advanced29 min studyLesson 883 in Physics

Local thermodynamic equilibrium and Kirchhoff's law

Apply thermal detailed balance without assuming a globally Planckian radiation field, and distinguish kinetic, excitation and brightness temperatures.

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What you’ll understand

  • State what LTE assumes about matter populations.
  • Apply Kirchhoff's law to true thermal emission and net absorption.
  • Compute an optically incomplete thermal brightness in the Rayleigh-Jeans limit.

A gas can have locally thermal particle distributions even while its radiation escapes into space and differs from a blackbody. Local thermodynamic equilibrium is an assumption about matter populations and microscopic balance at a local temperature, not a declaration that every ray already has the Planck intensity. Kirchhoff's law connects thermal emissivity with net true absorption under these conditions. We will identify precisely which source function becomes Planckian and why optical depth, scattering, and temperature gradients still affect an observed spectrum.

Local thermal matter does not require global radiative equilibrium

In LTE, translational velocities follow thermal distributions and excitation and ionization populations follow local Boltzmann and Saha relations at a common temperature, with the applicable particle statistics and chemical potentials. The state can vary with position. The radiation field need not equal the Planck function in every direction because photons connect regions with different temperatures and can escape through boundaries. LTE also does not require zero net radiative energy transport. Stellar interiors can carry an outward luminosity while their matter populations are close to local thermal equilibrium.

LTE is most plausible when relevant equilibration processes are fast compared with changes in the local gas and radiative perturbations of the populations. Low-density photoionized nebulae often require rate equations instead of a local Saha prescription. A Maxwellian electron distribution by itself does not prove that every atomic level or ion stage is in LTE. Conversely, an approximately thermal continuum can arise from one process without making all line populations thermal. Each diagnostic must state which part of the material distribution is assumed equilibrated.

Bν(T)=2hν3c21ehν/(kBT)−1,nunl=gugle−hν0/(kBT),jν,th=αν,absBν(T)B_\nu(T)=\frac{2h\nu^3}{c^2}\frac1{e^{h\nu/(k_BT)}-1},\qquad \frac{n_u}{n_l}=\frac{g_u}{g_l}e^{-h\nu_0/(k_BT)},\qquad j_{\nu,\mathrm{th}}=\alpha_{\nu,\mathrm{abs}}B_\nu(T)
Bnu has W m to the minus two Hz to the minus one sr to the minus one units, and jthermal is per solid angle. Net true absorption includes stimulated-emission corrections. The last equality is the thermal Kirchhoff relation, not a relation between B and total scattering extinction alone.↔ Scroll wide equations horizontally.

Kirchhoff's law concerns a specified process

In thermodynamic equilibrium a thermal emitter placed in a blackbody radiation bath neither gains nor loses photons through a given balanced process. The transfer equation then gives emissivity divided by net absorption equal to the Planck function. The same local relation can be used for thermal matter in LTE even when the actual incoming radiation differs from B. Spontaneous and stimulated transitions must be combined consistently; using a gross upward absorption coefficient while omitting stimulated emission gives the wrong source function.

If coherent scattering also contributes, its emissivity is proportional to the actual mean intensity rather than automatically to B. The total source function is consequently the weighted B and J combination derived previously. Large scattering optical depth alone does not ensure thermalization; enough true absorption and re-emission must occur to exchange energy with matter. In a varying atmosphere the emergent intensity samples a range of depths with different local temperatures. Replacing that entire contribution function by one blackbody requires an additional approximation, not merely the statement that matter is in LTE.

Iν,out=Bν(T)(1−e−τν)(Iν,in=0),Bν≃2kBTν2c2(hν≪kBT),Tb=c2Iν2kBν2=T(1−e−τν)I_{\nu,\mathrm{out}}=B_\nu(T)(1-e^{-\tau_\nu})\quad(I_{\nu,\mathrm{in}}=0),\qquad B_\nu\simeq\frac{2k_BT\nu^2}{c^2}\quad(h\nu\ll k_BT),\qquad T_b=\frac{c^2I_\nu}{2k_B\nu^2}=T(1-e^{-\tau_\nu})
The slab is isothermal, uniform, in LTE for true absorption/emission, and has no scattering or incident background. The brightness-temperature equality uses the Rayleigh-Jeans approximation. Tb approaches the kinetic temperature only in the optically thick limit of this particular model.↔ Scroll wide equations horizontally.

Several temperatures encode different information

Kinetic temperature describes a particle velocity distribution. An excitation temperature parameterizes the ratio of two level populations. Brightness temperature is the temperature assigned to a measured intensity by a chosen spectral convention. Under LTE the excitation and kinetic temperatures agree, but a partially transparent thermal slab can still have a lower brightness temperature. A nonthermal or amplified source can have a brightness temperature with no direct interpretation as the gas kinetic temperature. Always specify whether the definition uses the full Planck inversion or the Rayleigh-Jeans form.

