Abstract
Magnetization of Fe3Ga4 is measured as a function of magnetic field and temperature. In weak fields, Fe3Ga4 is an antiferromagnetic with a Néel temperature of 392 K. In strong fields, it shows a metamagnetic transition and gives a saturation moment of 1.27 μB per Fe atom at 4.2 K and 70 kOe. Its Mössbauer spectrum is analyzed into four sextets, assigned to the crystal site Fe(1), Fe(2), Fe(3) and fe(4): each site has, respectively, an internal field of 225, 190, 150 and 171 kOe at 80 K. The magnetic phase diagram of Fe3Ga4 involving the metamagnetism can be explained by the Moriya-Usami theory.