Single crystals of Zn doped lithium ferrite have been obtained by an improved flux method. The magnetic anisotropy and Mössbauer spectra of the system (Fe1−x3+Znx2+)[Fe(3+x)/23+Li(1−x)/2+]O4 with 0⩽x⩽0.5 have been investigated. According to the single-ion model, the magnetic anisotropy constant K1 depends mainly on the contribution of Fe3+ ions on tetrahedral sites and has always negative values (K1A≈−0.038 cm−1/ion; K1B≈0.0047 cm−1/ion for x=0.11–0.5) at room temperature. With increasing zinc content, the hyperfine magnetic field H on A sites is gradually decreased. The effect is presumably due to the spin canting and to the relaxation of the octahedral Fe3+ ions. The average reduction of the hyperfine magnetic field on B sites at 300 K is 22±2 kOe per Zn2+ nearest neighbor.
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Zhicheng Xu (2003) studied this question.
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