Abstract
Co-site crystalline fields in YCo5 and Y2 Co17 are calculated using a point-charge model. It is shown that the 2c site in YCo5 and the 18j site in Y2 Co17 make positive contributions to the magnetic anisotropy, while the 3g site in YCo5 and the 18h, 9d, and 6c sites in Y2 Co17 make negative contributions, in agreement with Streever's NMR result. Through an NMR investigation, M substitution for Co in Y2(Co1xMx)17 (M=Cu,Al) is demonstrated to occur at random in M=Cu and with a site preference in M=Al. Al is found mainly to prefer a 6c dumbbell site. Consequently, it is shown that the different magnetic anisotropy behaviors between Y2(Co1xCux)17 and Y2(Co1xAlx)17 arise from the differences in site preference between Cu and Al for Co.