§ 1. Laws of composition; associativity; commutativity
1. Laws of composition
Definition 1
Let E be a set. A mapping f of E × E into E is called a law of composition on E. The value f(x, y) of f for an ordered pair (x, y) ∈ E × E is called the composition of x and y under this law. A set with a law of composition is called a magma.
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Cited by I § 7. Free monoids, free groups
The composition of x and y is usually denoted by writing x and y in a definite order and separating them by a characteristic symbol of the law in question (a symbol which it may be agreed to omit). Among the symbols most often used are + and ., the usual convection being to omit the latter if desired; with these symbols the composition of x and y is written respectively as x + y and x.y or xy. A law denoted by the symbol + is usually called addition (the composition x + y being called the sum of x and y) and we say that it is written additively; a law denoted by the symbol . is usually called multiplication (the composition x.y = xy being called the product of x and y) and we say that it is written multiplicatively. In the general arguments of paragraphs 1 to 3 of this chapter we shall generally use the symbols ⊔ and ⊓ to denote arbitrary laws of composition.
By an abuse of language, a mapping of a subset of E × E into E is sometimes called a law of composition not everywhere defined on E.
Example
(1) The mappings (X, Y) ↦ X ∪ Y and (X, Y) ↦ X ∩ Y are laws of composition on the set of subsets of a set E.
(2) On the set N of natural numbers, addition, multiplication and exponentiation are laws of composition (the compositions of x ∈ N and y ∈ N under these laws being denoted respectively by x + y, xy or x.y and x^y) (Set Theory, III, § 3, no. 4).
(3) Let E be a set; the mapping (X, Y) ↦ X ⋅ Y is a law of composition on the set of subsets of E × E (Set Theory, II, § 3, no. 3, Definition 6); the mapping (f, g) ↦ f ⋅ g is a law of composition on the set of mappings of E into E (Set Theory, II, § 5, no. 2).
(4) Let E be a lattice (Set Theory, III, § 1, no. 11); if sup(x, y) denotes the least upper bound of the set {x, y}, the mapping (x, y) ↦ sup(x, y) is a law of composition on E. Similarly for the greatest lower bound inf(x, y). Example 1 above is a particular case of this with ordered by inclusion.
(5) Let be a family of magmas. Let denote the law of composition on . The mapping
Let be a law of composition on a set E. Given any two subsets X, Y of E, (provided this notation does not lead to confusion†) will denote the set of elements in E, where (in other words, the image of under the mapping ).
If we usually write instead of and instead of . The mapping is a law of composition on the set of subsets of E.
Definition 2
Let E be a magma and denote its law of composition. The law of composition on E is called the opposite of the above. The set E with this law is called the opposite magma of E.
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Let E and E' be two magmas; we shall denote their laws by the same symbol . Conforming with the general definitions (Set Theory, IV, § 1, no. 5), a bijective mapping f of E onto E' such that
More generally:
Definition 3
A mapping f of E into E' such that relation (1) holds for every ordered pair is called a homomorphism, or morphism, of E into E'; if , f is called an endomorphism of E.
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The identity mapping of a magma E is a homomorphism, the composition of two homomorphism is a homomorphism.
† The following is an example where this principle would lead to confusion and should therefore not be used. Suppose that the law of composition in question is the law between subsets of a set E; a law of composition
For a mapping of E into E' to be an isomorphism, it is necessary and sufficient that it be a bijective homomorphism and is then an isomorphism of E' onto E.
2. Composition of an ordered sequence of elements
Recall that a family of elements of a set E is a mapping of a set I (called an indexing set) into E; a family is called finite if the indexing set is finite.
A finite family of elements of E whose indexing set I is totally ordered is called an ordered sequence of elements of E.
In particular, every finite sequence , where H is a finite subset of the set of natural numbers, can be considered as an ordered sequence if H is given the order relation induced by the relation between natural numbers.
Two ordered sequences and are called similar if there exists an ordered set isomorphism of I onto K such that for all .
Every ordered sequence is similar to a suitable finite sequence. For there exists an increasing bijection of A onto an interval of .
Definition 4
Let* be an ordered sequence of elements in a magma E whose indexing set A is non-empty. The composition (under the law T) of the ordered sequence , denoted by , *is the element of E defined by induction on the number of elements in A as follows:
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(1) if then ;
(2) if A has elements, is the least element of A and , then .
It follows immediately (by induction on the number of elements in the indexing sets) that the compositions of two similar ordered sequences are equal; in particular, the composition of any ordered sequence is equal to the composition of a finite sequence. If has three elements () the composition is .
