crystal defect

crystal defects(Top left) A perfect crystal with a lattice of alternating positive (yellow) and negative (blue) ions. (Middle left) Frenkel defect, with a single ion displaced from its normal lattice point to a nearby interstice, or space, between atoms in the lattice. (Bottom left) Schottky defect, in which both a positive and negative ion have left the lattice. (Top center) Impurity defect, in which either a foreign atom has replaced one in the lattice, or a foreign atom has squeezed into an interstice. (Bottom center) Line defect, in which a new row of atoms is squeezed into the lattice. (Right) Surface defect, in which grains, or smaller crystals within the main crystal, have their rows of atoms misaligned.

crystal defect, imperfection in the regular geometrical arrangement of the atoms in a crystalline solid. These imperfections result from deformation of the solid, rapid cooling from high temperature, or high-energy radiation (X-rays or neutrons) striking the solid. Located at single points, along lines, or on whole surfaces in the solid, these defects influence its mechanical, electrical, and optical behavior.

Point defects include the Frenkel type, the Schottky type, and the impurity type. The Frenkel defect involves a single ion, which is displaced from its normal lattice point and shifts to a nearby interstice, or space, between atoms in the lattice. In the Schottky defect, two ions of opposite sign leave the lattice. Impurity defects are foreign atoms that replace some of the atoms making up the solid or that squeeze into the interstices; they are important in the electrical behavior of semiconductors, which are materials used in computer chips and other electronic devices.

Line defects, or dislocations, are lines along which whole rows of atoms in a solid are arranged anomalously. The resulting irregularity in spacing is most severe along a line called the line of dislocation. Line defects can weaken or strengthen solids.

Surface defects may arise at the boundary between two grains, or small crystals, within a larger crystal. The rows of atoms in two different grains may run in slightly different directions, leading to a mismatch across the grain boundary. The actual external surface of a crystal is also a surface defect because the atoms on the surface adjust their positions to accommodate for the absence of neighboring atoms outside the surface.

The Editors of Encyclopaedia Britannica This article was most recently revised and updated by Erik Gregersen.