The iron granular solid, in which ultrafine iron particles are dispers
ed, has been prepared with both SiO2 and Cu matrices using the sol-gel
method. The structure and morphology of these granular solid samples
are investigated by X-Ray Diffraction (XRD) and Transmission Electron
Microscopy (TEM). The magnetic properties are measured using a vibrati
ng sample magnetometer with 20 kOe maximum applied field. It is found
that the coercivity decreases very slightly with temperature from 80 t
o 300 K for these Fe-SiO2 and Fe-Cu granular solid samples with differ
ent average size of iron particles from 50 to 300 Angstrom. The magnet
ic anisotropy has been obtained from the measured magnetization curves
for these granular solid samples using the law of approach to saturat
ion, and the obtained values of the effective magnetic anisotropy are
all more than 10(6) erg/cm(3), which are larger than the value of the
magnetocrystalline anisotropy for bulk iron, The coercivity vs tempera
ture for these granular solid samples has been calculated using the Kn
eller and Luborsky theory, in which the magnetic anisotropy values obt
ained from the law of approach to saturation are used. The trends of t
he calculated coeroivity as a function of temperature are in reasonabl
e agreement with the observations.