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Transport theory and the Boltzmann equation

Begin with opposite particle populations at zero mean flow, follow conserved moments and collision gain–loss, solve a positive BGK relaxation, then derive the scope of kinetic entropy, fluid closure and transport coefficients.

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After reading, you can

  • Define a number-density velocity distribution, peculiar velocity, pressure tensor and physical heat flux with their measures and units.
  • Distinguish streaming, external forcing and collision gain–loss, and explain the incoming-pair closure behind the dilute Boltzmann equation.
  • Identify elastic collision invariants without assuming every distribution moment is fixed.
  • Solve the supplied matching-moment BGK example and distinguish directional relaxation, finite plotting windows and the infinite-time limit.
  • Derive moment balances and explain why constitutive closure, local scale separation and boundary laws are additional requirements.
  • Explain the conditioned H inequality, linearized invariant compatibility and the single-time model’s transport limitations.
01

Two opposite populations, with no bulk flow

Imagine a small, spatially uniform sample of dilute gas. Half its particles tend to move to the right and half to the left. The average velocity is zero, but motion along that direction is stronger than motion across it. Can collisions change this distribution while leaving particle number, total momentum and total energy unchanged?

Yes. Conservation fixes only particular averages, not the whole distribution of velocities. Collisions can redistribute energy between directions without creating energy or starting a bulk flow. Our supplied example begins with directional pressures in the ratio 5:1:1. Its equilibrium ratio will be 1:1:1, with the same sum of 7. The numerical values are dimensionless model values, not measurements of a named material.

We will first describe the distribution, identify what collisions preserve, and solve a deliberately simple relaxation model. Then we will see why a flowing gas needs more than a local equilibrium formula. The advanced return path derives the collision entropy inequality, the linearized invariant modes, and the conditions on a fluid approximation. The example is not an exact solution of the full Boltzmann collision integral.

02

Define the distribution before taking its averages

Let f(x,v,t) d³x d³v be the expected number of particles in a small position-and-velocity element. Here x is position, v is particle velocity and t is time. Integrating over velocity gives the local number density n=∫f d³v. Dividing by n gives a normalized local velocity probability density. The factor 1/n matters: u=(1/n)∫v f d³v is the mean flow velocity, not the unnormalized particle flux.

A particle’s velocity relative to that mean is c=v−u, called its peculiar velocity. Then ∫c f d³v=0. This is an average cancellation; individual particles still move. A distribution can have u=0 while being anisotropic, meaning different directions have different statistics. It can also have zero heat flux without being Maxwellian.

In SI units, n has units m⁻³ and f has units s³ m⁻⁶ when particle count is treated as dimensionless. A velocity marginal integrates over the other velocity components. Its graph is a density per velocity interval, not the probability of one exact velocity and not a picture of particle positions. The measure must stay the same when comparing curves or defining an entropy.

03

Separate travel, acceleration and collisions

For a specified velocity-independent force F(x,t) on each particle of mass m, the kinetic equation is ∂_t f+v·∇_x f+(F/m)·∇_v f=C[f]. Free streaming moves particles between positions. The force moves their velocities. The collision operator C redistributes velocities through encounters at a position. These are different mechanisms, even when they act simultaneously.

For example, a distribution that varies in space can change through streaming even where its collision term is zero. Conversely, our uniform force-free example has no streaming or acceleration term, so its change comes entirely from the assigned collisions. Uniformity here does not describe two spatial clouds separated by a hidden interface.

The displayed convective force term uses zero divergence of F/m in velocity space. A more general acceleration law needs the conservative phase-space form ∂_t f+∇_x·(v f)+∇_v·(a f)=C[f]. One must not silently use the simpler equation for an arbitrary compressible phase-space flow.

04

Read collision gain and loss

For the classical, dilute, elastic, binary-collision description, a standard gain-minus-loss form is C[f](v)=∫d³v₁ dΩ B(v−v₁,Ω)[f(v′)f(v₁′)−f(v)f(v₁)]. All distributions in this expression refer to the same position and time. The two velocity pairs are linked by the stated elastic scattering rule. Microreversibility allows the inverse encounter to supply the gain term in this common notation.

The nonnegative kernel B contains relative speed and the differential scattering cross section in the chosen angular convention. The loss term removes particles from a small velocity neighbourhood around v through encounters with other velocities. The gain term adds particles whose incoming velocities scatter into that neighbourhood. A collision does not remove a particle from the gas merely because it removes it from one velocity interval.

The product of two one-particle distributions is a closure assumption for the incoming pair statistics, often called molecular chaos. It is not the claim that collisions create no correlations, or that every exact many-particle state always factors into independent particles. The dilute binary regime and suitable scale separation matter. A measured cross section belongs in a quantitative material prediction; none has been assigned to our example.

05

Identify what collisions cannot change

An elastic encounter between identical particles preserves the pair’s total momentum and kinetic energy, as well as its particle count. A collision invariant ψ satisfies ψ(v)+ψ(v₁)=ψ(v′)+ψ(v₁′). For the ordinary nondegenerate monatomic elastic problem the independent invariants are 1, the three velocity components, and |v|². Multiplying by fixed mass factors gives the corresponding physical momentum and energy.

The collision integral therefore obeys ∫C d³v=0, ∫m v C d³v=0 and ∫(m|v|²/2)C d³v=0. These are local collision statements. Streaming can still change the number, momentum and energy in a small region by carrying them across its boundary, and an external force can exchange momentum and energy with the gas.

A directional second moment such as ∫v_x² f d³v is not separately invariant. Neither is a fourth moment. Their relaxation is possible precisely because only the appropriate total energy is constrained. Additional species, internal states, reactions or inelastic encounters change which invariants and energy bookkeeping are appropriate.

Collision conservation and quantities that remain free to relax
QuantityLocal elastic collision integralConsequence
Particle number∫C d³v=0Encounters redistribute velocities, not total count.
Momentum∫m v C d³v=0The three components are conserved together as a vector.
Kinetic energy∫(m|v|²/2)C d³v=0Total translational energy is conserved.
Directional pressure differenceNot generally zeroEnergy may be redistributed between directions.
Fourth velocity momentNot generally zeroA distribution’s shape can change at fixed energy.
06

Match a local Maxwellian

A local Maxwellian with the same number density, flow and translational energy is M=n[m/(2πk_B T)]^(3/2) exp[−m|v−u|²/(2k_B T)]. The Boltzmann constant k_B converts temperature to energy. For this monatomic model, the matching kinetic temperature is defined by (m/2)∫|c|² f d³v=(3/2)n k_B T. Away from equilibrium this energy-based definition need not have every meaning of an equilibrium thermometer reading.

Under the usual elastic collision-connectivity conditions, a positive collision-equilibrium distribution has ln M equal to a linear combination of the invariants. The normalizable isotropic form is the Maxwellian above. Thus C[M]=0 for the full classical operator in this regime. That equation alone does not say that a spatially varying local Maxwellian solves the streaming equation.

Local equilibrium and global equilibrium are different. Nearby particles may have almost Maxwellian velocity statistics while density, temperature or mean flow varies across an apparatus. Those slowly varying conserved fields drive transport. A gas can therefore be close to local equilibrium and still conduct heat or dissipate shear.

07

Solve a matching-moment relaxation model

To make the opening question exactly solvable, assign the BGK model C_BGK=(M[f]−f)/τ, with a positive constant relaxation time τ. The Maxwellian M[f] must share f’s number, momentum and total peculiar kinetic energy. Relaxation toward an arbitrarily chosen Gaussian could violate conservation and would be a different, generally unsuitable model.

In a homogeneous force-free sample these matching moments are constant. Consequently M[f] is constant too, and the equation has the exact solution f(t)=e^(−t/τ)f(0)+(1−e^(−t/τ))M. It is a positive convex mixture, not a polynomial correction that can turn negative in a tail. The equality is exact for this assigned BGK problem, not for every Boltzmann kernel or every nonequilibrium flow.

Use σ₀=√(k_B T₀/m), dimensionless velocity w=v/σ₀ and time s=t/τ, with positive symbolic T₀ and density n₀. Write Φ=σ₀³f/n₀, so ∫Φ d³w=1. Let G_θ(w)=(2πθ)^(−3/2)exp[−|w|²/(2θ)]. Our initial distribution is Φ₀=[G₁(w−2e_x)+G₁(w+2e_x)]/2, where e_x is a unit vector along x.

