Using 350-g arc-melted button heats, measurements have been made of the effects of residual silicon on the initial permeability (μ40B) of 4-Moly Permalloy. Cooling rates in the atomic ordering range (1200°–600°F) were varied between 70° and 4750°F/h. Silicon has a considerable effect on cooling rate response, its effect being similar to molybdenum in that it slows down the cooling rate (CRopt) required to develop the best permeability. Since minor variations in nickel and molybdenum content also affect CRopt, it cannot be stated unequivocally that silicon is good or bad for properties. It is demonstrated that if the cooling rate is too fast for a given base composition, silicon is detrimental, while the reverse is true if the cooling rate is too slow for the base composition. However, in the latter case, the benefit of silicon is dependent upon maintaining a dry hydrogen atmosphere during the final anneal; with a −30°F dew-point hydrogen, the improvement is lost due to oxidation of the silicon. Some further effects of dew-point variations during the final anneal on magnetic properties are described in relation to residual silicon and aluminum.
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