Tilted double well
The symmetric barrier scale is measured from either minimum. With tilt, the displayed release-side barrier is recomputed from actual stationary points.
M045 · Barrier / critical slowing
Tune the barrier, well spacing, asymmetry and damping. Compare confined oscillations with inter-well motion, approach the separatrix from both sides and capture an energetic particle through dissipation. Measure crossings and periods against independent energy quadrature.
Physics tutorial
BackgroundA quartic double well has two stable minima and a saddle between them. Below the saddle energy, a conservative particle remains on one side. Above it, the allowed interval connects both wells. At critical energy, a nonstationary separatrix approaches the saddle asymptotically rather than completing a periodic orbit.
Why it mattersThe energy and phase-space construction follows classical one-coordinate mechanics. The barrier threshold and tilt limit here are derived directly from the displayed quartic potential. The viscous model books every removed kinetic-energy increment.
Start with the essentials
The symmetric barrier scale is measured from either minimum. With tilt, the displayed release-side barrier is recomputed from actual stationary points.
The slider stays below the saddle-node threshold; the two minima and intervening saddle remain distinct.
Exponential viscous substeps account for their exact kinetic-energy loss. Conservative step error remains visible in the balance defect.
The critical orbit has no finite period. The plot leaves a gap instead of connecting the below- and above-barrier branches.
Logarithmic period growth near the saddle amplifies small energy errors. Exact saddle release remains at rest without perturbation.
Typical misconceptionEvery recorded crossing at critical energy is physical.
Better mental modelThe exact separatrix does not cross the saddle in finite time. Finite-step error can change its topology; compare energy and half-step defects.
Typical misconceptionThe symmetric barrier parameter always equals the launch-side barrier height.
Better mental modelTilt changes the energies of both minima and the saddle; the readout uses their actual difference.
Typical misconceptionThe conservative reference period remains the measured period after energy loss.
Better mental modelDissipation changes the instantaneous orbit. Capture is certified only after acquired energy lies below the saddle beyond numerical uncertainty.
Acquire trapped and crossing presets, then inspect phase space and acquired saddle events.
What to observe: Only above-barrier conservative motion connects the two wells.Compare near-below and near-above presets, then select critical energy.
What to observe: Both periods grow; the critical reference reports no finite period and its numerical sensitivity grows sharply.Acquire the dissipative-capture preset and inspect heat plus mechanical energy.
What to observe: The energy ledger closes while the orbit eventually becomes enclosed on one side.Change tilt and drag the release in phase space; compare actual saddle energy with the symmetric scale.
What to observe: The saddle moves and the two launch-side barriers differ even though both minima persist.