Remark
Note that there is a certain arbitrariness about the definition of the composition of an ordered sequence; the induction we introduced proceeds "from right to left". If we proceeded "from left to right", the composition of the above ordered sequence would be .
As a matter of notation, the composition of an ordered sequence is written for a law denoted by ; for a law written additively it is usually denoted by and called the sum of the ordered sequence (the being called the terms of the sum); for a law written multiplicatively it is usually denoted by and called the product of the ordered sequence (the being called the factors of the product).†
When there is no possible confusion over the indexing set (nor over its ordering) it is often dispensed with in the notation for the composition of an ordered sequence and we then write, for example for a law written additively, instead of ; similarly for the other notations.
For a law denoted by the composition of a sequence with indexing set a non-empty interval of is denoted by or ; similarly for laws denoted by other symbols.
Let E and F be two magmas whose laws of composition are denoted by and a homomorphism of E into F. For every ordered sequence of elements of E
3. Associative laws
Definition 5
A law of composition* on a set E is called associative if, for all elements in E,
The opposite law of an associative law is associative.
Example
(1) Addition and multiplication of natural numbers are associative laws of composition on (Set Theory, III, § 3, no. 3, Corollary to Proposition 5) (2) The laws cited in Examples (1), (3) and (4) of no. 1 are associative.
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Cites E III § 3. Equipotent sets. Cardinals, Corollary, E III § 3
Theorem 1 (Associativity theorem)
Let* E be an associative magma whose law is denoted by . Let A be a totally ordered non-empty finite set, which is the union of an ordered sequence of non-empty subsets such that the relations imply ; let be an ordered sequence of elements in E with A as indexing set. Then
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Cites E II § 5. Product of a family of sets, E III § 3. Equipotent sets. Cardinals, Definition 3
Cited by Exercise 3, § 1, Proposition 2, Theorem 3, Definition 3, I § 2, Proposition 3, I § 7
† The use of this terminology and the notation must be avoided if there is any risk of confusion with the product of the sets defined in the theory of sets (Set Theory, II, § 5, no. 3). However, if the are cardinals and addition (resp. multiplication) is the cardinal sum (resp. the cardinal product), the cardinal denoted by (resp. ) in the above notation is the cardinal sum (resp. cardinal product) of the family (Set Theory, III, § 3, no. 3).
§ 1.3
We prove the theorem by induction on the cardinal of . Let be the cardinal of and its least element; let . If , as the are non-empty, of necessity and the theorem is obvious. Otherwise, assuming the theorem holds for an indexing set with at most elements, we distinguish two cases:
(a) has a single element . Let . The left-hand side of (3) is equal, by definition, to ; the right-hand side is equal, by definition, to
(b) Otherwise, let be the least element of (and hence of ); let and let for ; then for . The set has elements and the conditions of the theorem hold for and its subsets ; hence by hypothesis:
For an associative law denoted by the composition of a sequence is also denoted (since no confusion can arise) by
In particular, if ,
If is a subset of , we sometimes denote, in conformity with the above notation, by the set , where
It is important not to confuse this set with the set of , where runs through .
4. Stable subsets. Induced laws
Definition 6
A subset of a set is called stable under the law of composition on if the composition of two elements of belongs to . The mapping of into is then called the law induced on by the law . The set with the law induced by is called a submagma of .
In other words, for to be stable under a law it is necessary and sufficient that . A stable subset of and the corresponding submagma are often identified.
The intersection of a family of stable subsets of is stable; in particular there exists a smallest stable subset of containing a given subset ; it is said to be generated by and is called a generating system of or a generating set of . The corresponding submagma is also said to be generated by .
Proposition 1
Let and be two magmas and a homomorphism of into . (i) The image under of a stable subset of is a stable subset of . (ii) The inverse image under of a stable subset is a stable subset of . (iii) Let be a subset of . The image under of the stable subset of generated by is the stable subset of generated by . (iv) If is a second homomorphism of from the set of elements of such that is a stable subset of .
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Assertions (i), (ii) and (iv) are obvious; we prove (iii). Let be the stable subset of E generated by X and the stable subset of F generated by . By (i) and by (ii) , whence .
Proposition 2
Let E be an associative magma and X a subset of E. Let X' be the set of , where and where for . The stable subset generated by X is equal to X'.
