Abstract
Magnetization curves for the yttrium gallium iron garnet system Y3GaxFe5xO12 in the region x=1.31.5 are presented. These show anomalous temperature dependences. They are very similar in character to those anticipated by Néel and found for some spinel ferrites by Gorter. The molecular field theory is applied to these curves using an appropriate set of exchange constants. The best fit is achieved using rather small values for Jaa and Jdd. This is in good agreement with the most reliable determination of these constants for yttrium iron garnet and with the current belief that these constants should indeed be small.