Medial magma

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In abstract algebra, a medial magma or medial groupoid is a magma or groupoid (that is, a set with a binary operation) that satisfies the identity

(xy) • (uv) = (xu) • (yv),

or more simply,

xyuv = xuyv

for all x, y, u and v, using the convention that juxtaposition denotes the same operation but has higher precedence. This identity has been variously called medial, abelian, alternation, transposition, interchange, bi-commutative, bisymmetric, surcommutative, entropic, etc.[1]

Any commutative semigroup is a medial magma, and a medial magma has an identity element if and only if it is a commutative monoid. The "only if" direction is the Eckmann–Hilton argument. Another class of semigroups forming medial magmas are normal bands.[2] Medial magmas need not be associative: for any nontrivial abelian group with operation + and integers mn, the new binary operation defined by xy = mx + ny yields a medial magma that in general is neither associative nor commutative.

Using the categorical definition of product, for a magma M, one may define the Cartesian square magma M × M with the operation

(x, y) • (u, v) = (xu, yv).

The binary operation of M, considered as a mapping from M × M to M, maps (x, y) to xy, (u, v) to uv, and (xu, yv)  to (xu) • (yv) . Hence, a magma M is medial if and only if its binary operation is a magma homomorphism from M × M to M. This can easily be expressed in terms of a commutative diagram, and thus leads to the notion of a medial magma object in a category with a Cartesian product. (See the discussion in auto magma object.)

If f and g are endomorphisms of a medial magma, then the mapping fg defined by pointwise multiplication

(fg)(x) = f(x) • g(x)

is itself an endomorphism. It follows that the set End(M) of all endomorphisms of a medial magma M is itself a medial magma.

Bruck–Murdoch–Toyoda theorem

The Bruck–Murdoch–Toyoda theorem provides the following characterization of medial quasigroups. Given an abelian group A and two commuting automorphisms φ and ψ of A, define an operation on A by

xy = φ(x) + ψ(y) + c,

where c some fixed element of A. It is not hard to prove that A forms a medial quasigroup under this operation. The Bruck–Toyoda theorem states that every medial quasigroup is of this form, i.e. is isomorphic to a quasigroup defined from an abelian group in this way.[3] In particular, every medial quasigroup is isotopic to an abelian group.

The result was obtained independently in 1941 by Murdoch and Toyoda.[4][5] It was then rediscovered by Bruck in 1944.[6]

Generalizations

The term medial or (more commonly) entropic is also used for a generalization to multiple operations. An algebraic structure is an entropic algebra[7] if every two operations satisfy a generalization of the medial identity. Let f and g be operations of arity m and n, respectively. Then f and g are required to satisfy

[math]\displaystyle{ f(g(x_{11}, \ldots, x_{1n}), \ldots, g(x_{m1}, \ldots, x_{mn})) = g(f(x_{11}, \ldots, x_{m1}), \ldots, f(x_{1n}, \ldots, x_{mn})). }[/math]

Nonassociative examples

A particularly natural example of a nonassociative medial magma is given by collinear points on Elliptic curves. The operation xy = −(x + y) for points on the curve, corresponding to drawing a line between x and y and defining xy as the third intersection point of the line with the elliptic curve, is a (commutative) medial magma which is isotopic to the operation of elliptic curve addition.

Unlike elliptic curve addition, xy is independent of the choice of a neutral element on the curve, and further satisfies the identities x • (xy) = y. This property is commonly used in purely geometric proofs that elliptic curve addition is associative.

See also

  • Category of medial magmas

Citations

References