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Tour of selected equations
Equation 1 x = x: the trivial law
This is the weakest law, satisfied by all magmas. No other law is equivalent to this law.
Equation 2 x = y: the singleton law
This is the strongest law, satisfied only by the trivial magmas: the singleton and empty magmas. Many laws are equivalent to this law; informally, they are so ``overdetermined'' that they can only be satisfied by trivial magmas. In fact, from our list of 4694 laws, exactly 1495 other laws are equivalent to this one.
Equations 14 x = y ◇ (x ◇ y), 29 x = (y ◇ x) ◇ y: 2001 Putnam laws
Problem A1 of the 2001 Putnam asked to show (in our language) that Equation 14 implies Equation 29. In fact, the two laws are equivalent.
Equation 43 x ◇ y = y ◇ x: the commutative law
One of the most famous laws in all of algebra.
Equation 46 x ◇ y = z ◇ w: the constant law
A very strong law, that makes the entire multiplication table constant.
Equations 65 x = y ◇ (x ◇ (y ◇ x)) "Asterix", and 1491 x = (y ◇ x) ◇ (y ◇ (y ◇ x)) "Obelix"
A surprisingly subtle pair of equations to analyze, see this discussion. The "Asterix" equation implies the "Obelix" equation for finite magmas, but not for infinite ones; similarly for the converse implication. The analysis of this pair led us to develop "greedy" methods for constructing counterexamples, which has turned out to be a fruitful and flexible approach that (after suitable modifications) resolved many other challenging implications.
Equation 168 x = (y ◇ x) ◇ (x ◇ z): the central groupoid law
This law defines central groupoids, which are magmas with some interesting combinatorial structure. For instance, all finite central groupoids have a cardinality that is necessarily a square number. This paper of Knuth establishes many of the basic properties of these objects.
Equations 381 x ◇ y = (x ◇ z) ◇ y, 3722 x ◇ y = (x ◇ y) ◇ (x ◇ y), 3744 x ◇ y = (x ◇ z) ◇ (w ◇ y): 1978 Putnam laws
Problem A4 of the 1978 Putnam asked to show (in our language) that Equation 3744 implies Equations 3722 and 381. This Putnam question referred to 3744 as a "bypass law".
Equation 387 x ◇ y = (y ◇ y) ◇ x: a law from MathOverflow
This response by pastebee to a MathOverflow question established that there was an equational law strictly between the constant law 46 and the commutative law 43, namely Equation 387.
Equation 477 x = y ◇ (x ◇ (y ◇ (y ◇ y))): a confluent law
This law is a non-trivial example of a confluent law: a law in which every word has a unique shortest reduction using the law. This makes it possible to easily determine which other equations are implied by this law, giving anti-implications that were not obtainable by other means. See this discussion.
Equation 543 x = y ◇ (z ◇ (x ◇ (y ◇ z))): Tarski's axiom
In 1938, Tarski showed that this law describes abelian groups: a magma obeys this law if and only if it has the structure of an abelian group, for which the magma operation is given by subtraction: x ◇ y = x - y.
Equation 854 x = x ◇ ((y ◇ z) ◇ (x ◇ z)): A "liquid" law.
Most laws tend to feel either "solid", in that their models have a lot of algebraic structure (or are forced to be almost trivial), or "gaseous", in that there is extensive freedom in their models, and little structure. This law is at an unusual intermediate state, that one might call "liquid". One the one hand, it implies many other laws and its models have intriguing structure, including a an associated directed graph and pre-order. Its free magma, while difficult to describe, does obey some interesting laws, such as a unique factorization property that can already be used to refute some implications. On the other hand, there are many sporadic solutions, including a specific example of order 12 that was discovered through an ATP and could also refute implications. Furthermore, given a finite magma solving this law, it is often possible to extend it by adding one more element, in sharp contrast to say the situation with finite groups, creating quite a large class of additional examples of this law.
