A scale is a monotonically increasing trajectory through log‑frequency space. Continuous, discrete, periodic, or none of the above. Everything below is piecewise.
t in note-space [0, 1]. The rate of increase is unconstrained — only the direction is.S(t + T) = S(t) + log2(r).A monotonic map t → log‑frequency is an inverse CDF.
Treating t as uniform on [0, 1], the scale becomes a draw from a
distribution over log‑frequency with density p(log f) = 1 / S'(t).
Slow-rise regions are high-density (stable pitches); fast-rise regions are
low-density (transition pitches).
| Scale property | Distribution interpretation |
|---|---|
| Slow-rise segment | High-density — "stable" pitches |
| Fast-rise segment | Low-density — "transition" pitches |
| Plateau (discrete) | Delta spike — a point mass at one pitch |
| Periodic, octave ratio | Density is octave‑equivalent on log‑pitch |
| Continuous aperiodic | Arbitrary continuous density |
| Major scale | Seven delta spikes, repeating each octave |
| Log‑linear sweep | Uniform density over log‑frequency |
In the trio below: the bass lives in slow-rise zones (it sounds anchored);
the lead lives in fast-rise zones (small p-movements become wide
pitch sweeps, so it reads as expressive). That alignment of voice-role to
density-region wasn't planned — it's why the piece holds together.
Each scale maps note‑space t (horizontal) to frequency (vertical, log‑scaled).
Periodic scales repeat by frequency‑doubling; discrete scales step; continuous scales bend.
Three theremin voices share one continuous aperiodic scale. Each voice is a trajectory through note‑space; played together they form a chord trajectory, with arpeggio passages where one voice carries the line.