The two components each have variance 1 in every direction, but their opposite drift velocities contribute to energy. Their combined mean is zero; their second moments are ⟨w_x²⟩=5 and ⟨w_y²⟩=⟨w_z²⟩=1. The conserved sum is 7, so the matching isotropic variance is θ_eq=7/3, not 1. Therefore Φ_s=e^(−s)Φ₀+(1−e^(−s))G_(7/3).

08

See directional pressure relax at fixed energy

Define the pressure tensor P_ij=m∫c_i c_j f d³v. A diagonal component measures the corresponding directional momentum flux; its unit is the pascal. The scalar kinetic pressure is p=(P_xx+P_yy+P_zz)/3. Outside an isotropic state, that average does not replace the individual tensor components.

In the example, divide P by n₀k_B T₀. The exact components are P_xx=7/3+(8/3)e^(−s) and P_yy=P_zz=7/3−(4/3)e^(−s), in these normalized units. Their sum stays 7 while their difference P_xx−P_yy=4e^(−s) decays. At one relaxation time, s=1, the difference is about 1.4715178: one time constant is not complete equilibration.

Every off-diagonal component and the heat-flux vector vanish here by reflection symmetry. Nevertheless the finite-time distribution is generally not Maxwellian. Its fourth x moment is ⟨w_x⁴⟩=49/3+(80/3)e^(−s), beginning at 43 and approaching 49/3. These are shape changes at fixed number, mean and total second moment.

At the final supplied time s=8, the pressure difference is still about 0.0013418505, strictly positive. Exact isotropy belongs to the separately labelled s→∞ limit. A plotted curve may look converged at finite resolution; the accompanying values must not teach that a finite endpoint is exactly the limit.

Directional pressure changes while total energy stays fixed

The pressure tensor is a directional momentum-flux moment. All pressures here are divided by n₀k_B T₀; s=t/τ is dimensionless. Pᵧᵧ=P𝓏𝓏 by this model’s symmetry. Markers are the seven supplied times; straight joining segments guide the eye, not additional exact time samples.

Different directions, one fixed trace

  • Pₓₓ
  • Pᵧᵧ=P𝓏𝓏
  • Trace = 7
  • Separate isotropic limit: 7/3
Different directions, one fixed tracePₓₓ falls and Pᵧᵧ=P𝓏𝓏 rise while their sum remains 7. The dashed 7/3 reference is the separate isotropic infinite-time limit.Pressure / (n₀ k_B T₀)0123456701248s = t/τ

A finite endpoint still has positive anisotropy

  • Pₓₓ−Pᵧᵧ = 4 exp(−s), supplied times
A finite endpoint still has positive anisotropyLogarithmic vertical scale of the strictly positive difference. At s=8 it is about 0.0013418505, not zero. The zero limit is not placed on a logarithmic axis.Pₓₓ−Pᵧᵧ, normalized (log₁₀ scale)0.0010.010.11401248s = t/τ

Shape changes beyond the conserved second moment

  • ⟨wₓ⁴⟩, supplied times
  • Separate infinite-time limit: 49/3
Shape changes beyond the conserved second momentThe raw fourth x moment begins 43 and tends to 49/3. Neither its initial value nor its relaxation is fixed by number, mean and total energy alone.⟨wₓ⁴⟩ (dimensionless)01020304001248s = t/τ
  • The scalar pressure is 7/3 throughout, but individual directional components are not equal until the separate limit.
  • Zero mean and zero heat flux do not establish a Maxwellian. Here every odd velocity moment cancels by reflection symmetry.
  • Physical heat flux is normalized by n₀mσ₀³; its zero vector remains zero in W m⁻². No measured viscosity or numerical kinetic entropy is inferred.

The original seven-time pressure table remains below this figure. Additional complete moment values are available here.

Exact BGK moment values at supplied times; pressures divided by n₀k_B T₀

Complete supplied moments: dimensionless normalized values, rounded to12significant digits
Complete supplied moments: dimensionless normalized values, rounded to12significant digits
s=t/τn/n₀⟨wₓ⟩⟨wᵧ⟩⟨w𝓏⟩p/(n₀k_B T₀)e/(n₀k_B T₀)⟨wₓ⁴⟩qₓ/(n₀mσ₀³)
010002.333333333333.5430
1/410002.333333333333.537.10135421520
1/210002.333333333333.532.5074842590
110002.333333333333.526.14345176460
210002.333333333333.519.94227421960
410002.333333333333.516.82175037040
810002.333333333333.516.34227900340
Separate analytic infinite-time limit; not a finite sample
Separate analytic infinite-time limit; not a finite sample
StatePₓₓ=Pᵧᵧ=P𝓏𝓏TraceAnisotropy⟨wₓ⁴⟩
s → ∞7/37049/3

On a narrow screen, scroll each graph or numeric table locally. Shapes and line styles distinguish series as well as colour.

Exact BGK moment values at supplied times; pressures divided by n₀k_B T₀
s=t/τP_xxP_yy=P_zzP_xx−P_yyTrace
05.00000001.00000004.00000007
1/44.41013541.29493233.11520317
1/23.95074841.52462582.42612267
13.31434521.84282741.47151787
22.69422742.15288630.541341137
42.38217502.30891250.0732625567
82.33422792.33288600.00134185057
09

Keep the distribution outside the plotting window

The x marginal initially has two peaks associated with the two opposite drift populations. The y marginal starts as a narrower, single Gaussian. The common equilibrium marginal has variance 7/3. Comparing both directions shows redistribution that an x-only plot could hide. These curves are ensemble velocity densities, not trajectories of individual molecules.

The supplied samples run from w=−8 to w=8 in steps of 1/20. The Gaussian mixtures themselves extend over the whole real line and are normalized there. Their positive tails outside this plotting window are not cut off physically, and the sampled curves are not renormalized to make the displayed area one.

This distinction also matters for moments: the exact pressure and fourth-moment formulas use the full infinite-domain distribution. A finite sum of plotted density samples is neither that integral nor a numerical entropy calculation. An honest finite canvas can show the important shape while its text and tables retain the complete model and its limits.

Compare the two velocity directions on the same scales

These are marginal ensemble densities in dimensionless velocity, not probabilities at one exact velocity, particle positions or trajectories. All four panels share the same axes. The initial x marginal has two opposed drift peaks; the y marginal initially has unit variance. All seven finite times are shown without renormalizing tails.

x direction: early times

  • s = 0
  • s = 1/4
  • s = 1/2
  • s = 1
  • Separate s → ∞: G₍₇/₃₎
x direction: early timesFull 321 samples for each of s=0,1/4,1/2,1, plus the separately labelled infinite-time Gaussian reference.Marginal density per unit wₓ00.10.20.30.4-8-4048wₓ = vₓ/σ₀

y direction: early times

  • s = 0
  • s = 1/4
  • s = 1/2
  • s = 1
  • Separate s → ∞: G₍₇/₃₎
y direction: early timesThe same early times and windows in the transverse direction. The z direction is identical to y for this assigned symmetric model.Marginal density per unit wᵧ00.10.20.30.4-8-4048wᵧ = vᵧ/σ₀

x direction: later finite times

  • s = 2
  • s = 4
  • s = 8
  • Separate s → ∞: G₍₇/₃₎
x direction: later finite timesFull 321 samples at s = 2,4,8, plus the separate infinite-time reference. Finite 8 is not declared exactly equal to the limit.Marginal density per unit wₓ00.10.20.30.4-8-4048wₓ = vₓ/σ₀

y direction: later finite times

  • s = 2
  • s = 4
  • s = 8
  • Separate s → ∞: G₍₇/₃₎
y direction: later finite timesThe same later times in the y direction, with the same vertical range. The reference variance is 7/3, not 1.Marginal density per unit wᵧ00.10.20.30.4-8-4048wᵧ = vᵧ/σ₀
  • The finite window is −8≤w≤8 with step 1/20. All Gaussian mixtures remain positive outside it and normalized over the whole real line.
  • The full three-dimensional distribution has conserved trace 7. The equilibrium variance 7/3 includes the energy of the two opposite drifts.
  • Native table values are rounded to 12 significant digits. The hash-bound 105-digit original model remains the numerical authority; graphs project its values to binary64 coordinates.

