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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. For extended systems, see Quantum Quenches and Driven Many-Body Systems. For an initial energy eigenstate, the characteristic function also connects to the Loschmidt amplitude.

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).

Choose the logarithm continuously near u=0u=0, with K(0)=0K(0)=0. Zeros of G(u)G(u) can obstruct a single logarithm over the whole real axis. When the required moments exist, 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, the two-point measurement scheme supplies joint probabilities p(m,n)p(m,n) for initial and final energies. Group branches with the same difference to obtain

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

This positive distribution describes the experiment with the initial energy measurement included. For coherent initial states its mean can differ from the energy change in an experiment that omits that measurement.

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.

A unitary drive on a two-dimensional Hilbert space has equal transition probabilities in the two directions. Write

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 Branch Final Branch Work
gg gg 00
gg ee ϵτ\epsilon_\tau
ee gg −ϵ0-\epsilon_0
ee ee ϵτ−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).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).

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 add or redistribute work branches; the variance need not grow monotonically with transition probability;
  • 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 initial Gibbs state is a squeezed thermal state relative to the final oscillator modes, with a structured energy distribution. It is pure only for an initial ground state.

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).

The formula is exact for a Gaussian distribution. A generic quantum work distribution is not Gaussian, so its higher cumulants cannot simply be dropped.

For a concrete sampling example, take a thermal qubit with βϵ=5\beta\epsilon=5 and a cyclic drive that swaps its two energy levels. Almost every run has W=+ϵW=+\epsilon, while W=−ϵW=-\epsilon occurs with probability pe=1/(1+e5)≃0.00669p_e=1/(1+e^5)\simeq0.00669. Nevertheless, the rare branch contributes pee5≃0.9933p_e e^5\simeq0.9933 to the exact exponential average of one. In 100 independent runs, the chance of seeing no such branch is (1−pe)100≃0.51(1-p_e)^{100}\simeq0.51. A stable-looking sample mean therefore does not guarantee an accurate Jarzynski estimate.

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.

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).
  • M. Campisi, P. Hänggi, and P. Talkner, “Colloquium: Quantum fluctuation relations: Foundations and applications,” Reviews of Modern Physics 83, 771–791 (2011). arXiv:1012.2268.
  • S. Deffner and S. Campbell, Quantum Thermodynamics: An Introduction to the Thermodynamics of Quantum Information, Morgan & Claypool, 2019.
  • M. Esposito, U. Harbola, and S. Mukamel, “Nonequilibrium fluctuations, fluctuation theorems, and counting statistics in quantum systems,” Reviews of Modern Physics 81, 1665–1702 (2009).
  • H. T. Quan and W. H. Zurek, “Testing quantum adiabaticity with quench echoes,” New Journal of Physics 12, 093025 (2010).
  • P. Talkner, E. Lutz, and P. Hänggi, “Fluctuation theorems: Work is not an observable,” Physical Review E 75, 050102(R) (2007).