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The magnetic properties of the alloy system Fe3-xMnxSi have been studied bymeasuring magnetization for samples with x = 0, 0.1, 0.25, 0.5, and by thermalscanning techniques for samples with x = 0, 0.1. The results reveal that thesystem is ferromagnetic in this composition range. Zero field cooling and fieldcooling magnetization measurements indicate a similar magnetic ordering andmagnetic anisotropy in all samples. The saturation magnetization for theannealed samples was higher than that for as prepared samples. This isattributed to the reduction of magnetic domain boundaries rather than toimproving magnetic order as a result of annealing. Further, TC valuesdetermined from thermal DSC measurements are in good agreement with previouslyreported results based on magnetic measurements.

Magnetization measurements on as prepared and annealed Fe3-xMnxSi alloys