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It follows immediately by induction on n that the composition of an ordered sequence of n terms belonging to X belongs to the stable subset generated by X; it is therefore sufficient to verify that X' is stable. Now if u and v are elements of X' they are of the form , with for ; then (Theorem 1) belongs to X'.
Example
(1) In the set of natural numbers the stable subset under addition generated by {1} is the set of integers ; under multiplication the set {1} is stable.
(2) Given a law on a set E, for a subset {h} consisting of a single element to be stable under the law it is necessary and sufficient that ; h is then said to be idempotent. For example, every element of a lattice is idempotent for each of the laws sup and inf.
(3) For an associative law on a set E the stable subset generated by a set {a} consisting of a single element is the set of elements , where n runs through the set of integers .
5. Permutable elements. Commutative laws
Definition 7
Let E be a magma whose law is denoted by . Two elements x and y of E are said to commute (or to be permutable) if .
Definition 8
A law of composition on a set E is called commutative if any two elements of E commute under this law. A magma whose law of composition is commutative is called a commutative magma.
A commutative law is equal to its opposite.
Example
(1) Addition and multiplication of natural numbers are commutative laws on (Set Theory, III, § 3, no. 3, Corollary to Proposition 5).
(2) On a lattice the laws sup and inf are commutative; so, in particular, are the laws and between subsets of a set E.
(3) Let E be a set of cardinal . The law between mappings of E into E is not commutative as is seen by taking f and g to be distinct constant mappings, but the identity mapping is permutable with every mapping.
(4) Let be a commutative law on ; the law
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Cites E III § 3. Equipotent sets. Cardinals, Corollary, E III § 3
Definition 9
Let be a magma and a subset of . The set of elements of which commute with each of the elements of is called the centralizer of .
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Let and be two subsets of and and their respective centralizers. If , then .
Let be a family of subsets of and for all let be the centralizer of . The centralizer of is .
Let be a subset of and the centralizer of . The centralizer of is called the bicentralizer of . Then . The centralizer of is equal to . For is contained in its bicentralizer and the relation implies .
Proposition 3
Let be an associative magma whose law is denoted by . If an element of commutes with each of the elements and of , it commutes with .
For
Corollary
Let be an associative magma. The centralizer of any subset of is a stable subset of .
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Definition 10
The centralizer of a magma is called the centre of . An element of the centre of is called a central element of .
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Cites Corollary
If is an associative magma its centre is a stable subset by the Corollary to Proposition 3 and the law induced on its centre is commutative.
Proposition 4
Let be an associative magma, and two subsets of . If every element of commutes with every element of every element of the stable subset generated by commutes with every element of the stable subset generated by .
Let and be the centralizer and bicentralizer of . They are stable subsets of . Now and and hence (resp. ) contains the stable subset of generated by (resp. ). As every element of commutes with every element of , the proposition follows.
Corollary 1
If and are permutable under the associative law so are and for all integers and ; in particular and are permutable for all and all integers and .
Corollary 2
If all pairs of elements of a subset X are permutable under an associative law T, the law induced by T on the stable subset generated by X is associative and commutative.
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Cited by Corollary 2, I § 4, I § 7. Free monoids, free groups
Theorem 2 (Commutativity theorem)
Let T be an associative law of composition on E; let be a non-empty finite family of elements of E which are pairwise permutable; let B and C be two totally ordered sets with A as underlying set. Then*
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Cited by Theorem 3, Proposition 11, I § 7
Since the theorem is true if A has a single element, we argue by induction on the number of elements in A. Let be an integer > 1 and suppose the theorem is true when Card A < . We prove it for Card A = . It may be assumed that A is the interval in ; the composition of the ordered sequence defined by the natural order relation on A is .
Let A be given another total ordering and let h be the least element of A under this ordering and A' the set of other elements of A (totally ordered by the induced ordering). Suppose first and let P = and Q = ; the theorem being assumed true for A', applying the associativity theorem, we obtain (since )
whence, composing with both sides and repeatedly applying the commutativity and associativity of T:
which proves the theorem for this case. If or , the same result follows, but more simply, the terms arising from P or the terms arising from Q not appearing in the formulae.
Under a commutative associative law on a set E the composition of a finite family of elements of E is by definition the common value of the composition of all the ordered sequences obtained by totally ordering A in all possible ways. This composition will still be denoted by under a law denoted by T; similarly for other notations.
Theorem 3
Let T be an associative law on E and a non-empty finite family of elements of E which are pairwise permutable. If A is a union of non-empty subsets which are pairwise disjoint, then
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Cites Theorem 1 (Associativity theorem), Theorem 2 (Commutativity theorem)
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This follows from Theorem 2 if and are totally ordered so that the satisfy the conditions of Theorem 1.