Expand the complete x/y table for each of the seven times and the common equilibrium reference.

All 321 supplied x/y marginal values at s = 0; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 0; density per unit dimensionless velocity
wx marginaly marginal (=z)
-83.03794142491e-95.05227108354e-15
-7.954.09566920174e-97.52768728903e-15
-7.95.50788181234e-91.11879562144e-14
-7.857.38853979324e-91.65864792706e-14
-7.89.88659820312e-92.4528552857e-14
-7.751.31962160179e-83.61829445111e-14
-7.71.75697754741e-85.32414837225e-14
-7.652.3334433988e-87.81467025177e-14
-7.63.09131025008e-81.14415649018e-13
-7.554.08509518927e-81.67099235704e-13
-7.55.38488002127e-82.43432053303e-13
-7.457.08050356508e-83.53749084761e-13
-7.49.28680922278e-85.1277536368e-13
-7.351.21501927054e-77.4143526997e-13
-7.31.58567460836e-71.06938378715e-12
-7.252.06423549432e-71.53853795056e-12
-7.22.68051767235e-72.20798996314e-12
-7.153.47210117693e-73.16082346147e-12
-7.14.48621758119e-74.51354367721e-12
-7.055.7820595179e-76.42908729075e-12
-77.43359757368e-79.13472040836e-12
-6.959.53300451562e-71.29465919383e-11
-6.90.000001219480372951.83033221702e-11
-6.850.000001556087789582.581182145e-11
-6.80.000001980649545523.63096150179e-11
-6.750.00000251475364435.09493795884e-11
-6.70.000003184912589447.131328124e-11
-6.650.000004023591228269.9567179055e-11
-6.60.000005070426032761.38667999417e-10
-6.550.000006373666190941.92641814794e-10
-6.50.000007991870553492.66955661476e-10
-6.450.000009995898353523.69013261612e-10
-6.40.00001247123564515.08814028165e-10
-6.350.00001552070352916.99826594858e-10
-6.30.00001926759837139.60143337031e-10
-6.250.00002385931827091.31400181816e-9
-6.20.00002947153387881.79378390796e-9
-6.150.00003631296515192.44263482681e-9
-6.10.00004463082858973.31788424355e-9
-6.050.00005471702172164.49550183101e-9
-60.0000669151128856.07588284982e-9
-5.950.00008162820438698.19133840348e-9
-5.90.0000993277357021.10157636247e-8
-5.850.0001205632901211.47770795865e-8
-5.80.0001459734629081.97731964062e-8
-5.750.0001762978412022.63924320357e-8
-5.70.0002123901353023.51395509482e-8
-5.650.0002552324872114.66688679759e-8
-5.60.0003059509651146.18262050017e-8
-5.550.0003658322314998.17019037854e-8
-5.50.0004363413476451.07697600425e-7
-5.450.0005191406480081.41610071302e-7
-5.40.0006161095844931.85736184456e-7
-5.350.0007293654027042.43003854108e-7
-5.30.0008612844700623.17134921672e-7
-5.250.001014524029424.12847098863e-7
-5.20.001192044101845.3610353447e-7
-5.150.001397129209026.94420235386e-7
-5.10.001633409530368.97243516238e-7
-5.050.001904881052330.00000115641190358
-50.002215924210540.00000148671951473
-4.950.0025713204680.00000190660090312
-4.90.002976266219040.00000243896074589
-4.850.003436383358210.00000311217557915
-4.80.003957725809640.00000396129909103
-4.750.004546781276270.00000502950728859
-4.70.005210467442870.00000636982517887
-4.650.005956121853590.00000804718245649
-4.60.006791484686180.0000101408520655
-4.550.007724673663520.0000127473323818
-4.50.008764150380260.0000159837411069
-4.450.00991867738040.0000199917967069
-4.40.01119726540180.0000249424712901
-4.350.01260911030750.0000310414070579
-4.30.01416351935090.0000385351967421
-4.250.01586982657480.0000477186365412
-4.20.017737297320.0000589430677565
-4.150.0197750220160.0000726259303023
-4.10.02199179964920.0000892616571771
-4.050.02439601153730.00010943404344
-40.02699548629450.000133830225765
-3.950.02979735713010.000163256408766
-3.90.03280791289520.000198655471393
-3.850.03603244455660.000241126580226
-3.80.0394750890370.000291946925791
-3.750.04313867260950.000352595682367
-3.70.04702455625820.000424780270551
-3.650.05113248561640.000510464974344
-3.60.05546044825280.000611901930114
-3.550.06000454119940.00073166446283
-3.50.06475885168170.000872682695046
-3.450.06971535402770.00103828129566
-3.40.0748638256860.00123221916847
-3.350.08019178517290.00145873080467
-3.30.08568445459140.00172256893905
-3.250.09132474911810.0020290480573
-3.20.09709329554340.00238408820146
-3.150.102968481570.00279425841488
-3.10.1089265371380.0032668190562
-3.050.1149416485480.00380976209822
-30.1209861056190.00443184841194
-2.950.1270304815350.00514264092305
-2.90.133043844430.00595253241978
-2.850.1389939991530.00687276669061
-2.80.144847757030.00791545158298
-2.750.1505712308310.00909356250159
-2.70.1561301515960.0104209348144
-2.650.1614902034250.0119122436076
-2.60.1666173718720.0135829692337
-2.550.1714783011760.0154493471344
-2.50.1760406552530.0175283004936
-2.450.1802734771290.0198373543918
-2.40.1841475413870.0223945302948
-2.350.1876356941620.0252182199152
-2.30.1907131753290.0283270377416
-2.250.193357917720.0317396518357
-2.20.1955508185220.0354745928462
-2.150.1972759784190.0395500415894
-2.10.1985209045670.0439835959804
-2.050.1992766740690.0487920185792
-20.1995380553140.0539909665132
-1.950.1993035852520.0595947060688
-1.90.1985756014740.0656158147747
-1.850.1973602287440.0720648743362
-1.80.1956673204510.0789501583009
-1.750.1935103562430.0862773188265
-1.70.1909062978660.0940490773769
-1.650.1878754059460.102264924564
-1.60.1844410211170.110920834679
-1.550.1806293134620.120009000697
-1.50.176469004730.129517595666
-1.450.1719910681580.139430566445
-1.40.167228411030.149727465636
-1.350.1622155452360.160383327342
-1.30.1569882511530.171368592048
-1.250.1515832401060.182649085389
-1.20.1460378204810.194186054983
-1.150.1403895722730.20593626872
-1.10.1346760344770.217852177033
-1.050.1289344092840.229882140684
-10.1232012864660.241970724519
-0.950.1175123908040.254059056469
-0.90.1119023547260.266085249899
-0.850.1064045177050.277984886131
-0.80.1010507532830.289691552761
-0.750.09587132394530.301137432155
-0.70.09089476343110.312253933367
-0.650.08614778547480.322972359668
-0.60.08165521743470.333224602892
-0.550.07743995678990.342943855019
-0.50.07352294807970.352065326764
-0.450.06992317754440.360526962462
-0.40.06665768248710.368270140303
-0.350.06374157223960.375240346917
-0.30.06118805755920.381387815461
-0.250.05900848533110.386668116803
-0.20.05721237557360.391042693975
-0.150.05580745796280.394479330908
-0.10.05479970537760.396952547477
-0.050.0541933623240.398443914095
00.05399096651320.398942280401
0.050.0541933623240.398443914095
0.10.05479970537760.396952547477
0.150.05580745796280.394479330908
0.20.05721237557360.391042693975
0.250.05900848533110.386668116803
0.30.06118805755920.381387815461
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0.550.07743995678990.342943855019
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0.80.1010507532830.289691552761
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5.90.0000993277357021.10157636247e-8
5.950.00008162820438698.19133840348e-9
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6.050.00005471702172164.49550183101e-9
6.10.00004463082858973.31788424355e-9
6.150.00003631296515192.44263482681e-9
6.20.00002947153387881.79378390796e-9
6.250.00002385931827091.31400181816e-9
6.30.00001926759837139.60143337031e-10
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6.450.000009995898353523.69013261612e-10
6.50.000007991870553492.66955661476e-10
6.550.000006373666190941.92641814794e-10
6.60.000005070426032761.38667999417e-10
6.650.000004023591228269.9567179055e-11
6.70.000003184912589447.131328124e-11
6.750.00000251475364435.09493795884e-11
6.80.000001980649545523.63096150179e-11
6.850.000001556087789582.581182145e-11
6.90.000001219480372951.83033221702e-11
6.959.53300451562e-71.29465919383e-11
77.43359757368e-79.13472040836e-12
7.055.7820595179e-76.42908729075e-12
7.14.48621758119e-74.51354367721e-12
7.153.47210117693e-73.16082346147e-12
7.22.68051767235e-72.20798996314e-12
7.252.06423549432e-71.53853795056e-12
7.31.58567460836e-71.06938378715e-12
7.351.21501927054e-77.4143526997e-13
7.49.28680922278e-85.1277536368e-13
7.457.08050356508e-83.53749084761e-13
7.55.38488002127e-82.43432053303e-13
7.554.08509518927e-81.67099235704e-13
7.63.09131025008e-81.14415649018e-13
7.652.3334433988e-87.81467025177e-14
7.71.75697754741e-85.32414837225e-14
7.751.31962160179e-83.61829445111e-14
7.89.88659820312e-92.4528552857e-14
7.857.38853979324e-91.65864792706e-14
7.95.50788181234e-91.11879562144e-14
7.954.09566920174e-97.52768728903e-15
83.03794142491e-95.05227108354e-15
All 321 supplied x/y marginal values at s = 1/4; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 1/4; density per unit dimensionless velocity
wx marginaly marginal (=z)
-86.62903495422e-86.39244023163e-8
-7.957.90272918076e-87.58375872886e-8
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1.050.1460287470910.224646919355
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1.150.1528495385670.203897357088
1.20.1561664556380.193664338371
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1.40.1681954649020.154565714925
1.450.1707630737750.145404929544
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1.850.181450071050.0838699509216
