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Concept · physics

Stochastic thermodynamics

3 studies1 discoveryEvidence last moved Sep 27, 2026

Stochastic thermodynamics applies work, heat and free energy to single small systems whose behaviour is dominated by thermal fluctuations. The evidence here comes from a colloidal experiment on first-passage times, a simulation of feedback-based work extraction, and molecular dynamics using the Jarzynski equality to compute nucleation free energies.

At the nanoscale, individual runs fluctuate wildly, yet averages over them obey exact relations that give equilibrium quantities from non-equilibrium data. This clears up the confusion that noisy, fast or imprecise processes can say nothing about free energies or efficiency.

Studies

3

Findings

4

5 supporting · 0 challenging · 3 qualifying citations

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Stochastic thermodynamics

Currently

What we know

  1. The timing of first arrivals can count hidden intermediate states.
  2. Imprecise measurements can still be used with full efficiency if the feedback is reversible.
  3. Exponential averaging of non-equilibrium work recovers an equilibrium free-energy barrier.
  4. Exact averages coexist with large run-to-run scatter, so sampling matters.

Largest unresolved question

The first-passage study is experimental and validated on real molecules, while the work-extraction and cavity results are simulations of idealised models; the latter show what the relations allow, not what is achieved in a lab.

Common misconceptions

  • A noisy measurement always wastes some of the work it could let you extract.

    In the simulated protocol, reversible feedback extracted exactly kT times the mutual information, an efficiency of 1; the limit is the information gained, not the precision itself.

  • Free energies can only be computed from slow, equilibrium (quasistatic) processes.

    The Jarzynski equality turns repeated fast, irreversible work measurements into a free-energy profile, as in the cavity-nucleation simulations, though it needs enough rare low-work runs.

  • First-passage times only tell you an average rate.

    The shape of the short-time distribution revealed how many intermediate minima lay on the path, and its duration encoded their depth.

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