhibits a stepwise fluorination in which the F atoms occupy first the O vacancies at the equatorial sites of the MnO 5 square pyramid and then the interstitial sites in the rock-salt layers to form Sr 3 Mn 2 O 6 F y ( y = 1, 2, 3) with increasing fluorine content .…”