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20.1799165762130.0665643894816
2.050.1786719360790.061474368543
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2.60.1433323281460.0241490155341
2.650.1385970118910.0221055796546
2.70.1337079402970.0202294881664
2.750.1286915534130.018508634531
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2.850.1183830857960.0154869664941
2.90.1131435895120.0141647761972
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30.1026213285520.0118487817688
3.050.09738684537680.0108372451854
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All 321 supplied x/y marginal values at s = 1/2; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 1/2; density per unit dimensionless velocity
wx marginaly marginal (=z)
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2.90.09764525539890.0205604780818
2.950.0929681695580.0190394571806
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3.050.08371515092030.0163102545167
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81.15551374515e-71.13708772963e-7
All 321 supplied x/y marginal values at s = 1; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 1; density per unit dimensionless velocity
wx marginaly marginal (=z)
-81.83794221314e-71.82676626979e-7
-7.952.18227616924e-72.16720907196e-7
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All 321 supplied x/y marginal values at s = 2; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 2; density per unit dimensionless velocity
wx marginaly marginal (=z)
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82.50290740548e-72.49879600568e-7
All 321 supplied x/y marginal values at s = 4; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 4; density per unit dimensionless velocity
wx marginaly marginal (=z)
-82.83752768148e-72.83697126402e-7
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4.10.007393205971070.00699204699446
4.150.006761223685830.00640036171388
4.20.006176278241020.00585248788839
4.250.005635586426290.00534579441083
4.30.005136458944580.0048777508355
4.350.004676304287280.00444592891939
4.40.004252631752220.00404800351988
4.450.003863053649090.00368175289846
4.50.003505286740920.00334505847982
4.550.003177152973230.00303590411541
4.60.00287657954460.00275237489976
4.650.00260159837430.00249265558654
4.70.002350345022950.00225502865024
4.750.002121057122820.0020378720375
4.80.001912072373350.00183965665032
4.850.001721826156720.00165894360153
4.90.00154884882660.00149438128042
4.950.001391762721010.00134470226447
50.00124927894810.00120872011067
5.050.001120193990520.00108532605746
5.10.001003386171510.00097348566598
5.150.000897812022260.000872235426937
5.20.0008025025872450.000780679357015
5.250.0007165597005070.000697985606298
5.30.0006391522628680.000623383096062
5.350.0005695125465580.000556158203995
5.40.0005069325506020.000495651511813
5.450.0004507604272150.000441254628253
5.50.0004003969964730.000392407098468
5.550.0003552923637480.000348593409125
5.60.0003149426517660.000309340096758
5.650.0002788868567430.000274212965444
5.70.0002467038357990.000242814418381
5.750.0002180094308720.00021478090667
5.80.0001924537324760.0001897804974
5.850.0001697184850890.000167510562056
5.90.0001495146344870.000147695585309
5.950.0001315800161010.000130085093416
60.0001156771824280.000114451700668
6.050.0001015913666050.000100589271732
6.10.00008912857849260.000088311197122
6.150.00007811382903810.0000774487786199
6.20.00006838947815560.0000678497210379
6.250.00005981370102850.0000593767264377
6.30.00005225906744840.00005190618666
6.350.00004561122863250.0000453269698491
6.40.00003976770586170.0000395392965324
6.450.00003463677525050.0000344537007446
6.50.00003013644298510.0000299900716595
6.550.0000261935054450.000026076771205
6.60.00002274268873950.0000226498231871
6.650.00001972586234370.0000196521695234
6.70.00001709132169340.0000170329892907
6.750.00001479313479980.0000147470764134
6.80.00001279054815860.0000127542719618
6.850.00001104744745060.0000110189471813
6.90.000009531868766120.00000950953353921
6.950.000008215556317220.00000819809624752
70.000007073562838490.00000705994789692
7.050.000006083889110810.00000607329901715
7.10.000005227159270280.00000521894255883
7.150.000004486328789120.00000447996947188
7.20.000003846422231110.00000384151273218
7.250.00000329429809280.00000329051734179
7.30.000002818438241280.00000281553399652
7.350.000002408759649360.00000240653427752
7.40.000002056446309930.00000205474538088
7.450.000001753799381770.00000175250254878
7.50.000001494103779820.0000014931175091
7.550.000001271509574160.00000127076136593
7.60.00000108092670280.00000108036051167
7.659.17931635402e-79.17504251767e-7
7.77.78684747475e-77.78362946787e-7
7.756.59857278218e-76.59615581754e-7
7.85.58566850468e-75.58385771555e-7
7.854.72320628122e-74.72185302599e-7
7.93.98965275846e-73.98864395677e-7
7.953.36642967905e-73.36567953245e-7
82.83752768148e-72.83697126402e-7
All 321 supplied x/y marginal values at s = 8; density per unit dimensionless velocity
All 321 supplied x/y marginal values at s = 8; density per unit dimensionless velocity
wx marginaly marginal (=z)
-82.88894239545e-72.88893220431e-7
-7.953.42733784141e-73.427324102e-7
-7.94.06171699393e-74.06169851708e-7
-7.854.8083615636e-74.80833677786e-7
-7.85.68616279834e-75.68612963258e-7
-7.756.71701288717e-76.71696861892e-7
-7.77.92625054455e-77.9261916047e-7
-7.659.34316754694e-79.3430892689e-7
-7.60.000001100158372730.00000110014800258
-7.550.000001294049873080.00000129403616917
-7.50.000001520482969930.00000152046490575
-7.450.000001784624498460.00000178460074614
-7.40.00000209241049950.0000020923793459
-7.350.000002450652235850.00000245061147674
-7.30.000002867155473990.00000286710228089
-7.250.000003350854487870.000003350785241
-7.20.000003911962372330.00000391187245172
-7.150.000004562139392030.00000456202291707
-7.10.000005314681237770.00000531453074345
-7.050.000006184729215390.00000618453525106
-70.000007189504552220.00000718925518587
-6.950.000008348569173170.00000834824938084
-6.90.000009684115470230.00000968370638628
-6.850.00001122128776670.000011220765766
-6.80.0000129885383580.0000129878739363
-6.750.00001501802119520.0000150171776064
-6.70.00001734602646080.0000173449580656
-6.650.00002001345947120.0000200121097401
-6.60.00002306636752160.0000230646666296
-6.550.00002655651846360.0000265543804014
-6.50.00003054203497720.0000305393540928
-6.450.00003508808865370.0000350847355271
-6.40.00004026765815310.0000402634746903
-6.350.00004616235582420.000046157149443
-6.30.00005286332728250.0000528568640454
-6.250.00006047222851960.0000604642250508
-6.20.00006910228516930.0000690923991728
-6.150.00007887943856630.000078867257743
-6.10.00008994358321120.0000899286123492
-6.050.0001024499001790.000102431546171
-60.0001165702908860.000116547845404
-5.950.0001324949154460.000132467534982
-5.90.0001504338396030.000150400522555
-5.850.000170618793890.000170578354369
-5.80.0001933050483080.0001932560863
-5.750.0002187734052860.000218714272802
-5.70.0002473323131470.000247261075982
-5.650.0002793201016330.000279234496328
-5.60.0003151073402520.000315004725878
-5.550.0003550993193370.000354976623703
-5.50.0003997386527170.000399592312631
-5.450.0004495079997840.000449333895003
-5.40.0005049329034740.000504726284041
-5.350.0005665847393690.000566340146053
-5.30.0006350837695750.000634794947211
-5.250.0007111022934560.000710762097054
-5.20.0007953678855320.000794968179127
-5.150.0008886667089770.000888198257293
-5.10.0009918468911750.000991299244314
-5.050.001105821945660.00110518331719
-50.001231574222540.00123083136152
-4.950.001370158367270.00136929642494
-4.90.001522704765090.00152170715719
-4.850.001690422946170.00168927121199
-4.80.001874604923720.00187327858349
-4.750.002076628435180.0020751048472
-4.70.002297960053530.00229621427327
-4.650.002540158133610.00253816277685
-4.60.002804875555750.00280260066832
-4.550.003093862226420.00309127516335
-4.50.003408967293540.00340603261057
-4.450.003752141031580.0037488203925
-4.40.004125436350080.00412168845327
-4.350.004531009876840.0045267904048
-4.30.004971122565950.00496638416165
-4.250.005448139779430.00544283205352
-4.20.005964530790390.00595860036321
-4.150.006522867655040.00651625823748
-4.10.007125823400980.00711847591802
-4.050.007776169479270.00776802224016
-40.008476772429120.00846776134738
-3.950.009230589704960.00922064857166
-3.90.01004066461810.0100297254309
-3.850.01091012034720.0108981136976
-3.80.01184215297630.0118290084965
-3.750.01284002352110.0128256703913
-3.70.01390704891010.0138914164268
-3.650.01504659189350.0150296100974
-3.60.0162620498550.0162436502175
-3.550.01755684251320.0175369586782
-3.50.01893439850250.0189129670804
-3.450.02039814083380.0203751022425
-3.40.02195147124320.0219267705909
-3.350.02359775344510.0235713414478
-3.30.02534029531950.0253121292447
-3.250.02718233006730.0271523746967
-3.20.02912699638510.0290952249855
-3.150.03117731771770.0311437130096
