In mathematics, a band is a semigroup in which every element is idempotent. Bands were first studied and named by ; the lattice of varieties of bands was described independently in the early 1970s by Biryukov, Fennemore and Gerhard. Semilattices, left-zero bands, right-zero bands, rectangular bands, normal bands, left-regular bands, right-regular bands and regular bands, specific subclasses of bands that lie near the bottom of this lattice, are of particular interest and are briefly described below.
A left-zero band is a band satisfying the equation
xy = x,
whence its Cayley table has constant rows. Symmetrically, a right-zero band is one satisfying
xy = y,
so that the Cayley table has constant columns.
Rectangular bands
A rectangular band is a band S that satisfies
xyx = x for all x, y ∈ S,
or equivalently,
xyz = xz for all x, y, z ∈ S,
The second characterization clearly implies the first, and conversely the first implies xyz = xy = z = xz. There is a complete classification of rectangular bands. Given arbitrary sets I and J one can define a semigroup operation on I × J by setting The resulting semigroup is a rectangular band because
In fact, any rectangular band is isomorphic to one of the above form. Left-zero and right-zero bands are rectangular bands, and in fact every rectangular band is isomorphic to a direct product of a left-zero band and a right-zero band. All rectangular bands of prime order are zero bands, either left or right. A rectangular band is said to be purely rectangular if it is not a left-zero or right-zero band. In categorical language, one can say that the category of nonempty rectangular bands is equivalent to, where is the category with nonempty sets as objects and functions as morphisms. This implies not only that every nonempty rectangular band is isomorphic to one coming from a pair of sets, but also these sets are uniquely determined up to a canonical isomorphism, and all homomorphisms between bands come from pairs of functions between sets. If the set I is empty in the above result, the rectangular band I × J is independent of J, and vice versa. This is why the above result only gives an equivalence between nonempty rectangular bands and pairs of nonempty sets. Rectangular bands are also the T-algebras, where T is the monad on Set with T=X×X, T=f×f, being the diagonal map, and.
This is the same equation used to define medial magmas, and so a normal band may also be called a medial band, and normal bands are examples of medial magmas. We can also say a normal band is a band S satisfying
axyb = ayxb for all a, b, x, and y ∈ S.
Left-regular bands
A left-regular band is a band S satisfying
xyx = xy for all x, y ∈ S
If we take a semigroup and define a ≤ bif and only ifab = b, we obtain a partial ordering if and only if this semigroup is a left-regular band. Left-regular bands thus show up naturally in the study of posets.
Right-regular bands
A right-regular band is a band S satisfying
xyx = yx for all x, y ∈ S
Any right-regular band becomes a left-regular band using the opposite product. Indeed, every variety of bands has an 'opposite' version; this gives rise to the reflection symmetry in the figure below.
Regular bands
A regular band is a band S satisfying
zxzyz = zxyz for all x, y, z ∈ S
Lattice of varieties
When partially ordered by inclusion, varieties of bands naturally form a lattice, in which the meet of two varieties is their intersection and the join of two varieties is the smallest variety that contains both of them. The complete structure of this lattice is known; in particular, it is countable, complete, and distributive. The sublattice consisting of the 13 varieties of regular bands is shown in the figure. The varieties of left-zero bands, semilattices, and right-zero bands are the three atoms of this lattice. Each variety of bands shown in the figure is defined by just one identity. This is not a coincidence: in fact, every variety of bands can be defined by a single identity.
