Phase matching and threshold
Here beta is particle speed divided by vacuum light speed. Below threshold this model emits no rays. We assume the same index at every wavelength.
Neutrinos · D09 · Water and geometry
Set a charged particle’s speed and tilt, then trace its light to a square detector plane. Move the emission point and distinguish a geometric ring from a detector’s finite acceptance.
TEACHING SIMULATION · RECORDED DATA
Preparing a reproducible teaching record…
Physics tutorial
BackgroundThe charged-particle direction lies in the horizontal–normal plane. The detector normal is positive z; horizontal is x, vertical is y. Lengths are metres. The small emission region is at the chosen horizontal offset and z zero.
Why it mattersWhat changes the physical cone, and what only changes the observed footprint?
Start with the essentials
Here beta is particle speed divided by vacuum light speed. Below threshold this model emits no rays. We assume the same index at every wavelength.
The unit ray direction is k. Only forward intersections inside the finite square are recorded. The normal-incidence radius is a reference even when the particle is tilted; it is not a fitted ring radius.
Typical misconceptionA ring is a photograph of a neutrino.
Better mental modelThe geometry describes light from a secondary charged particle. Full neutrino reconstruction also needs interaction kinematics and detector response.
Choose Below threshold. Raise the speed until light appears.
What to observe: The angle begins at zero. The model fixes the number of sampled rays above threshold, so do not infer an absolute light-yield law.Choose Tilted cone and compare the apparatus with the recorded plane.
What to observe: A tilted cone produces a displaced, stretched footprint. Finite acceptance can clip it.Return to a centered ring and double the plane distance.
What to observe: The radius doubles while the opening angle stays fixed, until the square clips the light.