-3.10.03333618065830.0333007357716
-3.050.035606312580.0355690319853
-30.03799025859210.0379511589947
-2.950.04049035792710.0404494691118
-2.90.04310871987530.0430660854898
-2.850.0458471993960.0458028776601
-2.80.0487073725450.048661436874
-2.750.05169051186830.0516430513979
-2.70.05479756192090.0547486819241
-2.650.05802911508130.0579789372658
-2.60.0613853878370.0613340505141
-2.550.0648661977260.0648138558431
-2.50.06847094112430.0684177661533
-2.450.07219857207290.0721447517495
-2.40.07604758234330.0759933202532
-2.350.0800159829410.0799614979483
-2.30.08410128724440.084046812764
-2.250.08830049597970.0882462790915
-2.20.09261008422340.092556384632
-2.150.09702599062260.0969730794654
-2.10.1015436090140.101491767523
-2.050.1061577826160.106107300638
-20.1108628009440.110813975335
-1.950.1156523996210.115605532513
-1.90.1205197631820.120475160143
-1.850.1254575310220.125415499114
-1.80.1304578065590.130418652313
-1.750.1355121696980.135476197021
-1.70.140611692660.140579200682
-1.650.145746959190.145718240073
-1.60.1509080871590.150883423884
-1.550.1560847545480.156064418699
-1.50.1612662287540.161250478311
-1.450.166441399160.166430476328
-1.40.1715988128580.171592941944
-1.350.1767267134070.176726098766
-1.30.1818130824670.181817906534
-1.250.1868456841270.186856105557
-1.20.1918121117220.191828263655
-1.150.1966998369040.196721825371
-1.10.2014962607170.201524163205
-1.050.206188766390.206222630581
-10.2107647735460.210804616254
-0.950.2152117935290.215257599832
-0.90.2195174854860.219569208085
-0.850.2236697128840.223727271686
-0.80.2276566000880.227719882027
-0.750.2314665886370.231535447745
-0.70.2350884928480.235162750577
-0.650.238511554380.238591000174
-0.60.2417254953770.241809887504
-0.550.2447205698280.244809636463
-0.50.2474876127840.247581053342
-0.450.2500180870880.250115573798
-0.40.2523041272780.252405306985
-0.350.2543385803430.254443076541
-0.30.2561150430550.256222458108
-0.250.2576278955790.25773781314
-0.20.2588723311260.258984318722
-0.150.2598443814360.259957993193
-0.10.2605409378870.260655717379
-0.050.2609597680780.261075251272
00.2610995277680.261215246043
0.050.2609597680780.261075251272
0.10.2605409378870.260655717379
0.150.2598443814360.259957993193
0.20.2588723311260.258984318722
0.250.2576278955790.25773781314
0.30.2561150430550.256222458108
0.350.2543385803430.254443076541
0.40.2523041272780.252405306985
0.450.2500180870880.250115573798
0.50.2474876127840.247581053342
0.550.2447205698280.244809636463
0.60.2417254953770.241809887504
0.650.238511554380.238591000174
0.70.2350884928480.235162750577
0.750.2314665886370.231535447745
0.80.2276566000880.227719882027
0.850.2236697128840.223727271686
0.90.2195174854860.219569208085
0.950.2152117935290.215257599832
10.2107647735460.210804616254
1.050.206188766390.206222630581
1.10.2014962607170.201524163205
1.150.1966998369040.196721825371
1.20.1918121117220.191828263655
1.250.1868456841270.186856105557
1.30.1818130824670.181817906534
1.350.1767267134070.176726098766
1.40.1715988128580.171592941944
1.450.166441399160.166430476328
1.50.1612662287540.161250478311
1.550.1560847545480.156064418699
1.60.1509080871590.150883423884
1.650.145746959190.145718240073
1.70.140611692660.140579200682
1.750.1355121696980.135476197021
1.80.1304578065590.130418652313
1.850.1254575310220.125415499114
1.90.1205197631820.120475160143
1.950.1156523996210.115605532513
20.1108628009440.110813975335
2.050.1061577826160.106107300638
2.10.1015436090140.101491767523
2.150.09702599062260.0969730794654
2.20.09261008422340.092556384632
2.250.08830049597970.0882462790915
2.30.08410128724440.084046812764
2.350.0800159829410.0799614979483
2.40.07604758234330.0759933202532
2.450.07219857207290.0721447517495
2.50.06847094112430.0684177661533
2.550.0648661977260.0648138558431
2.60.0613853878370.0613340505141
2.650.05802911508130.0579789372658
2.70.05479756192090.0547486819241
2.750.05169051186830.0516430513979
2.80.0487073725450.048661436874
2.850.0458471993960.0458028776601
2.90.04310871987530.0430660854898
2.950.04049035792710.0404494691118
30.03799025859210.0379511589947
3.050.035606312580.0355690319853
3.10.03333618065830.0333007357716
3.150.03117731771770.0311437130096
3.20.02912699638510.0290952249855
3.250.02718233006730.0271523746967
3.30.02534029531950.0253121292447
3.350.02359775344510.0235713414478
3.40.02195147124320.0219267705909
3.450.02039814083380.0203751022425
3.50.01893439850250.0189129670804
3.550.01755684251320.0175369586782
3.60.0162620498550.0162436502175
3.650.01504659189350.0150296100974
3.70.01390704891010.0138914164268
3.750.01284002352110.0128256703913
3.80.01184215297630.0118290084965
3.850.01091012034720.0108981136976
3.90.01004066461810.0100297254309
3.950.009230589704960.00922064857166
40.008476772429120.00846776134738
4.050.007776169479270.00776802224016
4.10.007125823400980.00711847591802
4.150.006522867655040.00651625823748
4.20.005964530790390.00595860036321
4.250.005448139779430.00544283205352
4.30.004971122565950.00496638416165
4.350.004531009876840.0045267904048
4.40.004125436350080.00412168845327
4.450.003752141031580.0037488203925
4.50.003408967293540.00340603261057
4.550.003093862226420.00309127516335
4.60.002804875555750.00280260066832
4.650.002540158133610.00253816277685
4.70.002297960053530.00229621427327
4.750.002076628435180.0020751048472
4.80.001874604923720.00187327858349
4.850.001690422946170.00168927121199
4.90.001522704765090.00152170715719
4.950.001370158367270.00136929642494
50.001231574222540.00123083136152
5.050.001105821945660.00110518331719
5.10.0009918468911750.000991299244314
5.150.0008886667089770.000888198257293
5.20.0007953678855320.000794968179127
5.250.0007111022934560.000710762097054
5.30.0006350837695750.000634794947211
5.350.0005665847393690.000566340146053
5.40.0005049329034740.000504726284041
5.450.0004495079997840.000449333895003
5.50.0003997386527170.000399592312631
5.550.0003550993193370.000354976623703
5.60.0003151073402520.000315004725878
5.650.0002793201016330.000279234496328
5.70.0002473323131470.000247261075982
5.750.0002187734052860.000218714272802
5.80.0001933050483080.0001932560863
5.850.000170618793890.000170578354369
5.90.0001504338396030.000150400522555
5.950.0001324949154460.000132467534982
60.0001165702908860.000116547845404
6.050.0001024499001790.000102431546171
6.10.00008994358321120.0000899286123492
6.150.00007887943856630.000078867257743
6.20.00006910228516930.0000690923991728
6.250.00006047222851960.0000604642250508
6.30.00005286332728250.0000528568640454
6.350.00004616235582420.000046157149443
6.40.00004026765815310.0000402634746903
6.450.00003508808865370.0000350847355271
6.50.00003054203497720.0000305393540928
6.550.00002655651846360.0000265543804014
6.60.00002306636752160.0000230646666296
6.650.00002001345947120.0000200121097401
6.70.00001734602646080.0000173449580656
6.750.00001501802119520.0000150171776064
6.80.0000129885383580.0000129878739363
6.850.00001122128776670.000011220765766
6.90.000009684115470230.00000968370638628
6.950.000008348569173170.00000834824938084
70.000007189504552220.00000718925518587
7.050.000006184729215390.00000618453525106
7.10.000005314681237770.00000531453074345
7.150.000004562139392030.00000456202291707
7.20.000003911962372330.00000391187245172
7.250.000003350854487870.000003350785241
7.30.000002867155473990.00000286710228089
7.350.000002450652235850.00000245061147674
7.40.00000209241049950.0000020923793459
7.450.000001784624498460.00000178460074614
7.50.000001520482969930.00000152046490575
7.550.000001294049873080.00000129403616917
7.60.000001100158372730.00000110014800258
7.659.34316754694e-79.3430892689e-7
7.77.92625054455e-77.9261916047e-7
7.756.71701288717e-76.71696861892e-7
7.85.68616279834e-75.68612963258e-7
7.854.8083615636e-74.80833677786e-7
7.94.06171699393e-74.06169851708e-7
7.953.42733784141e-73.427324102e-7
82.88894239545e-72.88893220431e-7
All 321 common infinite-time equilibrium marginal values; density per unit dimensionless velocity
All 321 common infinite-time equilibrium marginal values; density per unit dimensionless velocity
wG₍₇/₃₎ marginal
-82.8899016583e-7
-7.953.42847422695e-7
-7.94.06306152234e-7
-7.854.80995033639e-7
-7.85.68803775659e-7
-7.756.71922266689e-7
-7.77.92885143786e-7
-7.659.3462245777e-7
-7.60.00000110051718492
-7.550.00000129447041556
-7.50.00000152097513599
-7.450.00000178519961377
-7.40.00000209308149634
-7.350.00000245143384093
-7.30.00000286806440896
-7.250.00000335190968092
-7.20.00000391318517837
-7.150.00000456355381776
-7.10.00000531631416666
-7.050.00000618661062556
-70.00000719166771855
-6.950.00000835105084195
-6.90.00000968695599185
-6.850.0000112245311681
-6.80.0000129922323325
-6.750.0000150222169817
-6.70.0000173507785794
-6.650.0000200188252745
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On a narrow screen, scroll each graph or numeric table locally. Shapes and line styles distinguish series as well as colour.

