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Sandbox Physics

M045 · Barriers and critical slowing

Double-Well, Barrier & Separatrix Lab

How does a barrier between two wells change the way a particle moves? It depends on whether the energy clears the barrier. Below the top, the particle rocks back and forth in one well; above it, the particle runs between both wells. Close to the dividing energy it crawls past the top of the barrier, so the period becomes very long. Damping can drain just enough energy to trap a particle that used to cross.

Set the barrier, the well spacing, the tilt and the damping. Compare a particle trapped in one well with one that crosses between wells, approach the separatrix from below and from above, and let damping capture a fast particle on one side. Measure crossings and periods, and check the periods against an independent calculation from the energy integral.

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}
Fine inspection time0 s0\,\mathrm{s}
Signed viscous force0 N0\,\mathrm{N}
Signed net force along guide0 N0\,\mathrm{N}
Acquired numerical reversals00
Amber ruler span0 m0\,\mathrm{m}
Amber tick interval0 m0\,\mathrm{m}
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 with a saddle, the top of the barrier, between them. Without damping, a particle with less energy than the saddle stays on one side; with more, it can reach both wells. At exactly the saddle energy, a moving particle creeps ever closer to the saddle and never completes a cycle. That orbit is the separatrix.

Why it mattersThe energy and phase-space picture is standard classical mechanics for motion along one coordinate. The barrier height and the largest allowed tilt are worked out directly from the quartic potential shown. With viscous damping, the model counts every bit of kinetic energy the damping removes.

Start with the essentials

Focus question
Why does crossing a little above the barrier take so much longer?
One-sentence intuition
As the energy approaches the top of the barrier, the particle lingers longer and longer near the saddle. Damping can drain enough energy that an orbit that used to cross gets trapped on one side.

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

Without tilt, the barrier scale is the height of the barrier above either minimum. With tilt, the barrier shown for the release side is recomputed from where the minima and the saddle actually are.

When both minima survive

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

The tilt is kept below the saddle-node threshold, so the two minima and the saddle between them always stay distinct.

Energy balance with viscous damping

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

Each damping substep shrinks the velocity exponentially and adds the exact kinetic energy it removes to the heat. Errors from the conservative part of the step still show up as a mismatch in the balance.

Energy above the barrier and the undamped 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 orbit at exactly the critical energy has no finite period, so the plot leaves a gap between the branches below and above the barrier.

Motion near the saddle

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}

The period grows logarithmically near the saddle, which magnifies small energy errors. A particle released exactly at the saddle stays at rest unless something nudges it.

Common difficulties

Crossings at the critical energy come from the numerics

Typical misconceptionEvery crossing recorded at the critical energy really happens.

Better mental modelThe exact separatrix does not cross the saddle in any finite time. Error from a finite time step can tip it into crossing or turning back, so compare the energy error with the half-step difference.

With tilt, the barrier scale is not the real barrier

Typical misconceptionThe symmetric barrier setting always equals the barrier height on the launch side.

Better mental modelTilt shifts the energies of both minima and of the saddle. The readout uses the actual difference between them.

Damping changes the orbit

Typical misconceptionAfter the particle loses energy, the measured period still equals the undamped reference period.

Better mental modelAs energy drains away, the orbit keeps changing. Capture is reported only once the recorded energy sits below the saddle by more than the numerical uncertainty.

Run the experiment

  1. 01

    Compare trapped and crossing motion

    Acquire full records for Below the barrier and Across both wells, then look at the phase portrait and the recorded saddle crossings.

    What to observe: Without damping, only motion above the barrier reaches both wells.
  2. 02

    Approach the separatrix

    Compare Approach from below with Approach from above, then select Critical energy.

    What to observe: Both periods get longer. At the critical energy the reference shows no finite period, and the result becomes much more sensitive to numerical error.
  3. 03

    Let damping capture the particle

    Acquire a full record with Dissipative capture and look at heat plus mechanical energy.

    What to observe: Heat plus mechanical energy stays equal to the starting energy, and the orbit ends up trapped on one side.
  4. 04

    Tilt without erasing a well

    Change the tilt and drag the release point in phase space. Compare the actual saddle energy with the symmetric barrier scale.

    What to observe: The saddle shifts and the barrier is higher from one side than from the other, yet both minima remain.
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