The morphology and magnetic properties of ultrafine Co
1-xCa
xFe
2O
4 particles prepared by chemical coprecipitation have been investigated. For particles heat treated at 800°C, an incremental linear relationship was found to exist between the lattice constant, ao, and the nominal composition of CaFe
2O
4, X, for 0≤X≤0.7. The curie temperature, Tc, of these ferrites also increases from 518°C to 550°C for 0≤X≤0.5. The saturation magnetization, σs, of ultrafine CoFe
2O
4 particles is 75 emu/g at 300 K. Curves of σ
s vs. X appear convex with no linearity at all for 0≤X≤1. These results on a
0, T
c, and σ
s indicate that ultrafine Co
1-xCa
xFe
2O
4 particles form as a solid solution, at least when X is in the range 0≤X≤0.7. In samples heat treated at 600°C or more, the grain size drops markedly as X increases. For example, for an 800°C treatment the size is 63 nm when X=0, but only 33 nm when X=0.2. In addition, the amount of a Fe
2O
3 formed by heat treatment increases as X increases. The largest value of the coercivity,
IH
c, obtained is 2750 Oe (0.2≤X≤0.3) for a sample heat treated at 800°C. This value is approximately equal to the intensity of the anisotropic magnetic field, Ha, calculated from the crystalline magnetic anisotropy constant, K, , of bulk CoFe
2O
4. There are two possible causes of the high
IH
c. One is that the single-domain CoFe
2O
4 particles might be separated by α-Fe
2O
3 particles, the other is that, as X increases, the K, of Co
1-xCa
xFe
2O
4 particles might become increasingly higher than the value for bulk CoFe
2O
4.
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