10

Take moments without assuming a fluid closure

The kinetic equation connects a distribution to macroscopic balance laws by integration. Set ρ=mn and define the physical heat flux q=(m/2)∫c|c|² f d³v, with units W m⁻². The translational internal-energy density is e=(m/2)∫|c|² f d³v. These are distribution moments, not constitutive guesses.

Number balance is ∂_t n+∇·(nu)=0. Momentum balance is ∂_t(ρu)+∇·(ρu⊗u+P)=nF. For this monatomic elastic gas with the stated force, internal-energy balance is ∂_t e+∇·(eu)+P:∇u+∇·q=0. The double contraction P:∇u describes conversion between bulk motion and internal motion. Force work appears in the total-energy balance; it is not an extra direct heating term in this internal-energy equation.

These balances are exact within the kinetic model and its regularity assumptions, but they are not yet closed equations for n,u,T. Pressure and heat flux require f or further equations, whose moments involve still higher moments. Substituting a local Maxwellian gives isotropic ideal pressure and zero heat flux: useful leading behaviour, but not the dissipative correction needed for shear viscosity or heat conduction.

11

Connect small gradients to viscosity and heat conduction

A near-local-equilibrium approximation can express the pressure deviator and heat flux in terms of slowly varying fields. In the monatomic Newtonian convention used here, P_ij−pδ_ij=−μ(∂_i u_j+∂_j u_i−(2/3)δ_ij∇·u), and q=−κ∇T. The positive coefficients μ and κ are shear viscosity and thermal conductivity. Their signs oppose the corresponding gradients; the pressure tensor is not the same signed object as a positive viscous stress convention used in some fluid texts.

This approximation needs small local gradients relative to the collision scale. The Knudsen ratio Kn=λ/L_gradient compares a mean free path λ with the relevant variation length, not merely with the full apparatus length. A large container can still contain a thin boundary layer or steep shock where a uniformly small-Kn argument fails. Slow-time conditions and boundary distributions matter too.

The constitutive coefficients depend on the collision model. The uniform BGK relaxation above has no spatial gradients and does not measure a viscosity or conductivity. To obtain those coefficients from a kinetic model requires a separately controlled near-equilibrium calculation, not fitting the decay of one arbitrary far-from-equilibrium shape and declaring every transport rate equal.

Balances need a closure before they become fluid predictions

Integrating the kinetic equation gives conserved-field balances, but leaves pressure and heat flux unresolved. A controlled constitutive approximation connects those moments to gradients; the homogeneous relaxation example alone does not supply that approximation.

From kinetic moments to a conditioned fluid closure

From kinetic moments to a conditioned fluid closureA distribution gives moment balances. Constitutive information is additionally required to relate pressure deviator to strain rate and heat flux to temperature gradient.Kinetic distribution fnumber, mean, energy+ shape informationMoment balancesmass, momentum, energynot yet closedNear-local equilibriumsmall local gradientscollision + wall lawsPressure deviatorresponse to strain rateshear viscosity μHeat fluxresponse to ∇Tconductivity κ
  • Viscous shear responds to strain rate, not accumulated strain. The pressure-deviator convention here has the minus sign written in the article.
  • Heat conduction responds to a temperature gradient. No temperature gradient is present in the assigned spatially uniform example.
  • Small local Knudsen ratios, slow variation, collision physics and boundary laws limit the approximation. No universal numeric threshold or measured gas Prandtl number is added.

