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Magma (Algebra)In abstract algebra, a magma (also called a groupoid) is a particularly basic kind of algebraic structure. Specifically, a magma consists of a set M equipped with a single binary operation M × M → M. A binary operation is closed by definition, but no other axioms are imposed on the operation. The term magma for this kind of structure was introduced by Bourbaki; however, the term groupoid is a very common alternative. Unfortunately, the term groupoid also refers to an entirely different kind of algebraic concept described at Groupoid. Types of magmas Magmas are not often studied as such; instead there are several different kinds of magmas, depending on what axioms one might require of the operation. Commonly studied types of magmas include Free magma A free magma on a set X is the "most general possible" magma generated by the set X (that is there are no relations or axioms imposed on the generators; see free object). It can be described, in terms familiar in computer science, as the magma of full binary trees with leaves labelled by elements of X. The operation is that of joining trees at the root. It therefore has a foundational role in syntax. See also: free semigroup, free group. More definitions A magma (S, *) is called - medial if it satisfies the identity xy * uz = xu * yz (i.e. (x * y) * (u * z) = (x * u) * (y * z) for all x, y, u, z in S),
- left semimedial if it satisfies the identity xx * yz = xy * xz,
- right semimedial if it satisfies the identity yz * xx = yx * zx,
- semimedial if it is both left and right semimedial,
- left distributive if it satisfies the identity x * yz = xy * xz,
- right distributive if it satisfies the identity yz * x = yx * zx,
- autodistributive if it is both left and right distributive,
- commutative if it satisfies the identity xy = yx,
- idempotent if it satisfies the identity xx = x,
- unipotent if it satisfies the identity xx = yy,
- zeropotent if it satisfies the identity xx * y = yy * x = xx,
- alternative if it satisfies the identities xx * y = x * xy and x * yy = xy * y,
- power-associative if the submagma generated by any element is associative,
- a semigroup if it satisfies the identity x * yz = xy * z (associativity),
- a semigroup with left zeros if it satisfies the identity x = xy,
- a semigroup with right zeros if it satisfies the identity x = yx,
- a semigroup with zero multiplication if it satisfies the identity xy = uv,
- a left unar if it satisfies the identity xy = xz,
- a right unar if it satisfies the identity yx = zx,
- trimedial if any triple of its (not necessarily distinct) elements generates a medial submagma,
- entropic if it is a homomorphic image of a medial cancellation magma.
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