The emitter below and the reflector above trap a standing wave of sound in the gap. Where the wave is still — the pressure nodes — the beads can rest, held up against gravity. The scope shows the same wave as a line of light.
The emitter below and the reflector above trap a standing wave of sound in the gap. Where the wave is still — the pressure nodes — the beads can rest, held up against gravity. The scope shows the same wave as a line of light.
Sound is a wave of pressure moving through the air. Aim a strong enough wave at a hard surface and it bounces straight back. The wave going up and the wave coming down overlap — and where they meet just right, they lock into a standing wave: a pattern that no longer travels, with fixed points that heave and fixed points that stay perfectly still.
The still points are the nodes. At a node, the air is calm, but just above and below it the pressure pushes inward. A small, light object — a fleck of Styrofoam — dropped into that pocket gets squeezed from every side and held there, floating, against gravity. This is acoustic levitation. Over the last century physicists turned it into a real tool; it is now used to hold droplets and samples in mid-air with nothing touching them at all.
A standing wave only forms if the round trip fits. The gap between emitter and reflector must be a whole number of half-wavelengths. Hit that, and the wave locks; the beads rise. Miss it, and the reflected wave fights the outgoing one — the pattern drifts, and the beads fall. In this lab you tune it by hand: drag the reflector and watch for the lock.
The scope is an oscilloscope — an instrument built around a tube that paints a moving signal as a glowing line. It is the electrical cousin of Chladni's sand: a way to take a wave you cannot see and draw it where you can. On the trace, the nodes are the points that never move.
A standing wave is not a laboratory trick. Once you can see one, you start noticing them everywhere.
And the oscilloscope is in every electronics bench on Earth, for the same reason Chladni scattered sand: you cannot fix a wave you cannot see.
A browser physics lab pairing an ultrasonic levitation chamber with an oscilloscope read-out. Tune the gap, find the lock, and watch the beads rise into the nodes of a standing wave.
The wavelength is computed honestly: λ = c / f, with the speed of sound c = 343 m/s. Pressure nodes sit half a wavelength apart. The gap is "tuned" when it equals a whole number of half-wavelengths — the real boundary condition for a standing wave between two hard surfaces. Raise the frequency and the wavelength shrinks, so more nodes fit in the same gap and more beads can be held. The four drive frequencies (25–40 kHz) are in the real range used by ultrasonic levitators.
Lab 2 of the OPA Browser Physics Suite · ELUSK College of Engineering. Sibling to the Chladni Plate Lab. Built by Travis Jenkins / User Zero. Educational use. No tracking, no backend, no data stored.