The original collision-invariant table is linked for the conserved quantities. The dependency graph is also stated in text below.

Collision conservation and quantities that remain free to relax

  1. Distribution f → moment balances for number, momentum and energy.
  2. Moment balances + near-local-equilibrium, small-gradient, collision and boundary assumptions → constitutive approximation.
  3. Constitutive approximation → pressure deviator −μ(∂ᵢuⱼ+∂ⱼuᵢ−2δᵢⱼ∇·u/3) and heat flux −κ∇T.
  4. These are dependencies, not measured rates, a spatial apparatus or additional numerical data.

On a narrow screen, scroll each graph or numeric table locally. Shapes and line styles distinguish series as well as colour.

12

Further: derive the collision entropy inequality

Choose one fixed phase-space measure and a fixed reference scale f_* with the units of f. Define H=∫f ln(f/f_*) d³x d³v. For microreversible elastic binary scattering with the molecular-chaos closure, symmetrizing particle exchange and incoming/outgoing pairs gives a collisional contribution proportional to −(1/4)∫B(a−b)ln(a/b), where a=ff₁ and b=f′f₁′. The remaining integration covers position, both velocities and scattering angle.

For positive a and b, (a−b)ln(a/b)≥0 because the logarithm is increasing. Thus collisions make H nonincreasing, or the corresponding kinetic entropy −k_B H nondecreasing. The expression is nonnegative before the minus sign, not strictly positive at equilibrium. Streaming carries entropy across spatial boundaries; a global monotonic statement additionally needs suitable boundary/decay conditions. Reservoirs can exchange entropy with a sample.

For BGK the same-moment requirement makes ∫(M−f)ln M d³v=0, since ln M is a linear combination of 1,v and |v|². Consequently dH/dt=(1/τ)∫(M−f)ln(f/M)d³v≤0 in the homogeneous example. This proof does not require estimating H from a finite plotting grid; no numerical H value is supplied here.

The kinetic H theorem is not a proof that fine-grained Hamiltonian Gibbs entropy must increase. Hamiltonian phase-space volume preservation keeps that full many-particle entropy constant under its own boundary and regularity conditions. The kinetic closure discards particular correlation information. Reversing a specially correlated microscopic state does not preserve the uncorrelated incoming-pair assumption used in the reduced equation.

13

Further: linearize with invariant modes visible

Write a small perturbation as f=M(1+εh) around a fixed local Maxwellian. With gain-minus-loss convention, define Lh=M⁻¹[Q(Mh,M)+Q(M,Mh)], where Q is the bilinear collision operator. Use the weighted inner product ⟨g,h⟩_M=∫Mgh d³v. Microreversibility gives −⟨h,Lh⟩_M=(1/4)∫BMM₁(h′+h₁′−h−h₁)² d³v d³v₁ dΩ≥0.

Thus this L is nonpositive; authors who define its negative use the opposite sign convention. Every additive collision invariant makes the squared difference zero. For the usual connected, nondegenerate, single-species monatomic elastic kernel and appropriate function space, the nullspace is spanned by 1,v_x,v_y,v_z,|v|². Degenerate kernels or different species and internal processes can have a different nullspace.

An equation Lh=R therefore requires ⟨ψ,R⟩_M=0 for every invariant ψ. Adding an invariant to h does not change Lh; fixing ⟨ψ,h⟩_M=0 removes this hydrodynamic ambiguity by keeping the chosen n,u,T unchanged. Orthogonality is a necessary compatibility condition, not by itself a universal existence or invertibility theorem on every function space.

14

Further: explain the fluid expansion and its single-time limitation

In a dimensionless small-Knudsen scaling, collisions enter as Q/ε. Insert f=M+εMh+… into the kinetic equation. The leading collision equation selects M; the next equation relates Lh to streaming of M. Lower-order Euler balances provide the invariant-moment compatibility conditions. Solving on the invariant complement produces the stress and heat-flux corrections. This Chapman–Enskog construction is an asymptotic closure with a regime, not a claim that every distribution is a finite polynomial fluid state.

For the constant, velocity-independent, moment-matching BGK model in three-dimensional monatomic near-equilibrium flow, the physical coefficients are μ=pτ and κ=(5/2)(k_B/m)pτ. With mass-specific heat capacity c_p=5k_B/(2m), the Prandtl number is Pr=μc_p/κ=1. Viscous and heat diffusion then have the same c_p-based diffusivity (k_B T/m)τ.

The Gaussian moments show where these coefficients come from. Write ϑ=k_B T/m for the thermal velocity variance, with units of velocity squared; it is distinct from the toy’s dimensionless θ_eq. Set D_ij=(∂_i u_j+∂_j u_i)/2. If δf=f−M is the first-order distribution correction, its relative shear term δf/M is −τ(m/k_B T)(c_i c_j−δ_ij|c|²/3)D_ij. The Maxwellian identity ⟨c_i c_j c_k c_l⟩=ϑ²(δ_ijδ_kl+δ_ikδ_jl+δ_ilδ_jk) then gives P_ij−pδ_ij=−2pτ(D_ij−δ_ij∇·u/3), matching μ=pτ.

The relative temperature-gradient term in δf/M is −τ[|c|²/(2ϑ)−5/2]c·∇T/T. In three dimensions, ∫Mc_a c_b|c|²d³v=5nϑ²δ_ab and ∫Mc_a c_b|c|⁴d³v=35nϑ³δ_ab. Their combination in q leaves 5nϑ²δ_ab, giving q=−(5/2)n k_B² Tτ∇T/m. These polynomial corrections are used asymptotically to obtain moments; unlike our exact convex-mixture solution, a truncated polynomial correction is not guaranteed positive at every arbitrarily large velocity.

The fixed Pr=1 is a limitation of the single-time model, not a universal value for gases. A fuller collision calculation can relax the shear and heat-carrying distortions differently. The reference heat-flux convention and whether a thermal diffusivity uses c_p or c_v must be stated: a fixed-density temperature equation uses c_v, whereas the conventional Prandtl definition above uses c_p. Their difference is not a numerical discrepancy to hide.

The exact positive homogeneous BGK solution can illustrate a strongly anisotropic initial state, while the transport-coefficient expansion assumes small departures and gradients. An exact solution of the toy does not certify far-from-equilibrium Navier–Stokes closure, every boundary condition, or every measured collision kernel.

15

Choose the regime and keep the boundaries

Kinetic descriptions are useful when velocity distributions matter: rarefied gas transport, non-Maxwellian relaxation, and the link between molecular encounters and macroscopic fluxes. At a wall, reflected and emitted distributions need a boundary law. Accommodation, slip, temperature jumps and kinetic boundary layers can matter even when a bulk fluid approximation works away from the wall.

Dense gases can require nonlocal finite-size and correlation corrections such as Enskog-type descriptions. Quantum degeneracy changes the occupation factors through Bose enhancement or Pauli exclusion. Reactive or inelastic encounters and internal molecular states change the collision bookkeeping. Long-range collective plasma effects need their own kinetic approximations. These alternatives are not interchangeable additions to our neutral monatomic BGK formula.

The central question remains concrete: what can change while the conserved moments do not? A distribution carries more information than n,u,T alone. A successful kinetic approximation identifies its measure, scattering assumptions, invariants, boundary conditions and closure limits, then connects its predictions to the observables actually being compared.

Worked examples

Find the matching temperature

Why is the final variance 7/3 rather than 1?

  1. Each component has unit variance, but its x mean is +2 or −2. Its raw x second moment is variance plus mean squared: 1+4=5.
  2. The y and z second moments are each 1. Their conserved total is therefore 7.
  3. An isotropic Gaussian with variance θ has total second moment 3θ. Match 3θ=7.

θ_eq=7/3. Opposite drifts cancel momentum, not their positive kinetic energies.

One time constant leaves a substantial distortion

Find the normalized pressure difference at s=1.

  1. The exact difference is 4e^(−s).
  2. At s=1, the remaining non-Maxwellian mixture weight is e^(−1), about 0.36787944.
  3. Multiplying by 4 gives about 1.4715178. The pressure trace remains exactly 7.

