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Work Distributions

A work distribution describes run-to-run fluctuations of energy transferred by a driving protocol. In macroscopic thermodynamics one often tracks only average work. In a small quantum system, the whole distribution matters: individual realizations fluctuate, rare events control exponential averages, and the definition of a work random variable depends on the measurement protocol.

This page explains how work distributions are organized and interpreted. The standard closed-system construction is the Two-Point Measurement Scheme; here the focus is the distribution as a statistical object, with examples and diagnostics. Quantum Quenches owns the corresponding sudden many-body initial-value problem, Driven Many-Body Systems owns extensive absorption and heating, and Loschmidt Echo and Dynamical Phase Transitions Preview owns the pure-eigenstate characteristic-function relation, Fisher zeros, and return-rate singularities.

For a finite isolated system with discrete energy measurements, a work distribution often has the form

P(W)=∑jpj δ(W−Wj),∑jpj=1.P(W) = \sum_j p_j\, \delta(W-W_j), \qquad \sum_j p_j=1.

The labels jj may represent pairs of measured energy outcomes, monitored trajectories, or another operational record. The work values WjW_j and probabilities pjp_j are meaningful only after the protocol is specified.

The average work is

⟨W⟩=∫dW WP(W),\langle W\rangle = \int dW\,W P(W),

and higher moments are

⟨Wk⟩=∫dW WkP(W).\langle W^k\rangle = \int dW\,W^k P(W).

For a discrete distribution, the integrals are shorthand for sums over the delta peaks.

The characteristic function is

G(u)=⟨eiuW⟩=∫dW eiuWP(W).G(u) = \left\langle e^{iuW}\right\rangle = \int dW\,e^{iuW}P(W).

Moments follow from derivatives at u=0u=0:

⟨Wk⟩=1ikdkGduk∣u=0.\langle W^k\rangle = \frac{1}{i^k} \left. \frac{d^kG}{du^k} \right|_{u=0}.

The cumulant generating function is

K(u)=ln⁡G(u).K(u) = \ln G(u).

The first two cumulants are the mean and variance:

κ1=⟨W⟩,κ2=⟨W2⟩−⟨W⟩2.\kappa_1 = \langle W\rangle, \qquad \kappa_2 = \langle W^2\rangle-\langle W\rangle^2.

Characteristic functions are often easier to access than P(W)P(W) itself. Interferometric and full-counting-statistics protocols typically measure a generating function and reconstruct distributional information from it.

For a closed driven protocol with initial Hamiltonian H0H_0, final Hamiltonian HτH_\tau, and unitary Uτ,0U_{\tau,0}, the two-point measurement scheme gives

PTPM(W)=∑m,np(m,n)δ ⁣(W−Emτ+En0),P_{\mathrm{TPM}}(W) = \sum_{m,n} p(m,n) \delta\!\left( W-E_m^\tau+E_n^0 \right),

where

p(m,n)=Tr⁡[ΠmτUτ,0Πn0ρ0Πn0Uτ,0†Πmτ].p(m,n) = \operatorname{Tr} \left[ \Pi_m^\tau U_{\tau,0} \Pi_n^0\rho_0\Pi_n^0 U_{\tau,0}^\dagger \Pi_m^\tau \right].

This distribution is positive and normalized. If the initial state is thermal, it is the work distribution used in the standard quantum Jarzynski equality and Crooks relation. If the initial state has energy coherence, it is the distribution for the experiment in which the first projective energy measurement was actually performed.

A useful finite example has ground energy 00 and excited energy ϵ0\epsilon_0 initially, and ground energy 00 and excited energy ϵτ\epsilon_\tau finally. Let the initial excited-state population be pe0p_e^0, and set pg0=1−pe0p_g^0=1-p_e^0.

Assume the drive produces transition probabilities

Pg→e=Pe→g=r,Pg→g=Pe→e=1−r.P_{g\to e} = P_{e\to g} = r, \qquad P_{g\to g} = P_{e\to e} = 1-r.