Equations 917 x = y ◇ ((y ◇ y) ◇ (x ◇ y)) "Hardy", 1729 x = (y ◇ y) ◇ ((y ◇ x) ◇ y) "Ramanujan", and 2541 x = (y ◇ ((y ◇ y) ◇ x)) ◇ y "Littlewood"
Three closely related equations. They are known to be equivalent for finite magmas. For infinite magmas, Ramanujan implies Littlewood, but the other five implications between these laws are now known to be false (with rather sophisticated counterexamples in some cases).
Equation 1485 x = (y ◇ x) ◇ (x ◇ (z ◇ y)): the weak central groupoid law
A weaker form of the central groupoid law (Equation 168). Has some intriguing structure; for instance, all known finite examples have cardinality that is either a perfect square, or twice a perfect square, and such weak central groupoids can be associated to a directed graph obeying an intriguing axiom on its 5-cycles. A specific such example, of order 32, has led to the development of a "twisting semigroup" method that can rule out a small number of select implications. Discussed extensively here.
Equation 1571 x = (y ◇ z) ◇ (y ◇ (x ◇ z)): a law for abelian groups of exponent 2
It was shown by Mendelsohn and Padmanabhan that this law characterizes abelian groups of exponent 2.
Equation 1689 x = (y ◇ x) ◇ ((x ◇ z) ◇ z): a non-trivially singleton law
This law was identified by Kisielewicz as a law that collapses to the singleton law 2, but all known proofs are surprisingly lengthy.
Equation 4512 x ◇ (y ◇ z) = (x ◇ y) ◇ z: the associative law
One of the most famous laws in all of algebra.
Equations 3588 x ◇ y = z ◇ ((x ◇ y) ◇ z), 3994 x ◇ y = (z ◇ (x ◇ y)) ◇ z: An Austin pair
It was shown as part of this project that 3944 and 3588 form an "Austin pair": Equation 3944 implies Equation 3588 for finite magmas, but not for infinite magmas.
An Austin law is a law which has infinite models, but no non-trivial finite models (equivalently, this law and the trivial law (Equation 2) form an Austin pair). Kisielewicz showed that this law has no non-trivial finite models, but it remains open whether there is an infinite model.
It was shown by Knuth that this law characterizes "natural central groupoids", which, up to isomorphisms, are Cartesian squares S × S with magma operation (a,b) ∘ (c,d) = (b,c). These are special cases of central groupoids (Equation 168).
Kisielewicz showed that this law is an Austin law: it has no non-trivial finite models, but it has an infinite model. He also showed there is no shorter Austin law.
It was shown by McCune, Veroff, Fitelson, Harris, Feist, and Wos that this law defines the Sheffer stroke.
It was shown by Kisielewicz that this law is an Austin law: it has no non-trivial finite models, but it has an infinite model.
The second law of a Jordan algebras. (The first is the commutative law, Equation 43.)
Equations 910472 x ◇ (y ◇ (x ◇ z)) = (x ◇ (y ◇ x)) ◇ z, 930594 x ◇ ((y ◇ z) ◇ y) = ((x ◇ y) ◇ z) ◇ y, 914612 x ◇ (y ◇ (x ◇ z)) = ((x ◇ y) ◇ x) ◇ z, 916037 x ◇ (y ◇ (z ◇ y)) = ((x ◇ y) ◇ z) ◇ y, 936498 (x ◇ y) ◇ (z ◇ x) = (x ◇ (y ◇ z)) ◇ x, 921941 x ◇ ((y ◇ z) ◇ x) = (x ◇ y) ◇ (z ◇ x): the Bol-Moufang axioms
The first two equations 910472, 930594 are the axioms for left and right Bol loops (if one also assumes the loop axiom that an identity element exists). A Moufang loop is a loop that is both left Bol and right Bol; this is equivalent (for loops) to any one of the other four equations 914612, 916037, 936498, 921941 holding.
This axiom characterizes division in a (not necessarily abelian) group, as was worked out by Higman and Neumannin in 1956. It is one of the shortest such axioms.