1. Introduction
The self-dual concept of a quantum quasigroup offers a far-reaching unification of Hopf algebras (along with their non-associative extensions, e.g., [
1,
2,
3,
4]) and quasigroups [
5]. Consider a
bimagma , an object of a strict symmetric monoidal category
with
-morphisms giving a
magma structure or
multiplication , and a
comagma structure or
comultiplication , such that Δ is a magma homomorphism. (The latter
bimagma condition is equivalent to its dual: ∇ is a comagma homomorphism.) A bimagma
is a
quantum quasigroup if two dual morphisms are invertible in
: the
left composite
(“
” for “Gauche”) and the
right composite
(“
” for “Droite”). The qualifiers “left” and “right” refer to the side of the tensor product on which the comultiplications appear. Quantum quasigroups also have one-sided analogues [
6]. A
left quantum quasigroup just requires the invertibility of the left composite. Dually, a
right quantum quasigroup requires the invertibility of the right composite.
The present work surveys some connections between these structures and the quantum Yang–Baxter equation (QYBE):
[
7] (Section 2.2C). The QYBE applies to an endomorphism
of the tensor square of an object
A in a symmetric, monoidal category. For a given integer
, the notation
, for
, means applying
R to the
i-th and
j-th factors in the
n-th tensor power of
A. Since the left and right composite morphisms are endomorphisms of tensor squares, it is natural to seek conditions under which they satisfy the QYBE. Then, as observed by B.B. Venkov working in the category of sets with Cartesian products [
8] (Section 9), the QYBE corresponds to various distributivity conditions involving magma multiplications
appearing in the left and right composites along with diagonal or setlike comultiplications. While such classical distributivity conditions receive due consideration in this survey, the main novelty lies in the combination with more general comultiplications to obtain a much broader palette of QYBE solutions, corresponding to the bialgebraic concept of
quantum distributivity as recently introduced in [
9,
10]. It should also be noted (compare Remark 3) that distinct quantum quasigroups may furnish identical solutions to the QYBE. In other words, a classification of quantum quasigroups that exhibit quantum distributivity will be finer than a classification of the QYBE solutions that they provide.
The broad layout of the paper is as follows. The second section mainly covers background material about magmas and quasigroups, including some relations between the classical and quantum concepts of a quasigroup (
Section 2.4), and classical concepts of idempotence and distributivity (
Section 2.5), including a brief dictionary of the relevant knot theory terminology (Remark 2). The third section introduces the bialgebraic or “quantum” versions of idempotence (
Section 3.1), distributivity (
Section 3.2), and Albert’s notion of isotopy (
Section 3.3), in particular showing how quantum distributivity is transferred under bimagma isotopy (Theorem 4). The final section of the paper then presents various QYBE solutions obtained using quantum quasigroup techniques from one of the subtlest structures in quasigroup theory, commutative Moufang loops. While most of the QYBE solutions appearing in the paper are explicitly given in the symmetric monoidal category of sets under the Cartesian product, they may be transferred easily to categories of modules under the tensor product by application of the free module functor—compare [
11] (III, Ex. 3.6.3; IV, Proposition 2.4.8(d)).
For concepts and conventions that are not otherwise discussed in this paper, readers are referred to [
11]. We use algebraic notation, placing functions to the right of their arguments, or as superfixes. This enables compositions to be read in natural order from left to right. These conventions serve to control the profusion of brackets that all too easily arise in nonassociative structures. Since the comultiplications featured in this paper are not necessarily coassociative, the adapted version
of Sweedler notation is used (without any implication that the image of
a is of tensor rank 1) in concrete symmetric monoidal categories. Note that in this notation, coassociativity takes the form
Under coassociativity, the usual Sweedler notation is recovered for example by taking the superfixes or in lexicographic order as suffices (which are sometimes encased in parentheses).