We single out two important special cases of this theorem:
1. If is a finite family of permutable elements of an associative magma whose indexing set is the product of two non-empty finite sets (a "double family"), then
as follows from Theorem 3 by considering as the union of the sets on the one hand and of the sets on the other.
For example, if has elements and for each all the have the same value , then
If has two elements, we obtain the following results: let be two non-empty families of elements of . If the and the are pairwise permutable, then
Because of formula (7) the composition of a double sequence whose indexing set is the product of two intervals and in is often denoted for a commutative associative law written additively by
and similarly for laws denoted by other symbols.
2. Let be an integer and let be the set of ordered pairs of integers such that and ; the composition of a family (under a commutative associative law) is also denoted by (or simply , if no confusion arises); Theorem 3 here gives the formulae
There are analogous formulae to (7) for a family whose indexing set is the product of more than two sets and analogous formulae to (10) for a family whose indexing set is the set of strictly increasing sequences of integers such that (): in the latter case the composition of the family is denoted by
Proposition 5
Let E and F be magmas whose laws are denoted by T and let f and g be homomorphisms of E into F. Let f T g be the mapping x ↦ f(x) T g(x) of E into F. If F is associative and commutative, f T g is a homomorphism.
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For all elements x and y of E:
6. Quotient laws
Definition 11
Let E be a set. A law of composition T and an equivalence relation R on E are said to be compatible if the relations x ≡ x' (mod R) and y ≡ y' (mod R) (for x, x', y, y' ∈ E) imply x T y ≡ x' T y' (mod R); the law of composition on the quotient set E/R which maps the equivalence classes of x and y to the equivalence class of x T y is called the quotient law of the law T with respect to R. The set E/R with the quotient law is called the quotient magma of E with respect to R.
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To say that an equivalence relation R on E is compatible with the internal law of composition f: E × E → E on E means that the mapping f is compatible (in the sense of Set Theory, II, § 6, no. 5) with the product equivalence relation R × R on E × E and the equivalence relation R on E. (Set Theory, II, § 6, no. 8). This also means that the graph of R is a submagma of E × E.
If the law T is associative (resp. commutative) so is the quotient law (more briefly we say that associativity, or commutativity, is preserved when passing to the quotient).
The canonical mapping from the magma E to the magma E/R is a homomorphism.
For a mapping g of E/R into a magma F to be a homomorphism it is necessary and sufficient that the composition of g with the canonical mapping of E onto E/R be a homomorphism.
The two following propositions are immediate from the definitions:
Proposition 6
Let E and F be two magmas and f a homomorphism of E into F. Let R[x, y] denote the relation f(x) = f(y) between elements x, y of E. Then R is an equivalence relation on E compatible with the law on E and the mapping of E/R onto f(E) derived from f by passing to the quotient is an isomorphism of the quotient magma E/R onto the submagma f(E) of F.
Proposition 7
Let E be a magma and R an equivalence relation on E compatible with the law on E. For an equivalence relation S on E/R to be compatible with the quotient law it is necessary and sufficient that S be of the form T/R where T is an equivalence relation on E implied by R and compatible with the law on E. The canonical mapping of E/T onto (E/R)/(T/R) (Set Theory, II, § 6, no. 7) is then a magma isomorphism.
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Proposition 8
Let E be a magma, A a stable subset of E and R an equivalence relation on E compatible with the law on E. The saturation B of A with respect to R (Set
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Theory, II, , no. 5) is a stable subset. The equivalence relations and induced by on and respectively are compatible with the induced laws and the mapping derived from the canonical injection of into by passing to the quotients is a magma isomorphism of onto
Let denote the law on . If and are two elements of there exist two elements and of such that and ; then and , whence . Thus is a stable subset of and the other assertions are obvious.
Let be a magma and a family of elements of . Consider all the equivalence relations on which are compatible with the law on and such that for all . The intersection of the graphs of these relations is the graph of an equivalence relation which is compatible with the law on and such that . Hence is the finest (Set Theory, III, § 1, nos. 3 and 7) equivalence relation with these two properties. It is called the equivalence relation compatible with the law on generated by the .
Proposition 9
Preserving the above notation, let be a homomorphism of into a magma such that for all . Then is compatible with .
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Let be the equivalence relation associated with . Then for all and is compatible with the law on , hence is coarser than ; this proves the proposition.
Exercises
See the exercises for § 1.