The difference is about 1.4715178, not zero. One time constant reduces a distortion by a factor e.

Zero flow is not equilibrium

The initial mean and heat flux are zero. What rejects an equilibrium Maxwellian?

  1. Reflection symmetry makes all odd velocity moments vanish.
  2. But P_xx=5 while P_yy=P_zz=1 in normalized units.
  3. A single isotropic Maxwellian would have equal diagonal components. The two-beam distribution fails that test even though its mean is zero.

The unequal directional pressures demonstrate nonequilibrium. Zero selected moments do not determine the whole distribution.

A finite endpoint is not the limit

How much anisotropy remains at s=8?

  1. Use 4e^(−8), without rounding the remaining weight to zero.
  2. e^(−8) is about 0.00033546263.
  3. Thus the difference is about 0.0013418505. Exact zero occurs only as s tends to infinity.

A strictly positive residual remains at the finite endpoint, even if the plotted curves appear coincident.

A normalized curve does not contain one physical particle

What does ∫Φ d³w=1 mean when Φ=σ₀³f/n₀?

  1. The velocity change of variables gives d³v=σ₀³d³w.
  2. Therefore ∫Φd³w=(1/n₀)∫f d³v=n/n₀.
  3. In the example n=n₀. A spatial volume V would contain expected particle number n₀V, not necessarily one.

The normalized integral states a density ratio of one. It is not a claim that the sample is a one-particle system.

Use the local gradient length

A mean free path is 1 μm. Compare a 1 mm variation scale with a 2 μm layer.

  1. For the 1 mm scale, Kn=(1 μm)/(1000 μm)=0.001.
  2. For the 2 μm layer, Kn=0.5.
  3. The apparatus has not changed size, but the local scale separation is very different. Boundary distributions and the particular approximation still need checking.

A small ratio based on a large bulk length does not justify the same fluid approximation inside a thin layer.

Distinguish heat-capacity conventions

For single-time monatomic BGK, compare κ/(ρc_p) with κ/(ρc_v).

  1. Use κ=(5/2)(k_B/m)pτ, ρ=mn and p=nk_B T.
  2. With c_p=5k_B/(2m), κ/(ρc_p)=(k_B T/m)τ.
  3. With c_v=3k_B/(2m), κ/(ρc_v)=(5/3)(k_B T/m)τ. The intended temperature equation determines which coefficient is relevant.

The second is 5/3 of the first. Pr=1 uses c_p; it does not make all temperature-diffusion conventions identical.

Check a proposed linearized forcing

Can Lh=1 hold with finite positive Maxwellian weight and the stated invariant structure?

  1. Number is an invariant, so the collision identity gives ⟨1,Lh⟩_M=0.
  2. The proposed right-hand side has ⟨1,1⟩_M=∫M d³v=n>0.
  3. The necessary compatibility condition fails before any inversion is attempted.

No. A correction cannot have a collision forcing with a nonzero invariant-number component in this closed elastic model.

Try it yourself

  1. Why is u not simply ∫v f d³v?

    Show the answer and reasoning

    The integral is number flux; divide by n for mean velocity.

    f is a number-density distribution, not already a normalized local probability density.

  2. Do opposite component drifts cancel their energy?

    Show the answer and reasoning

    No.

    Momentum is signed and cancels; kinetic energy contains squared speed and is positive for both drifts.

  3. If normalized P_xx is 3 and P_yy=P_zz, what are the other two components at conserved trace 7?

    Show the answer and reasoning

    Each is 2.

    Solve 3+2P_yy=7. Directional equality is an additional symmetry of this example, not a universal constraint.

  4. Does collision loss from a velocity interval mean particle destruction?

    Show the answer and reasoning

    No.

    It means redistribution out of that interval. The collision number integral is zero.

  5. Can the local density change even though ∫C d³v=0?

    Show the answer and reasoning

    Yes, through particle flux across the region.

    The number balance includes ∇·(nu); local collision conservation is not a ban on transport.

  6. Is C[M]=0 sufficient to make an arbitrary spatially varying M stationary?

    Show the answer and reasoning

    No.

    Its streaming and force terms must also satisfy the kinetic equation.

  7. What is wrong with relaxing the opening distribution toward G₁?

    Show the answer and reasoning

    It would discard the drift contribution to energy.

    The conserved trace is 7, whereas G₁ has trace 3. The matching target is G_(7/3).

  8. What fraction of the initial BGK distortion remains at s=2?

    Show the answer and reasoning

    e^(−2), about 0.13533528.

    The solution separates the fixed Maxwellian from a distortion multiplied by the positive exponential.

  9. Is the initial fourth x moment 3?

    Show the answer and reasoning

    No; it is 43.

    For a unit-variance Gaussian at mean ±2, ⟨w_x⁴⟩=2⁴+6·2²+3=43. The mixture preserves that value initially.

  10. May the supplied velocity samples be renormalized to area one and called the same model?

    Show the answer and reasoning

    No.

    The model is normalized over infinite velocity space. Its finite plotting window omits positive tails; renormalizing changes the displayed distribution.

  11. What are the units of q=(m/2)∫c|c|²f d³v?

    Show the answer and reasoning

    W m⁻².

    Mass times number density times speed cubed gives kg s⁻³, the unit of energy per area per time.

  12. For positive a and b, what sign has (a−b)ln(a/b)?

    Show the answer and reasoning

    It is nonnegative.

    Both factors have the same sign, and the product is zero when a=b. The collision H expression has a minus sign.

  13. Does the kinetic H theorem contradict conserved fine-grained Hamiltonian entropy?

    Show the answer and reasoning

    No.

    They describe different statistical objects and assumptions; the kinetic closure discards incoming correlation information.

  14. May a source call the linearized collision operator positive while this article calls L nonpositive?

    Show the answer and reasoning

    Yes, if it defines the negative of L.

    The definition and squared collision bracket fix the sign; the word alone does not identify a contradiction.

  15. Does Pr=1 from single-time BGK prove every dilute gas has Pr=1?

    Show the answer and reasoning

    No.

    It is the fixed relationship imposed by that simplified relaxation model. Full collision physics can distinguish shear and heat relaxation.

  16. Does the exact homogeneous BGK solution validate a far-from-equilibrium fluid closure near every wall?

    Show the answer and reasoning

    No.

    The homogeneous solution has no gradients or wall law; a fluid closure requires separate local scale, operator and boundary assumptions.

What to carry forward

  • Conservation fixes selected moments, not an entire velocity distribution. Opposite drifts can cancel mean flow while retaining excess directional kinetic energy.
  • The Boltzmann collision law has an incoming-pair closure and a collision regime. It is not an arbitrary exact replacement for full many-particle dynamics.
  • A moment-matching BGK target conserves number, momentum and energy. Our positive homogeneous mixture is exact for that toy, not every scattering kernel.
  • Local collision equilibrium is not automatically global equilibrium. Moment balances still require stress and heat-flux closure to become fluid equations.
  • The kinetic H inequality has measure, collision and boundary conditions. It does not assert growth of fine-grained Hamiltonian Gibbs entropy.
  • Small local Knudsen ratios, invariant compatibility, actual collision physics and boundary conditions determine the scope of transport predictions. A visually converged curve does not establish an exact limit.

References

Sources for the concepts and teaching approaches in this article.

  1. Statistical Mechanics I: Statistical Mechanics of ParticlesMehran Kardar · MIT OpenCourseWare · 8.333, Fall 2013, Lectures 8–11Course notesStatistical Mechanics I: Statistical Mechanics of ParticlesBinary collision gain and lossCollision entropy inequalityPressure tensor and moment balancesShear and heat transport conventionsocw.mit.edu
  2. Kinetic Theory · Classical GasesDavid Tong · University of CambridgeCourse notes · PDFKinetic Theory · Classical GasesThe Boltzmann equation and its assumptionsThe relaxation-time approximationdamtp.cam.ac.uk
  3. Chapman–Enskog derivation of multicomponent Navier–Stokes equationsPhilippe Arnault and Sébastien Guisset · Physics of Plasmas 29, 090901 (2022)Research paper · PDFChapman–Enskog derivation of multicomponent Navier–Stokes equationsFluid scaling, invariant moments and the expansionSymmetric collision bracketsguisset.perso.math.cnrs.fr