2. Magmas, Quasigroups, and Loops
2.1. Magmas
Classically, a
magma is a set
Q carrying a binary
multiplication operation. The operation is generally written as · or otherwise indicated by simple juxtaposition of the two arguments, with · binding less strongly than juxtaposition (The older term
groupoid [
12] (p. 1) is now best reserved for categories with invertible morphisms). Thus
is a magma in the symmetric, monoidal category of sets under the Cartesian product, writing
in place of the usual ordered pair notation
. The magma
is described as the
opposite of the magma
or
. Here and elsewhere, the twist morphism of the symmetric, monoidal category in question is written as
, for example concretely implemented as
.
For a set
Q, the
transformation monoid is the monoid of self-maps from
Q to
Q. Now for an element
q of a magma
, define the
left multiplication or
and
right multiplication or
Specifying
or
is then equivalent (by Currying) to specification of the magma structure. In particular, using the algebraic convention for composition of maps, the associativity of a magma is equivalent to
R being a magma homomorphism.
2.2. Combinatorial and Equational Quasigroups
Quasigroups may be defined combinatorially or equationally. Combinatorially, a quasigroup is defined as a magma with the property that any two of the arguments in the equation determine the third uniquely. A loop is defined as a quasigroup Q having an element 1, the identity element, satisfying for each x in Q.
Under the equational definition, a quasigroup
is a set
Q carrying binary operations of multiplication,
right division / and
left division ∖, which together satisfy the following identities:
Note that (SL) gives the surjectivity of the left multiplication , while (IL) expresses its injectivity. The other two identities are their mirror images (chiral duals).
When an abelian group is considered as a combinatorial quasigroup under subtraction, the addition operation is the right division, while subtraction becomes the left division. If
x and
y are elements of a group
, the left division is given by
, with
as right division. More generally, these equations hold in a
diassociative loop, where the subloop generated by each pair of elements is associative, and thus forms a group. The loop
of unit octonions is diassociative, but not associative [
13] (Section 1.7).
2.3. Equational and Combinatorial One-Sided Quasigroups
Using an equational definition, a left quasigroup is a set Q equipped with a multiplication and left division satisfying the identities (SL) and (IL) of Equation (6). Dually, a right quasigroup is a set Q equipped with a multiplication and right division satisfying the identities (SR) and (IR) of Equation (6). A left loop is a left quasigroup with an identity element. Dually, a right loop is a right quasigroup with an identity element.
Combinatorially, a left quasigroup is a set Q with a multiplication such that in the equation , specification of a and b determines x uniquely. In equational terms, the unique solution is . The combinatorial definition of right quasigroups is dual. If Q is a set, the right projection product yields a left quasigroup structure on Q, while the left projection product yields a right quasigroup structure.
The following algebraic observations are often useful. In particular, they underlie simple conceptual proofs of results (such as Proposition 1 below) that otherwise require more complicated computational or syntactical proofs.
Lemma 1. Let and be magmas.- (a)
If is a right quasigroup, then so is .
- (b)
If is a left quasigroup, then so is .
- (c)
If and are right quasigroups, and is a magma homomorphism, then it is a right quasigroup homomorphism.
- (d)
If and are left quasigroups, and is a magma homomorphism, then it is a left quasigroup homomorphism.
Proof. Claims (a) and (b) are immediate from the definitions. Claim (c) will be proved and the claim (d) is dual. For elements x and z of P, one has by (SR). Thus, , whence by (IR). ☐
2.4. Quasigroups and Quantum Quasigroups
This paragraph summarizes some connections between quasigroups and quantum quasigroups. The symbol ⊤ is often used to denote a singleton set, in its role as a terminal object of categories of sets and functions.
Recall that a
unital magma
in a symmetric, monoidal category
is a magma
equipped with a
unit -morphism
such that
. Dually, a
counital comagma
within a symmetric, monoidal category
is a comagma
equipped with a
counit -morphism
such that
. In particular, in the symmetric, monoidal category
of sets with Cartesian products, the only counital comultiplication is the diagonal or setlike comultiplication
[
10] (Lemma 4.6).
