The Mullins cyclotron used a cheap, uncalibrated Hall-effect meter (one never checked against a known field) to establish the approximate field, then varied the magnet current to find reproducible beam-current peaks; a second peak appeared at 427 mT (build log, “It works!”). The second peak, at twice the field, was the hydrogen molecular ion H₂⁺, a hydrogen molecule missing one electron and so twice the mass on the same charge.
If it does not work. Separate three jobs: measuring how the field varies with position; knowing its absolute magnitude; finding the resonance by watching the machine respond. For the first two, read the cheap meter with the RF off; the Mullins log made that a
standing rule after one coil change (hosted instrumentation note). Keep the probe flat against a
reference surface, since a Hall element reads only the part of the field perpendicular to its face and a tilted probe therefore reads low. Cycle
the magnet to the same maximum each time so the field-against-current curve repeats (Zickler (2010), p. 26).
If you suspect the field changes too much across the magnet, measure it at several positions between the poles. Start near the center and move the probe outward toward the edge, recording the field every centimetre or so; then repeat in another direction, toward twelve o’clock and toward three o’clock, say. That shows whether the field gets weaker toward the edge, as it should slightly for the vertical focusing, and whether one side of the magnet behaves differently from another. Houghton did this with a Hall probe on a rotating aluminium jig at 1 cm steps (Loucks (2007), p. 36-38), and a more detailed analysis of such readings reveals problems with particle focusing (magnet-design page). How the Mullins experiment was recorded is one way to do the sweep, not a requirement: a slow triangle ramp from a function generator into the magnet supply’s analog input, with an oscilloscope in XY persistence plotting field against electrometer current (hosted instrumentation note). The electrometer is the sensitive current meter on the collector. If a once-around pattern dominates a circle, the field high on one side and low opposite, check pole parallelism, since tilted poles produce exactly that, and the
jig’s pivot before shimming anything, that is, before adding iron to correct the field (Livingston & Blewett (1962), p. 197-284). For the third job, the Mullins remedy for a resonance that was easy to miss, since the peak is narrow, was to set the field near the expected value, tune the RF frequency for maximum DC current at the collector, and only then sweep (hosted instrumentation note).
To understand it. The map a magnet designer wants has four parts. Field against current at the center. The radial profile and its index n(r). Circles at two or three radii, including the collector radius, to size the once-around variation (Livingston & Blewett (1962), p. 197). And the magnetic midplane, the plane about which the field is symmetric, found with a pair of opposed search coils; it sat half an inch off the geometric midplane at MIT (Livingston & Blewett (1962), p. 197). Measure with the chamber in place if its lids are steel, because steel lids become part of the poles. Houghton’s modelled magnetic lids moved the n = 0.2 radius outward by centimetres (Morrow (2015)). Rutgers found the normalized profile, the field at each radius divided by the field at the center, unchanged across 20, 30 and 40 A of magnet current on its 12-inch
(Koeth (2006), p. 3), which is worth checking. A calibrated Hall probe can serve both the mapping and the absolute roles. For accuracy beyond it, the classical reference is proton NMR, whose resonance frequency is set by the field alone, at 234.82 G per MHz (Livingston & Blewett (1962), p. 286-287, McGuire (1961), p. 9-10). The species is which ion it is; the harmonic is whether the RF runs at the ion’s own frequency or an odd multiple of it. Once the beam’s species and harmonic
are established, the resonance frequency constrains the orbit-averaged field more tightly than
any meter (magnet-design page); until they are, a peak is a candidate. Artifacts: position error multiplies by the local gradient and dominates at the edge (Livingston & Howard (eds.), p. 31). Probe settling and backlash, play in the positioning mechanism, need handling (Koeth & Krutzler (2015), p. 3, Koeth & Krutzler (2015), p. 2). A feature that repeats at two excitations (two magnet currents) is likely the magnet’s, though a repeatable positioning or calibration error survives the same test (Alford (1961), p. 11).
Which number goes where. Into the frequency: the azimuthal average of the field at the radius in
question, the average round the circle, which the ion samples whole on each turn, so the resonance is found by sweeping rather than computing (Livingston & Blewett (1962), p. 156). Into the
energy: the field at the final orbit radius, inside the usable region about half a gap inside the
pole edge (Livingston & Blewett (1962), p. 158, Livingston & Blewett (1962), p. 260). Into the focusing check: n(r). Into the centering check: the
once-around at the collector radius.