The four TPM work values are:

Initial BranchFinal BranchWork
gggg00
ggeeϵτ\epsilon_\tau
eegg−ϵ0-\epsilon_0
eeeeϵτ−ϵ0\epsilon_\tau-\epsilon_0

The distribution is

P(W)=pg0(1−r)δ(W)+pg0r δ(W−ϵτ)+pe0r δ(W+ϵ0)+pe0(1−r)δ ⁣(W−ϵτ+ϵ0).\begin{aligned} P(W) = {}& p_g^0(1-r)\delta(W) + p_g^0 r\,\delta(W-\epsilon_\tau) \\ &+ p_e^0 r\,\delta(W+\epsilon_0) + p_e^0(1-r) \delta\!\left( W-\epsilon_\tau+\epsilon_0 \right). \end{aligned}

The mean work is

⟨W⟩=pg0r ϵτ−pe0r ϵ0+pe0(1−r)(ϵτ−ϵ0).\langle W\rangle = p_g^0 r\,\epsilon_\tau - p_e^0 r\,\epsilon_0 + p_e^0(1-r)(\epsilon_\tau-\epsilon_0).

This example shows three generic features:

  • work can be negative in individual runs even when the average is positive;
  • nonadiabatic transitions broaden the distribution;
  • changing gaps and changing populations contribute differently to the work values.

When r=0r=0, each initial energy branch stays on its corresponding final branch. When rr is nonzero, the drive can promote the system from ground to excited or de-excite it while the Hamiltonian changes.

The frozen-state criterion and final-basis overlap probabilities are derived in Sudden Approximation. Here those probabilities are used to construct a work distribution.

A harmonic oscillator with frequency ω\omega has Hamiltonian

H(ω)=p22m+12mω2x2,H(\omega) = \frac{p^2}{2m} + \frac12m\omega^2x^2,

with energy levels

En(ω)=ℏω(n+12).E_n(\omega) = \hbar\omega \left( n+\frac12 \right).

In a sudden frequency quench, the frequency changes from ω0\omega_0 to ωτ\omega_\tau so rapidly that the state does not have time to evolve during the change. The initial and final energy eigenstates are different oscillator bases. The TPM distribution is

P(W)=∑m,npn0∣⟨m;ωτ∣n;ω0⟩∣2δ ⁣(W−Em(ωτ)+En(ω0)).P(W) = \sum_{m,n} p_n^0 \left| \langle m;\omega_\tau|n;\omega_0\rangle \right|^2 \delta\!\left( W - E_m(\omega_\tau) + E_n(\omega_0) \right).

The overlaps encode the mismatch between the two oscillator bases. For a sudden quench they are not generally diagonal in m,nm,n, so the distribution has many peaks. Parity is conserved by the instantaneous frequency change, so only same-parity overlaps contribute.

The mean work can be found without summing all overlaps. For an initial thermal state of H(ω0)H(\omega_0),

⟨H(ω0)⟩0=ℏω02coth⁡(βℏω02).\langle H(\omega_0)\rangle_0 = \frac{\hbar\omega_0}{2} \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

The sudden final average energy is

⟨H(ωτ)⟩0=ℏ4(ω0+ωτ2ω0)coth⁡(βℏω02).\langle H(\omega_\tau)\rangle_0 = \frac{\hbar}{4} \left( \omega_0 + \frac{\omega_\tau^2}{\omega_0} \right) \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

Therefore

⟨W⟩=ℏ4(ωτ2ω0−ω0)coth⁡(βℏω02).\langle W\rangle = \frac{\hbar}{4} \left( \frac{\omega_\tau^2}{\omega_0} - \omega_0 \right) \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

This mean is useful, but it hides the distributional structure: the quench creates a squeezed-state energy distribution in the final oscillator basis.

Fluctuation relations often involve

⟨e−βW⟩.\left\langle e^{-\beta W}\right\rangle.

This average weights low-work and negative-work events strongly. In simulations or experiments, it can converge slowly even when the ordinary mean ⟨W⟩\langle W\rangle appears stable. A small number of rare events can dominate the estimate.

