Dynamo — where it appears
Named by 2 essays across one field — each of them below, with the objects they name alongside it.
The field no symmetric flow can keep
The Earth's core would forget its magnetic field in about forty thousand years, and the field is at least three and a half thousand million years old, so something must be making it again all the time. The obvious candidate is the flow of liquid iron. In 1934 Thomas Cowling proved that the simplest version cannot work: no motion of a conductor, however fast or however arranged, can keep up a field that is symmetric about an axis. The reason is a single ring inside the field where the current it needs cannot be driven.
The dynamo that reverses with nothing pushing it
A copper disc spinning in a magnetic field drives a current from its axle to its rim. Wire that current through a coil wound round the disc and the coil supplies the field the disc needs — and above one definite speed, a resistance divided by an inductance, the arrangement makes its own field out of any stray one, with nothing else magnetic anywhere. It cannot choose which way the field points; the stray field chooses. Couple two such discs, each feeding the other's coil, and with the motors' torque held perfectly steady the field flips direction again and again at intervals that follow no pattern. The simplest dynamo that works is also the simplest one that reverses.
Named alongside it
The objects these essays reach for when they reach for this one.
InductionMagnetic fluxChaosConductivityDissipationFlux freezingGeomagnetic reversalHomopolar generatorMagnetic reynolds numberMean-field theoryResistivitySelf excitation