A useful limiting check is to hold the slab temperature fixed while decreasing optical depth. Its Rayleigh-Jeans brightness falls linearly with small depth, even though the particles have not cooled. An observed brightness decrease can therefore indicate less emitting material, a smaller beam filling factor, or an opacity change instead of a different kinetic temperature. Frequency-dependent opacity further changes which depths are sampled. Comparing continuum brightness with line ratios and independent geometry helps separate these possibilities, while recognizing that each inference carries its own population and transfer assumptions.

A thermal slab with half its blackbody brightness

An isothermal pure-absorption LTE slab has T = 100 K, frequency 1 GHz, ray depth ln two, and zero incoming intensity. Use kB=1.38×10−23 J K−1k_B=1.38\times10^{-23}\,\mathrm{J\,K^{-1}}, h=6.63×10−34 J sh=6.63\times10^{-34}\,\mathrm{J\,s}, and c = 3 × 10^8 m/s. Find the approximate intensity and Rayleigh-Jeans brightness temperature.

  1. The ratio hν/(kBT)≈4.8×10−4h\nu/(k_BT)\approx4.8\times10^{-4} is much smaller than one, so the Rayleigh-Jeans approximation is justified at the stated frequency and temperature.

  2. The Planck intensity is approximately 2kBTν2/c2=3.07×10−20 W m−2 Hz−1 sr−12k_BT\nu^2/c^2=3.07\times10^{-20}\,\mathrm{W\,m^{-2}\,Hz^{-1}\,sr^{-1}}. Depth ln two gives the emitted fraction one half.

  3. The outgoing intensity is therefore about 1.53×10−201.53\times10^{-20} in the same units, and Tb=T/2=50 KT_b=T/2=50\,\mathrm K. A lower brightness temperature here reflects incomplete optical thickness rather than a colder gas.

The result

The intensity is approximately 1.53 × 10^−20 W m^−2 Hz^−1 sr^−1 and the Rayleigh-Jeans brightness temperature is 50 K.

Explore the model

Interactive lab

Interactive lab · probability

An incomplete thermal contribution has a fractional weight

Reset and set BOTH Success probability p = 0.50 and Trials n = 1; predict mean success count 0.50. For a fresh comparison, Reset and set p = 1 and n = 1; predict mean 1. Interpret only these weights as partial versus complete contributions.

An incomplete thermal contribution has a fractional weightThese are exact binomial probabilities for independent trials with one fixed success probability. Playback tours the distribution; it does not resample outcomes. Current readings: Mean · np: 5; Variance · np(1−p): 2.5; Total probability: 1. All parameters are adjustable with the labeled controls below.03581000.070.150.220.3Successes kP(X = k)k = 0 · P = 9.77e-4
Exact probabilityHighlighted outcomeMean np
Mean · np
5
Variance · np(1−p)
2.5
Total probability
1
t = 0 s

These are exact binomial probabilities for independent trials with one fixed success probability. Playback tours the distribution; it does not resample outcomes. Parameter changes pause playback and recompute the model at the current elapsed time. Reset restores both parameters and returns time to zero. Playback starts paused. Adjust either parameter, then choose Play or Step.

Look forThe exact Bernoulli weights illustrate a fractional contribution. They do not compute a Planck spectrum, LTE populations, optical depth, brightness temperature, or radiation hydrodynamics.

Check your understanding

What does LTE by itself imply about the radiation field in an atmosphere with boundaries and temperature gradients?

Try it yourself

For an LTE two-level transition let gu/gl=2g_u/g_l=2 and hν0/(kBT)=ln⁡4h\nu_0/(k_BT)=\ln4. Find the upper-to-lower population ratio and the Planck photon occupation number at that frequency. What source intensity follows in units of Q=2hν03/c2Q=2h\nu_0^3/c^2?

Take a moment to make a prediction or work it out on paper. Open a hint when you need one.

Give me a hint

The exponential is four. Population degeneracy and photon occupation enter different expressions.

Compare with the solution

The population ratio is nu/nl=2e−ln⁡4=1/2n_u/n_l=2e^{-\ln4}=1/2. The photon occupation factor is 1/(eln⁡4−1)=1/31/(e^{\ln4}-1)=1/3, so Bν0=Q/3B_{\nu_0}=Q/3. With the stated LTE true-absorption convention, j divided by alpha equals that same Q over three. The population ratio one half is not the photon occupation number; the statistical weights account for their difference, and neither ratio is itself the emergent intensity of a finite slab.

Take it with you

  • LTE is a local matter-population assumption and does not force a globally blackbody radiation field.
  • Kirchhoff's law uses thermal emissivity and net true absorption with consistent stimulated emission.
  • Brightness, excitation, and kinetic temperatures coincide only under additional conditions.

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