Hertz to Millihertz

It is largely a historical accident. Early generators in the US settled on 60 Hz because it divided neatly by common motor pole counts and worked well with the 110 V supply Edison promoted. Germany standardized on 50 Hz with a 220 V supply, and colonial-era wiring spread each standard across continents. Changing now would mean replacing every motor, transformer, and clock in the country — so both standards persist.

Concert pitch A4 = 440 Hz was standardized internationally in 1955, but some musicians insist 432 Hz sounds warmer or more natural. There is no physics-based reason 432 is special — it is 8 Hz lower, which shifts every note slightly flat. Historical tuning varied wildly (baroque pitch was often ~415 Hz). The debate is real in music circles, but the claimed health benefits of 432 Hz have no scientific support.

In 1887 Hertz built a spark-gap transmitter and a loop antenna receiver in his lab in Karlsruhe. When the transmitter sparked, the receiver — across the room with no wire connecting them — also sparked. He measured the wavelength and speed, confirming they matched Maxwell's theoretical predictions for light. Hertz was 30 years old. Ironically, he called the discovery of no practical use.

Older magnetic-ballast fluorescent tubes ignite and extinguish twice per mains cycle (100 or 120 times per second) because AC current crosses zero twice per cycle. Most people can't consciously see 100 Hz flicker, but it can cause headaches and eye strain. Modern electronic ballasts drive the tube at 20–40 kHz, eliminating visible flicker entirely.

About 20 Hz under ideal conditions, though sensitivity at that frequency is poor — you need extremely high sound pressure to perceive it. Below 20 Hz is infrasound: you cannot hear it as a tone, but at sufficient intensity you feel it as chest pressure or unease. Pipe organs exploit this: their longest 64-foot pipes produce notes around 8 Hz that you feel more than hear.

After a magnitude-9 earthquake the entire planet vibrates like a struck gong, with its deepest mode at about 0.3 mHz — one oscillation every 54 minutes. The surface rises and falls by fractions of a millimeter. You cannot hear it (human hearing starts at 20 Hz), but gravimeters and seismometers worldwide pick it up. The 2004 Sumatra quake kept Earth ringing measurably for weeks.

Ocean swells, tidal constituents, and seiches (standing waves in harbours or lakes) all oscillate in the millihertz band. A 10-second ocean swell is 100 mHz; a harbour seiche with a 10-minute period is about 1.7 mHz. Monitoring these frequencies helps coastal engineers predict resonance in ports and design breakwaters that don't amplify destructive wave energy.

Not directly — our senses are far too fast. But some physiological rhythms operate here: the Mayer wave, a ~0.1 Hz oscillation in blood pressure, sits at the high end of the millihertz scale, and slower vasomotion (tiny blood vessel contractions) can dip below 10 mHz. You don't feel them as vibrations, but they show up clearly on a continuous blood-pressure monitor.

Infrasound is sound below the ~20 Hz threshold of human hearing. The lowest infrasound blends into the millihertz range — the International Monitoring System for nuclear-test detection listens down to about 20 mHz. Sources include volcanic eruptions, meteor airbursts, severe storms, and ocean microbaroms (standing pressure waves between ocean swells and the atmosphere).

Instruments record a time series (pressure, acceleration, displacement) over hours or days, then apply a Fourier transform to extract frequency content. Superconducting gravimeters can resolve Earth's free oscillations below 1 mHz by measuring gravity changes of 10⁻¹² g. The trick is not a fast sensor but a patient, ultra-stable one and enough data to separate signal from drift.