“…It is seen that H r and DH decrease nonlinearly with Sr 2þ ion content x. The decrease of H r may be attributed to the effect of anisotropy, porosity, inhomogeneous demagnetization, saturation magnetization and the internal field [8,38,39]. The decrease of DH can be explained by existence of the divalent ions Fe 2þ , Mn 2þ , Sr 2þ and/or Mg 2þ among the octahedral B-sites which may affect the broadening of line width.…”