Theorem 1. [5,6] Consider the category of sets and functions, with the symmetric monoidal category structure . Then, counital left, right, or two-sided quantum quasigroups in are, respectively, equivalent to left, right, or two-sided quasigroups. Theorem 2. Consider the symmetric, monoidal category of finite sets under the Cartesian product:- (a)
Left quantum quasigroups in are equivalent to triples that consist of a left quasigroup A with an automorphism L and endomorphism R [6]. - (b)
Right quantum quasigroups in are equivalent to triples that consist of a right quasigroup A with an endomorphism L and automorphism R [6]. - (c)
Quantum quasigroups in are equivalent to triples consisting of a quasigroup A equipped with automorphisms L and R [5].
Corollary 1. [6] Given a left quasigroup equipped with an automorphism L and endomorphism R, define as a multiplication and as a comultiplication. Then, is a left quantum quasigroup in . The chiral dual is as follows.
Corollary 2. Given a right quasigroup equipped with an endomorphism L and automorphism R, define as a multiplication and as a comultiplication. Then, is a right quantum quasigroup in .
Corollary 3. [5] Suppose that is a quasigroup equipped with two automorphisms L and R. Define as a multiplication and as a comultiplication. Then, is a quantum quasigroup in . 2.5. Some Classical Concepts
Definition 1. Let be a magma:- (a)
The magma is idempotent if for all x in Q.
- (b)
The magma is left repetitive if for all in Q, i.e., if the monogenic submagmas of Q are contained entirely within kernel classes of the map L of Equation (4).
- (c)
The magma is right repetitive if for all in Q, i.e., if the monogenic submagmas of Q are contained entirely within kernel classes of the map R of Equation (5).
- (d)
The magma is left (self-)distributive if for all in Q, i.e., if each left multiplication Equation (2) is a magma endomorphism.
- (e)
The magma is right (self-)distributive if for all in Q, i.e., if each right multiplication Equation (3) is a magma endomorphism.
- (f)
The magma is (self-)distributive if it is right and left distributive.
Remark 1. As observed at the end of Section 2.1, the “global" magma homomorphism property for the map R of Equation (5) corresponds to associativity of the magma in question. On the other hand, the “local" magma homomorphism property for each individual value corresponds to right distributivity as in Definition 1e. Remark 2. A quandle
is just an idempotent, right distributive right quasigroup (or dually, an idempotent, left distributive left quasigroup) [14] (Definition 14). A rack
is a right distributive right quasigroup (or dually, a left distributive left quasigroup) [14] (Definition 27). Racks may also be described by giving the opposite of the division along with the multiplication (as in Proposition 1 below). Crans has used the term shelf
for a one-sided distributive magma [15] (p. 52), the term spindle
for a one-sided idempotent distributive magma [15] (p. 53), and the term quasi-idempotent
for repetitive magmas [15] (Section 3.1.3). Proposition 1. Let be a right quasigroup, with opposite division :- (a)
If the magma is right distributive, then so is the magma .
- (b)
If the magma is right distributive, then the magma is left distributive.
- (c)
If the magma is right distributive, then it is right repetitive.
Proof. (a): If the magma is right distributive, its right multiplications and their inverses are magma automorphisms. Then, by Lemma 1(c), the right multiplications are magma automorphisms of .
(b): By (a), the magma is right distributive. Thus, its opposite is left distributive.
(c): For elements
of
Q, one has
since
is an automorphism of
. Right multiplication of the extremes of Equation (7) by
x then yields the right repetitiveness. ☐
3. Quantum Idempotence, Distributivity, and Isotopy
Idempotence, (self-)distributivity, and isotopy are standard concepts for magmas in the monoidal category of sets and Cartesian products. It is convenient to describe them as
classical concepts (compare the heading of
Section 2.5), as their extensions to
quantum concepts in bimagmas provide key tools for the identification of solutions to the QYBE in one- or two-sided quantum quasigroups.
