The substructure was observed means of the X-ray diffraction microscopy and the magnetic properties were measured at room temperature on single crystals of 4% Si-Fe alloys as produced from the melt at various growth rates. Single crystals produced at slow cooling rate consist of large subgrains with a small orientation difference and have small coercive force and large remanent magnetization, as compared with those produced at fast cooling rate. Such a dependence of magnetic properties upon the substructure is discussed in terms of the nature of sub-boundaries.
Kenichi AraiKenji OhmoriHiroki MiuraN. Tsuya
Masaki ChibaTakenori TannoMaho AbeS. HashiK. IshiyamaToru KawamataRie Y. UmestuKazumasa SugiyamaShigeo SatoYosuke MochizukiKoji YatsushiroTsuyoshi KumagaiTsuguo FukudaShun‐ichiro TanakaShigeru Suzuki