For a Gaussian work distribution with mean μ\mu and variance vv,

⟨e−βW⟩=exp⁡(−βμ+β2v2).\left\langle e^{-\beta W}\right\rangle = \exp \left( -\beta\mu + \frac{\beta^2v}{2} \right).

This formula is not generally exact for quantum work distributions; it is a useful warning. Fluctuations are not a small correction inside exponential work identities.

When the initial state has energy coherence, a projective initial energy measurement changes the state. There are then several inequivalent questions:

  • What work distribution is obtained if the initial energy is strongly measured?
  • What average energy change occurs if the initial measurement is not performed?
  • Can one construct a weak-measurement or interferometric quasiprobability that keeps some coherence information?
  • Which distribution appears in a particular fluctuation theorem?

Quasiprobability approaches can retain phase-sensitive information, but they may become negative or complex. That is not a defect if the object is not being claimed as an ordinary probability distribution. It is a sign that the protocol is answering a different operational question from TPM.

The practical rule is simple: do not compare work distributions unless their measurement protocols match.

For open systems, the work distribution is not determined by the reduced system energy difference alone. A stochastic first-law statement along a monitored trajectory often has the schematic form

Δe[γ]=w[γ]+∑αqα[γ],\Delta e[\gamma] = w[\gamma] + \sum_\alpha q_\alpha[\gamma],

where w[γ]w[\gamma] is work assigned to external driving and qα[γ]q_\alpha[\gamma] is heat exchanged with reservoir α\alpha. This expression requires a trajectory model, a sign convention, and jump or measurement records that correspond to physical energy exchanges.

Examples include:

  • quantum-jump trajectories with thermally consistent jump operators;
  • full counting statistics for reservoir energy or particle number;
  • continuously monitored systems with feedback;
  • inclusive system-plus-bath energy measurements.

A reduced master equation may predict ρ(t)\rho(t) accurately while still being insufficient to define a trustworthy work distribution. The record-level model matters.

Before using a work distribution, check:

  • Is the protocol closed, open, monitored, or inclusive system-plus-bath?
  • Which energy measurements or counting fields define WW?
  • Does the initial state commute with the initial Hamiltonian?
  • Are degeneracies handled by energy projectors or by refined measurements?
  • Is the distribution positive, or is it a quasiprobability?
  • Does the mean agree with the relevant energy balance?
  • Does the distribution satisfy the intended normalization and fluctuation relation?
  • Are rare events sampled well enough for exponential averages?

These checks prevent a common failure mode: computing a plausible histogram and then interpreting it with the wrong theorem.

  1. Calling any histogram of final-minus-initial system energy “the work distribution” without specifying the measurement protocol.

  2. Inferring Jarzynski or Crooks relations from a distribution whose initial state, dynamics, or reverse protocol does not satisfy the theorem’s assumptions.

  3. Ignoring negative-work events because they are rare.

  4. Treating quasiprobability negativity as a numerical error without checking the protocol.

  5. Using average work alone to validate a distribution.

  6. Applying closed-system TPM formulas to dissipative dynamics without tracking heat.

Starting from the two-level distribution above, derive the mean work.

Solution

The distribution has four branches:

branchprobabilityworkg→gpg0(1−r)0g→epg0rϵτe→gpe0r−ϵ0e→epe0(1−r)ϵτ−ϵ0\begin{array}{c|c|c} \text{branch} & \text{probability} & \text{work} \\ \hline g\to g & p_g^0(1-r) & 0 \\ g\to e & p_g^0 r & \epsilon_\tau \\ e\to g & p_e^0 r & -\epsilon_0 \\ e\to e & p_e^0(1-r) & \epsilon_\tau-\epsilon_0 \end{array}

Multiplying probability by work and summing gives

⟨W⟩=pg0r ϵτ−pe0r ϵ0+pe0(1−r)(ϵτ−ϵ0).\langle W\rangle = p_g^0 r\,\epsilon_\tau - p_e^0 r\,\epsilon_0 + p_e^0(1-r)(\epsilon_\tau-\epsilon_0).

The g→gg\to g branch contributes zero.

