Every essay — page 14
What symmetry decides
Thirty-two classes, enumerated rather than listed — and then the one thing they are for outside crystallography's own bookkeeping: which components of a physical property a crystal is permitted to have before anybody measures it.
Lattices
The repeating scaffold underneath every crystal. Five in the plane, fourteen in space, and no others — a classification with a short proof.
What symmetry decides
Thirty-two classes, enumerated rather than listed — and then the one thing they are for outside crystallography's own bookkeeping: which components of a physical property a crystal is permitted to have before anybody measures it.
Lattices
The repeating scaffold underneath every crystal. Five in the plane, fourteen in space, and no others — a classification with a short proof.
A reduction with one rule
Niggli's reduction is eight numbered conditions with sub-cases, applied in order until none applies. Selling's is a single rule on four vectors that sum to zero: while any of six numbers is positive, do one thing. It terminates sooner, its termination is a quantity that visibly falls, and when it stops the six numbers are the Voronoi cell — the pattern of which ones vanish gives Fedorov's five solids and nothing else.
The halving a lattice will not permit
Admit time reversal and a lattice splits into points that leave the moments alone and points that reverse them. The second set is a coset of a subgroup of index two, and every lattice has exactly seven of those, whatever its shape. What differs is how many of the seven the lattice's own symmetry survives — and the face-centred cubic lattice survives none of them.
Symmetry at work
Crystal forms, twins, domain walls and grain boundaries. Mineralogy, metallurgy and ferroelectrics each worked these out separately, and every one of them turns out to be an orbit or a coset of a group already built here.
Into space
Seventeen becomes two hundred and thirty. Screw axes, glide planes, and the translations that no choice of origin can remove — the operations a flat surface has no room for.
What symmetry decides
Thirty-two classes, enumerated rather than listed — and then the one thing they are for outside crystallography's own bookkeeping: which components of a physical property a crystal is permitted to have before anybody measures it.
Lattices
The repeating scaffold underneath every crystal. Five in the plane, fourteen in space, and no others — a classification with a short proof.
The sum that turns a lattice into its dual
Put a Gaussian on every point of a lattice and add them up. The answer equals the same sum over the dual lattice with the width inverted and the covolume divided out — exactly, to the last bit a double carries, on lattices with no symmetry in them. The identity is free and the reason to have it is that the two sides do not cost the same: at one end of the range the direct sum needs forty thousand terms and the dual sum needs a hundred and twenty-five.
The sum whose answer depends on the shape
Give the points of a cubic lattice alternating signs and add up one over the distance. Added over expanding cubes the total creeps towards 1.747565; added over expanding spheres it does not converge at all, landing on both sides of that number and never settling. The terms are identical and only the order differs. Splitting the sum in two with the theta transformation gives it a value — ten decimal places from a few thousand terms.
Symmetry at work
Crystal forms, twins, domain walls and grain boundaries. Mineralogy, metallurgy and ferroelectrics each worked these out separately, and every one of them turns out to be an orbit or a coset of a group already built here.
The plane a deformation leaves alone
Two differently deformed regions can meet across a plane only if that plane is deformed identically from both sides — which forces the two deformations to differ by a rank-one term. Multiplying each side by its own transpose removes the rotation and leaves a condition on a signature: one positive eigenvalue, one negative, one exactly zero. In that form the classical rule that the middle principal stretch must be one is not quoted but derived, and it says that no single variant of a cubic-to-tetragonal transition can meet its parent at all.
The plate that only fits when it is twinned
No single variant of a cubic-to-tetragonal transition can meet its parent across a plane. A fine mixture of two variants can, because its average deformation carries a free parameter — the volume fraction — and that parameter passes through the compatibility condition twice. Sweeping it gives the two fractions, the two habit planes, and one inequality: the plate exists exactly when the two principal stretches satisfy η₁² + η₃² ≤ 2.
The classification
Exactly seventeen ways to fill the plane with a repeating pattern. Not a fact to memorise: a theorem, with a finite argument and no eighteenth case.
Lattices
The repeating scaffold underneath every crystal. Five in the plane, fourteen in space, and no others — a classification with a short proof.
Operations
Rotations, mirrors, glides and translations — what a symmetry is, how they compose, and why the composition is a group rather than a list.
What symmetry decides
Thirty-two classes, enumerated rather than listed — and then the one thing they are for outside crystallography's own bookkeeping: which components of a physical property a crystal is permitted to have before anybody measures it.
How many axes there are is a Sylow count
Sylow's theorems say that the subgroups of prime-power order in a finite group are all conjugate and that how many there are is congruent to one modulo the prime. Applied to the thirty-two crystal classes that arithmetic counts axes: the number of Sylow 3-subgroups is the number of equivalent threefold directions, it is four in exactly five classes, and those five are the cubic ones. So cubic has a definition with no geometry in it.
The table that decides every action
Burnside's lemma counts orbits and stops there — two completely different actions with the same orbit count are indistinguishable to it. The object that settles the whole question is a square table whose entries count fixed cosets: lower triangular because a subgroup fixes no coset of anything smaller, positive on the diagonal because it fixes its own, and therefore invertible. Inverting it turns a list of fixed-point counts back into the orbits themselves.
Lattices
The repeating scaffold underneath every crystal. Five in the plane, fourteen in space, and no others — a classification with a short proof.
The classification
Exactly seventeen ways to fill the plane with a repeating pattern. Not a fact to memorise: a theorem, with a finite argument and no eighteenth case.
Symmetry at work
Crystal forms, twins, domain walls and grain boundaries. Mineralogy, metallurgy and ferroelectrics each worked these out separately, and every one of them turns out to be an orbit or a coset of a group already built here.
Lattices
The repeating scaffold underneath every crystal. Five in the plane, fourteen in space, and no others — a classification with a short proof.
Symmetry at work
Crystal forms, twins, domain walls and grain boundaries. Mineralogy, metallurgy and ferroelectrics each worked these out separately, and every one of them turns out to be an orbit or a coset of a group already built here.
A polyhedron is two properties of a graph
Steinitz's theorem says a graph is the corner-and-edge graph of a convex polyhedron exactly when it can be drawn in the plane without crossings and stays connected after any two vertices are removed. No lengths, no angles, no convexity — the conditions are about the graph alone, and each one is needed, which four small counterexamples show.
The room a thirteenth sphere would need
Twelve equal spheres touch one, and whether a thirteenth could was argued in 1694 and settled in 1953. The reason it took so long is measurable: the twelve leave three and a half degrees of slack, which is enough room to look promising and not enough to use — and in the plane, where the same question has no slack at all, nobody ever argued.
The point defect whose charge has no sign
A line defect is read on a loop; a point defect is read on a sphere, and the number that comes off the sphere is a degree. In a nematic that degree is an integer whose sign depends on a choice nobody can make — and the media where no such number exists at all are exactly the ones whose residual symmetry is a crystal class.