Quartic residue Created 2026-10-06 Updated 2026-10-14
A nonzero element of a finite field is a quartic residue when for some nonzero . If , the multiplicative group of a finite field is cyclic of order divisible by four, so the quartic residues form a subgroup of index four; equivalently .
With the characteristic-prime-free part of , all roots of unity over a finite field lie in exactly when . This follows from the cyclicity of the multiplicative group of a finite field. For the least positive degree is one. A primitive root of order has the same field degree, because its Frobenius orbit closes exactly when .