Simulate neutrino flavor oscillation from source to detector. Measure the νμ→νe conversion probability versus distance L and energy E, verifying P≈sin2(2θ)sin2(1.27Δm2L/E).
Research
Equipment
3D scene from neutrino source to detector
Sliders for distance L and energy E
Illustrative P(νμ→νe) probability readout
Procedure
Observe oscillation with distance
With E fixed, drag "Distance L" and watch the neutrino beam change "flavor color" along its path to the detector. Read the P(νμ→νe) readout: the probability oscillates periodically in L — the signature of two mass states accumulating different phases Δm2L/(2E).
Vary the energy
At fixed L, sweep "Energy E": the probability oscillates in 1/E — the oscillation wavelength scales as Losc∝E/Δm2. Record the peak/trough positions of P versus E and compare with P≈sin2(2θ)sin2(1.27Δm2L/E) (L in km, E in GeV, Δm2 in eV²).
Reset the phase and check the maximum
Press "Reset phase" then choose L so that 1.27Δm2L/E=π/2 — the conversion probability reaches its maximum sin2(2θ). Compare two settings (small L, large E) and (large L, small E) with the same L/E ratio: the oscillations match — only the ratio L/E sets the phase.
Simulation
Experiment history
The neutrino was proposed by Wolfgang Pauli in 1930 to rescue energy conservation in β decay; Pauli himself called it undetectable — yet Reines and Cowan captured antineutrinos in 1956 with a water tank near a reactor. Bruno Pontecorvo (1957–68) proposed that neutrinos could oscillate between flavors if they carry different masses.
The "solar neutrino deficit" recorded by Raymond Davis at Homestake (from 1968) — only ~1/3 of the predicted νₑ flux — was resolved when Super-Kamiokande (Koshiba, 1998) saw atmospheric-neutrino oscillation and SNO (McDonald, 2001–02) proved νₑ convert into νμ/ντ. The 2015 Nobel Prize went to Kajita and McDonald. Oscillation proves neutrinos have mass — the first crack in the Standard Model.