Division conic algebras (GPR 8.6, GPR 13.8) #
A conic algebra can fall short of being a division algebra in the sense of GPR 8.6 (IsDivision:
nonzero, with bijective left and right multiplications by nonzero elements) in two ways: its norm
may have a nonzero null vector, or — without alternativity — a two-sided inverse may fail to make
the multiplications bijective. This file compares the three conditions
IsDivision A,C.HasTwoSidedInverses(every nonzero element has a two-sided inverse),C.norm.Anisotropic,
over a field. Without any hypothesis on the multiplication, division implies anisotropy, and
anisotropy implies two-sided inverses (n(x)⁻¹ (conj x)). For an alternative conic algebra all
three agree, once A ≠ 0: that is GPR 13.8 for conic algebras. The real sedenions show that the
alternativity hypothesis cannot be dropped (ConicAlgebra.not_isDivision_realSedenion,
GPR Exc. 19.29(e)).
The engine is the pair of identities (conj x) (x y) = n(x) y = (y x) (conj x), which hold in every
alternative conic algebra: write conj x = t(x)·1 - x and apply the alternative laws and
x² = t(x) x - n(x)·1. So when n(x) is invertible, n(x)⁻¹ (conj x) inverts left and right
multiplication by x.
Main results #
ConicAlgebra.conj_mul_mul_of_isAlternative,ConicAlgebra.mul_mul_conj_of_isAlternative:(conj x) (x y) = n(x) yand(y x) (conj x) = n(x) yin an alternative conic algebra.ConicAlgebra.anisotropic_of_isDivision: a division conic algebra has anisotropic norm.ConicAlgebra.hasTwoSidedInverses_of_anisotropic: over a field, an anisotropic norm gives two-sided inverses. No alternativity is needed.ConicAlgebra.anisotropic_of_hasTwoSidedInverses: for an alternative conic algebra, two-sided inverses force the norm to be anisotropic.ConicAlgebra.isDivision_of_anisotropic: over a field, a nonzero alternative conic algebra with anisotropic norm is a division algebra.ConicAlgebra.isDivision_iff_hasTwoSidedInverses,ConicAlgebra.isDivision_iff_anisotropic:GPR 13.8for alternative conic algebras over a field.
References #
- [GPR] Garibaldi, Petersson, Racine, Albert Algebras over Commutative Rings, 8.6, 13.8, Exc. 19.29.
In an alternative conic algebra, (conj x) (x y) = n(x) y: expand conj x = t(x)·1 - x, use
the left alternative law x (x y) = (x x) y, and the degree-two identity x x = t(x) x - n(x)·1.
In an alternative conic algebra, (y x) (conj x) = n(x) y, by the right alternative law.
x ((conj x) y) = n(x) y: the identity conj_mul_mul_of_isAlternative for conj x.
(y (conj x)) x = n(x) y: the identity mul_mul_conj_of_isAlternative for conj x.
A division conic algebra has anisotropic norm. If n(x) = 0 then x (conj x) = n(x)·1 = 0,
and conj x ≠ 0 when x ≠ 0, so x would be a zero divisor. No alternativity is needed.
For an alternative conic algebra, two-sided inverses force an anisotropic norm. If x y = 1
and n(x) = 0, then conj x = (conj x) (x y) = n(x) y = 0, so x = 0. Only the one-sided inverse
x y = 1 is used.
Over a field, an anisotropic norm gives two-sided inverses: n(x)⁻¹ (conj x) inverts any
nonzero x. Only x (conj x) = (conj x) x = n(x)·1 is used, so neither alternativity nor
associativity is needed — and the result is correspondingly weak: see
ConicAlgebra.HasTwoSidedInverses.
Over a field, a division conic algebra has two-sided inverses.
Over a field, a nonzero alternative conic algebra with anisotropic norm is a division
algebra in the sense of GPR 8.6. For u ≠ 0 the scalar n(u) is invertible, and
v ↦ n(u)⁻¹ ((conj u) v) and v ↦ n(u)⁻¹ (v (conj u)) invert left and right multiplication by u,
by the identities (conj x) (x y) = n(x) y = x ((conj x) y) and
(y x) (conj x) = n(x) y = (y (conj x)) x.
GPR 13.8, for conic algebras over a field. An alternative conic algebra is a division
algebra in the sense of GPR 8.6 exactly when it is nonzero and every nonzero element has a
two-sided inverse. Without alternativity only → holds: the real sedenions have two-sided inverses
but are not a division algebra (ConicAlgebra.not_isDivision_realSedenion).
An alternative conic algebra over a field is a division algebra exactly when it is nonzero and its norm is anisotropic.