3.1. Quantum Idempotence
For the following definition, compare [
10,
16].
Definition 2. Let be a bimagma in a symmetric, monoidal category . If the diagram commutes in , then the bimagma is said to satisfy the condition of quantum idempotence.
A comagma is said to be cocommutative if . The first result relates classical idempotence to quantum idempotence.
Proposition 2. [10] (Proposition 5.2) Let be a magma in . Define ; :- (a)
The structure is a counital, cocommutative, coassociative bimagma.
- (b)
The bimagma is quantum idempotent if and only if the magma is idempotent in the classical sense.
Non-classical examples of quantum idempotence are obtained as follows (Compare [
10] (Theorem 5.4) for the dual.).
Theorem 3. Let be a right quasigroup in which the identityis satisfied. Defineand .- (a)
The structure forms a right quantum quasigroup within the category .
- (b)
The bimagma is quantum idempotent.
Corollary 4. [10] (Corollary 5.5) Under the conditions of Theorem 3, the bimagma is cocommutative if and only if is classically idempotent. Commutative, diassociative loops (such as abelian groups) satisfy the conditions of Theorem 3, along with entropic right quasigroups (i.e., where the multiplication is a homomorphism), including sets equipped with left projections. The comultiplication (9) of Theorem 3 is also useful in other contexts.
Proposition 3. Let be a right distributive right quasigroup. Then, and Equation (9) yield a right quantum quasigroup .
Proof. The bimagma condition for amounts to satisfaction of in . It follows from the right distributivity and right repetitiveness as , and thus holds by Proposition 1c. Let be the right composite of , and let be the right composite of with the diagonal comultiplication Δ. Since , Corollary 2 shows that is a right quantum quasigroup. ☐
3.2. Quantum Distributivity
Definition 3. Suppose that is a bimagma in a symmetric, monoidal category:- (a)
The bimagma is said to satisfy the condition of quantum left distributivity if the left composite of satisfies the quantum Yang–Baxter equation (1).
- (b)
The bimagma is said to satisfy the condition of quantum right distributivity if the right composite of satisfies the quantum Yang–Baxter equation (1).
- (c)
The bimagma is said to satisfy the condition of quantum distributivity if it has both the left and right quantum distributivity properties.
The following result records B.B. Venkov’s motivating observation [
8] (Section 9) quoted in the introduction.
Proposition 4. [10] (Proposition 6.2) Let be a magma in the category of sets with the Cartesian product. Define :- (a)
The bimagma is quantum left distributive if and only if the magma is left distributive.
- (b)
The bimagma is quantum right distributive if and only if the magma is right distributive.
Remark 3. It is noteworthy that the distinct right quantum quasigroups and appearing in the proof of Proposition 3 have identical right composites. By Proposition 4, this common right composite solves the QYBE. Thus, a classification of quantum right distributive right quantum quasigroups would be finer than a classification of the QYBE solutions that they provide.
Corollary 5. [10] (Corollary 6.3) Suppose that is a nontrivial left quantum distributive left quantum quasigroup, or right quantum distributive right quantum quasigroup, within the category :- (a)
If is unital, it is not counital.
- (b)
If is counital, it is not unital.
Proposition 5. [9] (Proposition 4.4) Let be a bimagma in , equipped with comultiplication .- (a)
The bimagma is quantum left distributive if and the identityis satisfied. - (b)
The bimagma is quantum right distributive if and the identityis satisfied.
Corollary 6. Let be a bimagma in , equipped with comultiplication ; .- (a)
The bimagma is quantum left distributive if and the identityis satisfied [10] (Corollary 6.5). - (b)
The bimagma is quantum right distributive if and the identityis satisfied.
3.3. Quantum Homotopy and Isotopy
To begin, recall some classical definitions.
