“…After significant effort, Sc 3+ has been substituted into the wurtzite AlN crystal structure at compositions of up to x ≈ 0.43 (i.e., Al 0.57 Sc 0.43 N) before phase separation to the rocksalt ScN end-member crystal structure occurs. ,,− Recent work has shown that the solubility of Sc 3+ depends both on ionic size and on ionicity, with Sc–N bonds more ionic than Al–N bonds; however, this ionicity effect is difficult to deconvolute from other effects. Other transition-metal cations such as Cr, Zr, Hf, Y, Ta, and Ni have also been investigated as alloys with AlN, and their properties have been studied. − While it seems unlikely from an ionic radius perspective that any rare earth cations would be able to incorporate into wurtzite AlN, recent work has shown that Er 3+ and Yb 3+ , much larger cations than Sc 3+ , were substituted successfully at x = 0.015 and up to x ≈ 0.15, respectively. , In GaN, Yb 3+ can incorporate up to x ≈ 0.3, consistent with the larger radius of Ga 3+ (∼0.47 Å) …”