MARIJA VUCELJA / RESEARCH AND ATTRIBUTION

The route back
can change.

Marija Vucelja’s work asks how a system’s preparation changes its route to equilibrium. Build the probability picture, watch the modes, and test the result.

Computed probability-simplex curve for our large-gap C5 fixture. Each point is a normalized distribution; this is our calculation, not a reproduced paper figure.
Computed probability-simplex curve for our large-gap C5 fixture. Each point is a normalized distribution; this is our calculation, not a reproduced paper figure.

The surprising question is about the whole state.

A starting temperature tells you how a system was prepared. It does not, by itself, describe every stage of its return to equilibrium.

Imagine repeatedly preparing one tiny system with three possible states. Record the fraction of repetitions found in each state: that gives three probabilities. The probabilities can change while the allowed states and the surrounding bath stay the same. This is the language of our illustration.

Vucelja and her coauthors use statistical physics to investigate anomalous relaxation. The relevant connection here is slow-mode cancellation in a specified Markovian model. The geometric picture below is our own calculation, built to make that idea inspectable.

LEARN THE PICTURE / OUR C5 FIXTURE

One point. Three probabilities.

A point inside a triangle encodes three nonnegative probabilities summing to one. Each corner assigns probability one to its named state; the center assigns one third to every state.

Every corner is a possible state.

A point at State 0 means probability one in State 0. At the center, all three probabilities are one third. Moving a point changes the probabilities, not an object’s physical position.

p₀ = 0.333333

p₁ = 0.333333

p₂ = 0.333333

The triangle is probability space. Coordinates are calculated from the C5 state probabilities; line lengths on this drawing are not L1 distances or distances through physical space. The bath marker is the common equilibrium.

A triangle is a bookkeeping device.

Three probabilities might seem to need three coordinates. But p₀ + p₁ + p₂ = 1 removes one degree of freedom. A flat triangle can therefore hold every possible distribution. Its corners are certainty in one state; its edges set one probability to zero; points inside give positive probabilities to all three states.

For the large-gap C5 fixture, the warm start is approximately (0.120, 0.409, 0.471). The hotter strong-root start is (0.255, 0.365, 0.380). Both approach the same bath distribution, approximately (0.041, 0.416, 0.543). Read the bars beside the triangle: the object represented is a distribution, not a droplet moving across a surface.

The animation uses the saved rate matrix. We change the initial preparation while holding that matrix and the bath fixed. It is a controlled numerical comparison; the points are not experimental observations from Vucelja’s laboratory.

What “removing the slow mode” means.

In this three-state model, the departure from equilibrium separates into two vector contributions. Each shrinks exponentially at its own rate. Their initial coefficients depend on the preparation.

p(t) − π = a eλ₂t + b eλ₃ta and b are vector contributions; both rates are negative in this fixture.

The slow contribution has the smaller magnitude rate, |λ₂| = 0.0015912. The other rate is |λ₃| = 0.0115395. For an ordinary preparation, the fast contribution eventually becomes small enough that the slower one governs the late tail. At the special strong-root preparation, the slow contribution vanishes in the model. The fast decay remains.

Computed L1 norms of the two initial mode contributions in our large-gap fixture. Their norms are shown separately; vector cancellation means these norms do not generally add to the total L1 distance.
Computed L1 norms of the two initial mode contributions in our large-gap fixture. Their norms are shown separately; vector cancellation means these norms do not generally add to the total L1 distance.
WORKED EXAMPLE / ATLAS CALCULATION

A faster tail does not settle every finish line.

At ε = 0.001, the strong-root start arrives at 525.008 model units and the warm start at 1,998.331. At the looser ε = 0.1, warm arrives at 39.014 and strong-root at 125.929. The same generator, preparations and decay rates produce both orderings. The operational question includes the threshold.

Try both thresholds and the small-gap counterexample ↗

This is why the Atlas reports a mode criterion and an arrival criterion together. Changing the threshold is a legitimate exploratory question; a confirmatory comparison must declare the relevant threshold before looking for a winning result.

A way into nonequilibrium physics

Marija Vucelja is an associate professor of physics at the University of Virginia, with a mathematics affiliation. Her research spans nonequilibrium statistical physics and anomalous thermal relaxation. Here we focus on work that helps us ask a precise question: which preparation changes the route back to equilibrium? Vucelja’s research website ↗

“Using statistics and probability, we can see the forest for the trees”Marija Vucelja, quoted by Fariss Samarrai in UVA Today, 21 May 2020. Read the original profile ↗

The papers that matter to this investigation

WorkContributionHow we use it
Klich, Raz, Hirschberg & Vucelja · PRX 2019Strong Mpemba relaxation and the geometry of slow-mode cancellation.A theoretical basis for a clearly identified, separate three-state illustration.
Klich & Vucelja · 2019 preprintAn exact result for specified complete-graph Metropolis dynamics.A narrowly defined negative control, rather than a claim about every complete graph.
Teza, Bechhoefer, Lasanta, Raz & Vucelja · 2026 reviewDefinitions, experimental systems and routes to applications.A guide to distinguishing distance measures, model classes and experiments.
Klich & Vucelja · J. Phys. A 2026Related near-complete-graph / independence Metropolis–Hastings publication.Title and publication metadata confirmed. Full-text extensions are not reproduced here.
Vucelja & Fouxon · JFM 2007Weak compressibility of liquid-surface wave turbulence.An explicit limit on transferring surface-wave clustering into an airborne-fog claim.

Her research. Our numerical illustration.

The downloadable C5 records were generated for Waveform Atlas’s research review. They are not a dataset supplied by Vucelja’s group, and they are not measurements of a laboratory cooling apparatus. The papers are credited for the relevant theory; our code, fixtures and limitations have their own provenance.

Two selected three-state chains expose the practical distinction. At L1 distance 0.001, the strong-root preparation arrives earlier than the warm preparation in the large-gap example, but later in the small-gap example. Both have a preparation that removes the slow mode. The starting amplitudes and the chosen finish line still matter.

Attribution, not affiliation. Vucelja and her coauthors have not reviewed or endorsed this site. This page does not imply a collaboration. No unpublished experimental data or personal correspondence is represented.

The useful next question

For a specified physical system, can its measured relaxation modes and accessible preparations support a repeatable improvement at a declared operational threshold? Answering that requires an actual system model, calibrated observations and preparation costs. The theoretical possibility is valuable; the transfer remains to be tested.

The Atlas keeps this thread alongside its damping investigation, compression chapter and measurement methods.

Sources for this chapter

Published work, author attribution and the limits relevant to this chapter. Atlas examples and calculations are labeled separately.

Marija Vucelja

Research and academic profile ↗

Author’s research website

Scope and access record

First-person research profile

University of Virginia affiliation and nonequilibrium statistical-physics research interests.

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