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Sandbox Physics

M045 · Barrier / critical slowing

Double-Well, Barrier & Separatrix Lab

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.

Interactive modelDouble-Well, Barrier & Separatrix Lab
Acquired time0 s0\,s
Position0 m0\,m
Velocity0 m s−10\,\mathrm{m\,s^{-1}}
Conservative force0 N0\,N
Potential energy0 J0\,J
Kinetic energy0 J0\,J
Mechanical energy0 J0\,J
Dissipated energy0 J0\,J
Current energy balance defect0 J0\,J
Full-record maximum balance defect0 J0\,J
Half-step displacement difference · first ten seconds0 m0\,m
Actual integration step0 ms0\,ms
Nearest release-side minimum0 m0\,m
Local undamped angular frequency0 rad s−10\,\mathrm{rad\,s^{-1}}
Allowed regions at release energy11
Release-region left boundary0 m0\,m
Release-region right boundary0 m0\,m
Conservative quadrature period0 s0\,s
Last acquired full turn intervalAwait turns\text{Await turns}
Period quadrature resolution difference0 s0\,s
Measured minus conservative period0 s0\,s
Acquisition statusComplete\text{Complete}
Barrier above nearest release-side minimum0 J0\,J
Saddle position0 m0\,m
Current energy above saddle0 J0\,J
Acquired numerical saddle crossings00
First acquired numerical crossingNot acquired\text{Not acquired}
Release energy classificationAbove barrier\text{Above barrier}
Acquired dissipative enclosureUnconfirmed\text{Unconfirmed}

Physics tutorial

A separatrix separates confined and crossing orbits

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

Focus question
Why does crossing a little above the barrier take so much longer?
One-sentence intuition
The particle spends an increasing time near the saddle as its energy approaches the barrier. Damping can remove enough energy to disconnect a previously crossing orbit.

Core mathematical model

Tilted double well

U(x)=B[(xa)2−1]2+fxU(x)=B\left[\left(\frac{x}{a}\right)^2-1\right]^2+fx

The symmetric barrier scale is measured from either minimum. With tilt, the displayed release-side barrier is recomputed from actual stationary points.

Persistence of two minima

∣f∣<fcrit=8B33 a,U′(x∗)=0|f|<f_{\mathrm{crit}}=\frac{8B}{3\sqrt3\,a},\qquad U\prime(x_*)=0

The slider stays below the saddle-node threshold; the two minima and intervening saddle remain distinct.

Viscous energy ledger

mx¨=−U′(x)−cx˙,H(t)+Q(t)=H(0),Q(t)=∫0tcx˙2 dtm\ddot x=-U\prime(x)-c\dot x,\qquad H(t)+Q(t)=H(0),\qquad Q(t)=\int_0^t c\dot x^2\,dt

Exponential viscous substeps account for their exact kinetic-energy loss. Conservative step error remains visible in the balance defect.

Barrier and conservative period

ΔH=H−U(xs),T(H)=2m∫x−x+dxH−U(x)\Delta H=H-U(x_s),\qquad T(H)=\sqrt{2m}\int_{x_-}^{x_+}\frac{dx}{\sqrt{H-U(x)}}

The critical orbit has no finite period. The plot leaves a gap instead of connecting the below- and above-barrier branches.

Local saddle dynamics

U(x)≃U(xs)−mλs22(x−xs)2,λs2=−U′′(xs)mU(x)\simeq U(x_s)-\frac{m\lambda_s^2}{2}(x-x_s)^2,\qquad \lambda_s^2=-\frac{U\prime\prime(x_s)}{m}

Logarithmic period growth near the saddle amplifies small energy errors. Exact saddle release remains at rest without perturbation.

Common difficulties

Crossing is a numerical observation

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.

A tilted scale is not the actual barrier

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.

Damping changes the orbit

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.

Run the experiment

  1. 01

    Compare both topologies

    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.
  2. 02

    Approach the boundary

    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.
  3. 03

    Capture by dissipation

    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.
  4. 04

    Tilt without erasing a well

    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.