“…In order to improve magnetic performance with limited Co content, site-selective Co substitution is highly required; commercially it is important to reduce the usage of Co because of its unstable price and supply. For the Sr-La-Co system, although it was widely believed that Co mainly occupies the octahedrally coordinated 4f 2 site [8], it is now gradually accepted that Co mainly occupies the tetrahedrally coordinated 4f 1 site and partly octahedrally coordinated 2a and/or 12k sites [5,6,9,10]. Furthermore, it has been revealed that, in the samples synthesized under ambient atmosphere, La 3+ content, x, and Co 2+ content, y, are not necessarily identical but in general x>y, and their difference is compensated by the reduction of Fe 3+ to Fe 2+ [4,[11][12][13].…”