The chemistry of Sm2+ in solid oxide environment is reviewed and explored b
y a systematic search for crystal lattices stabilizing Sm2+ at particular r
eaction conditions. It is demonstrated that SrB4O7 is representing an uniqu
e lattice stabilizing Sm2+ even when crystals are prepared in air. However,
when exchanging Sr by e.g. Ca, Ba, Cd, Pb, only Sm3+ doping could be trace
d. Sm2+ in lattices free of nuclear spins is of interest to hyperfine optic
al hole burning. In this respect we have prepared single crystals of SrSO4
doped predominantly by Sm2+. In summary, we can say that the stability of S
m2+ in an oxide environment is strongly depending on local effects of coord
ination and a reduction mechanism not revealed so far. In particular it rem
ains unclear, why Sm2+ can be included into SrB4O7 crystals under oxidizing
conditions, whereas in the rapidly cooled melt no Sm2+ could be traced.