Definition 4. Consider magma structures(for ) in a concrete symmetric monoidal category .- (a)
A homotopy (in the classical sense)is defined as a triple of -morphisms such that the diagramcommutes. (See [13] (Section 1.2) for the case of quasigroups in the category of sets.) - (b)
The classical homotopy (14)
is an isotopy (in the classical sense)
if are -isomorphisms. (See [17] (Section 11) for the concept in a category of vector spaces, and [18] (Section 4) for quasigroups in the category of sets.) - (c)
A classical isotopy is principal when and .
Remark 4. Note that a classical homotopy (14) becomes a magma homomorphism if .
Definition 5. Let be a symmetric monoidal category. Let be a magma in , for . Consider a pair consisting of -morphisms and :- (a)
The pair is a magma homotopyin if the diagramcommutes in . - (b)
The magma homotopy (16) is said to be a magma isotopy if h and are -isomorphisms.
- (c)
A magma isotopy (16) is principal when and . Thus, a principal magma isotopy is specified by its second component .
Example 1. For a commutative ring K, take the symmetric monoidal category of K-modules:- (a)
Let be a Hopf algebra in . Then,is a non-classical magma homotopy. - (b)
Let denote the algebra of -matrices, considered as a magma in . Let denote matrix transposition. Then,is a non-classical magma isotopy.
Remark 5. (a) The concepts of Definition 4 provide instances of those of Definition 5.
(b) Under magma homotopies, the class of magmas in forms the object class of a category, the homotopy category of magmas in . The magma isotopies are the isomorphisms in this category.
Definition 6. Consider a symmetric monoidal category . Let be a bimagma in , for . Then, an automorphism of the object of is a principal bimagma isotopy
in if the decagon diagram
commutes in . Here, the superfix is used for the r-th tensor power of an object or morphism in . The lower part of the decagon diagram is called the nonagon diagram
or enneagon diagram.
Remark 6. The commuting of the upper triangle within the decagon diagram means that the pair is a principal magma isotopy.
For the following, compare [
9] (Proposition 5.5), which used a dual convention for labeling the domain and codomain of an isotopy.
Proposition 6. Suppose that , for , are bimagmas in , with permutations and . Then, the validity of the equationsis equivalent to the commuting of the enneagon diagram (18) for a principal bimagma isotopycomposed from and . Corollary 7. Consider a magma in , with commuting automorphisms f and g:- (a)
There is a bimagmain . - (b)
There is a bimagmain . - (c)
There is a principal bimagma isotopy
Remark 7. In Corollary 7b, duality interchanges and inverts the respective components of the magma isotopy to yield the corresponding components of the comultiplication.
3.4. Isotopy of Quantum Distributive Structures
In this section, some results from [
9] (Section 6) concerning the preservation of quantum distributivity under principal isotopy are summarized.
Proposition 7. Suppose that are bimagmas on an object Q of for , such that the following conditions are satisfied:- (a)
The comultiplication component is surjective;
- (b)
The comultiplication components and commute for ;
- (c)
The bimagma is quantum left distributive;
- (d)
There is a principal magma isotopywhose components are commuting automorphisms of ; - (e)
The equations and hold.
Then, is quantum left distributive.
The chiral dual of Proposition 7 is formulated as follows.
Corollary 8. Suppose that are bimagmas on an object Q of for , such that the following conditions are satisfied:- (a)
The comultiplication component is surjective;
- (b)
The comultiplication components and commute for ;
- (c)
The bimagma is quantum right distributive;
- (d)
There is a principal magma isotopywhose components are commuting automorphisms of ; - (e)
The equations and hold.
Then, is quantum right distributive.
The conditions of Proposition 7 and Corollary 8 are simplified and unified for quantum quasigroups in the symmetric monoidal category of finite sets and Cartesian products.
Theorem 4. Suppose that are quantum quasigroups on an object Q of for , such that the following conditions are satisfied:- (a)
The comultiplication components and commute for ;
- (b)
The quantum quasigroup is quantum distributive;
- (c)
There is a principal bimagma isotopywhose components are commuting automorphisms of . Then, is quantum distributive.