Show that G(u)=⟨eiuW⟩G(u)=\langle e^{iuW}\rangle satisfies

⟨W⟩=1iG′(0),⟨W2⟩=1i2G′′(0).\langle W\rangle = \frac{1}{i}G'(0), \qquad \langle W^2\rangle = \frac{1}{i^2}G''(0).
Solution

Differentiate under the average:

G′(u)=⟨iWeiuW⟩.G'(u) = \left\langle iW e^{iuW} \right\rangle.

At u=0u=0,

G′(0)=i⟨W⟩,G'(0)=i\langle W\rangle,

so

⟨W⟩=1iG′(0).\langle W\rangle=\frac{1}{i}G'(0).

Differentiating twice gives

G′′(u)=⟨(iW)2eiuW⟩.G''(u) = \left\langle (iW)^2e^{iuW} \right\rangle.

Thus

G′′(0)=i2⟨W2⟩,G''(0)=i^2\langle W^2\rangle,

and

⟨W2⟩=1i2G′′(0).\langle W^2\rangle = \frac{1}{i^2}G''(0).

For an initial thermal oscillator at frequency ω0\omega_0, use

⟨p22m⟩0=⟨12mω02x2⟩0=ℏω04coth⁡(βℏω02)\left\langle \frac{p^2}{2m}\right\rangle_0 = \left\langle \frac12m\omega_0^2x^2\right\rangle_0 = \frac{\hbar\omega_0}{4} \coth \left( \frac{\beta\hbar\omega_0}{2} \right)

to derive the mean work for a sudden quench to ωτ\omega_\tau.

Solution

The initial energy is

⟨H(ω0)⟩0=ℏω02coth⁡(βℏω02).\langle H(\omega_0)\rangle_0 = \frac{\hbar\omega_0}{2} \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

The kinetic part immediately after the quench is unchanged:

⟨p22m⟩0=ℏω04coth⁡(βℏω02).\left\langle \frac{p^2}{2m}\right\rangle_0 = \frac{\hbar\omega_0}{4} \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

The position variance follows from the initial potential energy:

12mω02⟨x2⟩0=ℏω04coth⁡(βℏω02),\frac12m\omega_0^2\langle x^2\rangle_0 = \frac{\hbar\omega_0}{4} \coth \left( \frac{\beta\hbar\omega_0}{2} \right),

so

12mωτ2⟨x2⟩0=ℏωτ24ω0coth⁡(βℏω02).\frac12m\omega_\tau^2\langle x^2\rangle_0 = \frac{\hbar\omega_\tau^2}{4\omega_0} \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

Therefore

⟨H(ωτ)⟩0=ℏ4(ω0+ωτ2ω0)coth⁡(βℏω02).\langle H(\omega_\tau)\rangle_0 = \frac{\hbar}{4} \left( \omega_0 + \frac{\omega_\tau^2}{\omega_0} \right) \coth \left( \frac{\beta\hbar\omega_0}{2} \right).

Subtracting the initial energy gives

⟨W⟩=ℏ4(ωτ2ω0−ω0)coth⁡(βℏω02).\langle W\rangle = \frac{\hbar}{4} \left( \frac{\omega_\tau^2}{\omega_0} - \omega_0 \right) \coth \left( \frac{\beta\hbar\omega_0}{2} \right).
  • P. Talkner, E. Lutz, and P. Hänggi, “Fluctuation theorems: Work is not an observable,” Physical Review E 75, 050102, 2007.
  • M. Campisi, P. Hänggi, and P. Talkner, “Colloquium: Quantum fluctuation relations: Foundations and applications,” Reviews of Modern Physics 83, 771, 2011.
  • M. Esposito, U. Harbola, and S. Mukamel, “Nonequilibrium fluctuations, fluctuation theorems, and counting statistics in quantum systems,” Reviews of Modern Physics 81, 1665, 2009.
  • S. Deffner and S. Campbell, Quantum Thermodynamics: An Introduction to the Thermodynamics of Quantum Information, Morgan & Claypool, 2019.
  • H. T. Quan and W. H. Zurek, “Testing quantum adiabaticity with quench echoes,” New Journal of Physics 12, 093025, 2010.