The nuclear configuration plane
Cyan indicates the lower energy surface, coral the upper. The total brightness is square-root density with a fixed scale. These are nuclear coordinates, not electron tracks.
TWO SURFACES / ONE WAVEPACKET
Send a nuclear wavepacket toward a two-state conical intersection. Compare a central arrival, an off-centre passage and a zero-mixing control using surface populations and independently sampled configurations.
LOWER ENERGY SURFACE POPULATION
EVOLUTION TIME
READ THE PROBABILITY
Cyan indicates the lower energy surface, coral the upper. The total brightness is square-root density with a fixed scale. These are nuclear coordinates, not electron tracks.
Solid cyan: local lower-surface population. Dashed violet: fixed channel A population. These are different projections. Gold is the pinned lower-surface population.
INDEPENDENT SIMULATED MEASUREMENTS
Sample nuclear configuration and fixed electronic channel from each of 768 independent preparations. Violet dots are channel A; gold dots are B. These are fixed electronic channels, not energy surfaces.
Ideal joint position readout, without blur or loss. Moving the time cursor preserves old records; changing preparation clears them. Samples are not a wavefunction reconstruction or a continuous movie of one molecule.
Length, time and energy are dimensionless. No specific molecular mass or experimental time scale is assigned. Positive stretch points outward; in the two-coordinate model the second coordinate is positive upward in the flat map.
The full two-component state is propagated in a fixed diabatic basis. Lower-surface density uses the local spectral projector; at an exactly degenerate grid point its weight is assigned equally. Setting mixing to zero removes electronic-channel transfer and changes the point intersection to a line crossing. No claim of measuring a Berry phase is made.
A periodic Fourier grid and symmetric split-step propagation solve the declared Hamiltonian. No absorption or propagation renormalization is used. Edge occupation, high-wave-number weight and relative energy drift are checked; the view warns if the chosen run loses numerical resolution.
Sources establish the model context; this illustrative parameter set is not a fit or a reproduction of those experimental data.
Physics tutorial
BackgroundSend a nuclear wavepacket toward a two-state conical intersection. Compare a central arrival, an off-centre passage and a zero-mixing control using surface populations and independently sampled configurations.
Why it mattersConnect the energy landscape to the changing probability, then ask what a measurement actually records.
Start with the essentials
Dimensionless units set the effective mass and reduced Planck constant to one. All propagation is unitary; no time-step renormalization is used.
With nonzero mixing the surfaces meet at one point. Setting mixing to zero produces a crossing line, so it changes the model geometry as well as the dynamics.
Typical misconceptionThe bright spot is one atom moving on a literal surface.
Better mental modelIt is a nuclear configuration probability. Energy is plotted vertically only as a visualization.
Typical misconceptionThe simulation predicts a particular molecule.
Better mental modelDimensionless two-coordinate linear vibronic-coupling model, evolved as a two-component wavefunction. The axes are nuclear configuration coordinates; height is electronic potential energy. This is not an atom trajectory, a particular molecular reaction or a direct measurement of geometric phase.
Start with the first two presets and select the same time in both. Pin a frame before changing the preparation.
What to observe: An off-centre preparation changes both the spatial pattern and the populations.Switch between landscape and density views, then inspect the data row.
What to observe: Potential height, density brightness and probability relief are distinct quantities with explicit display scales.Sample independent preparations at one chosen instant. Move time and confirm the old records stay fixed. Export the raw CSV.
What to observe: A finite sample fluctuates. It does not reconstruct the complex wavefunction or reveal a continuous path.