A method was reported by which the effective anisotropy of the Fe-SiO, and FezoNiso-SiO, granular solid can be measured using the magnetic relaxation equations. The pure Fe-SiO, and Fe20Ni,o-Si0, granular solid samples were fabricated using a sol-gel method in which the nanoscale bcc structure Fe and fcc structure Fe,oNi,o particles are dispersed in the silica matrix. The average size of the metal particles in the two ctiscussed Fe-SiO, and Fe,oNi80-Si0, granular solid samples are 10 n m and 8 nm, respectively. The obtained values of the effective magnetic anisotropy are in the order of the 106erg/cm3 and almost independent with temperature from 80K to 300K for these granular solid samples. These values are far larger than the magnetocrystalline anisotropy for the bulk bcc structure Fe and fcc structure FeZ,Niso. The larger stress magnetic anisotropy may result in these larger magnetic anisotropy for these granular solid samples. It was found that the efkctive magnetic anisotropy of the Fe-SiO, granular solid is larger than that of the FezoNiso-SiO, granular solid, which may result from the larger stress anisotropy in Fe-SiO, granular solid than in FezoNis,-SiO, granular solid and the reason is discussed.