A piece of material in which the atoms are lined up in one unbroken pattern from one side to the other, with every row pointing the same way. Most solids are not like that: they are , made of many small crystals stuck together at random angles, like a pavement of tiles laid every which way. The boundaries between those grains scatter electrons, weaken the material and blur measurements, so physics experiments and the best devices want single crystals – a centimetre-sized block to peel from, or a sheet grown across a whole in one orientation.
Going deeper
In a single crystal one pattern runs unbroken through the whole piece; a polycrystal is a patchwork of grains at random angles whose boundaries scatter electrons. Single-crystal films are grown from islands that all point the same way and merge seamlessly; islands of two orientations meet in twin walls.
One crystal, or many
When a melt freezes or a film grows, crystals usually start at many points at once. Each grows with its own orientation until it meets its neighbours, and the result is polycrystalline: many grains joined at boundaries where the rows of atoms do not match. A single crystal results when only one of them is allowed to grow – by seeding with a small crystal, by letting a narrow tip select one grain as in , or by growing so slowly from a vapour or a solution that only a few crystals form.
For layered materials, single crystals are where most experiments begin. A crystal of MoS2, CrI3 or Bi2Se3 a few millimetres or centimetres across, grown by or from a flux, is peeled into flakes, and each flake is a single crystal too, as long as its parent was.
Why it matters
Grain boundaries scatter electrons and , trap charge, let chemicals in and can carry electronic states of their own, so a polycrystalline film usually has a lower and more variation from device to device than a single crystal. For delicate effects – quantum oscillations, unconventional , fragile – the difference decides whether anything is seen at all. Only a single crystal lets a property be measured along a chosen crystal direction, which layered materials need.
A crystal can be single and still imperfect. Twins, and mixed hide inside crystals that look flawless, so with narrow rocking curves, the of metals and microscopy across the sample are the usual checks.
Single-crystal films
Growing one crystal across a whole wafer from a single nucleus would be far too slow, so large single-crystal films are grown from many nuclei that all point the same way and merge without boundaries. The supplies the alignment. A copper (111) or germanium (110) surface aligns graphene; sapphire or copper cut at a slight angle, so that its surface carries regular atomic steps, aligns MoS2 and hBN in a single direction, removing the mirror-image orientation whose domains would otherwise meet in twin boundaries. Films of this kind have reached wafer size in research laboratories.
For specialists
A solid whose lattice is continuous and uniformly oriented throughout, without grain boundaries – unlike polycrystalline material, made of misoriented grains, or amorphous solids without long-range order. Bulk single crystals of layered compounds are grown by chemical vapour transport, flux or Bridgman methods and are the usual source of exfoliated flakes; their quality is judged by X-ray rocking-curve widths, the residual resistivity ratio and the absence of twins and stacking faults. Large single-crystal films grow either from one nucleus or from aligned nuclei that merge without boundaries, as for graphene on Cu(111) or Ge(110) and MoS2 or hBN on vicinal sapphire or copper, where substrate steps fix one orientation and remove the twin boundaries that two antiparallel orientations would form.