A cesium fountain clock laser-cools a small cloud of cesium-133 atoms, tosses it upward through a microwave cavity, lets it fly freely under gravity, and catches it falling back through the same cavity. Each pass delivers a π/2 microwave pulse tuned near the 9,192,631,770 Hz hyperfine transition — together the two pulses form a Ramsey interferometer.
Free evolution time: T = t_down − t_up
Ramsey signal: P(δ) = ½[1 − cos(2π·Δf·T)]
Fringe half-width: ΔfFWHM ≈ 1 / (2T)
Timing (this sim): t_up,down solved from
½g·t² − v₀·t + h_cavity = 0, g = 9.8 m/s²
- Launch velocity v₀ — sets the fountain's apex height and, crucially, the free-evolution time T between the two microwave pulses. A higher toss (real fountains reach ~1 m) gives a longer T and a narrower, more precise fringe — the whole reason fountains beat tabletop cesium clocks.
- Microwave detuning Δf — how far the interrogation frequency sits from the true 9,192,631,770 Hz resonance. The atoms accumulate a phase 2π·Δf·T between the two pulses, which the second pulse converts into a probability of finding the atom in the excited hyperfine state.
- Cloud temperature — colder atoms (µK-scale, reached by laser cooling) drift less sideways during flight and stay inside the cavity's aperture on the way back down; hotter clouds lose atoms out the sides, lowering the detected fraction and washing out fringe contrast.
- Detected fraction — the share of launched atoms whose transverse thermal drift keeps them inside the cavity aperture at the second pass; this emerges directly from the simulated trajectories, not a fudge factor.
A real cesium clock steers Δf to keep P pinned at the fringe's steepest slope (usually the two half-maximum points, alternating), which is exactly how the SI second is realized and how GPS timing chains stay synchronized.