Gravity length
About 5.87 micrometers at Earth gravity.
Q017 · Mirror / absorber / neutron counts
Lift an absorber above a horizontal mirror. Record neutrons at each height and compare a four-state mixture with a prepared ground state. Change the flight time to see why the transmission edge is not an energy level.
02 / FIRST THE COUNTS. THEN THE CURVE.
· Blue: current records. Amber: last saved other sample. Dashed: optional model. Drag to inspect; the slider supports keyboard input.
AT THIS PROBE SETTING
No recorded particles yet.
95% pointwise Wilson interval. No simultaneous-band or optional-stopping guarantee.
LATEST 60 RAW OUTCOMES
Blue: transmitted. Gray: reflected or absorbed. No hidden trajectory is recorded.
03 / WHAT CAN THESE RECORDS TELL US?
Model only: each bar shows its contribution before and after the absorber. Absorption changes populations, not the energy markers.
FIRST OBSERVED HALF-TRANSMISSION CROSSING
MODEL INSPECTION · NO NEW RECORDS
· Drag the absorber. Gray: incoming density. Blue: surviving unnormalized density per incident neutron. Orange markers: classical turning heights.
· Numerical hard-mirror eigenstates. The incoming state mixture has only the first four modes.
04 / KEEP THE EVIDENCE
Eight frozen samples. Restoring inspects the original records; acquiring again starts a new run. CSV contains individual outcomes, scan membership and original settings.
The ground-state scale uses the neutron mass and SI constants. A 360-point finite-difference solution extends to eighteen gravity lengths. The absorber is a diagonal phenomenological loss channel proportional to each unperturbed mode’s probability above the gap; it does not impose a second hard wall. Coherent mixing, distorted eigenstates, real roughness, energy-dependent material absorption, loading efficiency and neutron decay are omitted. Preparation is ideal and the detector has unit efficiency. Geometry magnification is anisotropic; vertical position is a probability distribution, never a hidden ballistic track.
Nesvizhevsky et al. · mirror, absorber and transmitted neutrons · Voronin et al. · absorbing waveguide and limits of a simple loss model
Physics tutorial
BackgroundLift an absorber above a horizontal mirror. Record neutrons at each height and compare a four-state mixture with a prepared ground state. Change the flight time to see why the transmission edge is not an energy level.
Why it mattersA boundary changes the allowed wave, and a detector records only a sample.
Start with the essentials
About 5.87 micrometers at Earth gravity.
The positive Airy zeros set energies. The probability density extends beyond the classical turning height.
A phenomenological diagonal loss channel, not a solution of a rough absorbing waveguide. The mirror length is twelve centimeters.
Typical misconceptionNeutrons occupy discrete height shelves.
Better mental modelEnergies are discrete; each state has a continuous density. The detector records only survival through an absorber.
Typical misconceptionAgreement here certifies a real device.
Better mental modelUltracold neutrons above an ideal hard mirror in uniform gravity. Four incoherent prepared vertical states; a declared overlap-loss model removes population during horizontal flight. Absorber-induced state distortion, roughness scattering and mode mixing are omitted. Density is continuous in height; turning heights are not shelves for particles.
Choose the four-state mixture. Predict whether a wider slit can lower the transmission.
What to observe: Keep the reference curve hidden until after recording.Scan heights and save. Prepare only the ground state and repeat.
What to observe: Frozen samples retain the settings that produced them.Increase horizontal speed at the same height. The state energies remain fixed, but less flight time means less loss.
What to observe: A half-transmission height is an operational statistic, not an energy measurement.