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Noether's first theorem

From The Invariance Itself
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Plain-language version: Symmetry and conservation

Noether's first theorem states that a continuous symmetry of an action integral produces a conserved quantity, one for each parameter of the symmetry group. It subsumes every first integral found piecemeal in this volume so far, and it explains why those integrals existed rather than merely recording that they did.

Provenance note

Symmetry to conservation, four examples.

Noether's 1918 paper is a verified source for this volume, but her mathematics and her prose stand differently. The equations below are her own, from the 1918 original, and are reproduced in her notation. The English wording is a 1971 translation still under copyright, so her prose is paraphrased throughout this page and never transcribed. Where a phrase of hers is characterised, it is characterised, not quoted. See Hamilton's principle/Sources.

Setup and notation

Noether works with independent variables x1,…,xn and dependent variables u1,…,uμ, and with the integral

I=∫⋯∫f(x,u,∂u∂x,…)dx(1)

She writes ψi for the Lagrange expressions — the left-hand sides of the Euler-Lagrange equations of Hamilton's principle/Mathematics/Several independent variables — so that the first variation is

δI=∫⋯∫∑ψiδuidx(2)

when the variations vanish at the boundary. Retaining the boundary terms instead gives an identity free of integrals,

∑ψiδui=δf+DivA(3)

where DivA=∂A1/∂x1+⋯+∂An/∂xn and A is linear in δu and its derivatives. Equation (3) holds for any f and any variation; it is the partial-integration identity of Hamilton's principle/Mathematics/Several independent variables written without discarding anything.

The two kinds of variation

A transformation moves both the independent and dependent variables:

yi=xi+Δxi,vi(y)=ui+Δui(4)

Noether distinguishes Δu, the total change, from the variation at fixed argument,

δui=vi(x)−ui(x)=Δui−∑∂ui∂xλΔxλ(5)

Equation (5) is the step most modern accounts compress, and compressing it is where sign errors come from. The correction term accounts for the fact that the field is being compared at a shifted point.

Deriving the divergence relations

Invariance of I under the infinitesimal transformation means the integral is unchanged when computed over the transformed region. Converting that region back to the original gives an extra divergence, and the condition becomes

δf+Div(f⋅Δx)=0(6)

Substituting (3) into (6) to eliminate δf,

∑ψiδui=DivB,B=A−f⋅Δx(7)

For a group with ρ parameters ε1,…,ερ, both δu and B are linear in the parameters. Equating coefficients gives ρ separate relations:

∑ψiδui(1)=DivB(1),…∑ψiδui(ρ)=DivB(ρ)(8)

Theorem I. If I is invariant under a ρ-parameter continuous group, then ρ linearly independent combinations of the Lagrange expressions are divergences. The converse also holds.

Statement paraphrased from Noether 1918, §1, Theorem I. The equations are hers; the English is this volume's.

Passing to conservation laws

Everything above is an identity, true whether or not the field equations hold. Impose them — set ψi=0, which Noether notes is what physicists call the field equations — and (8) collapses to

DivB(1)=0,…DivB(ρ)=0(9)

These are the conservation laws. Noether observes that such divergence equations had lately come to be called laws of conservation, the phrasing marking how recent the terminology then was.

In one independent variable a divergence is a total derivative, so (9) reads B(k)=const and gives ρ first integrals. That recovers the results of Hamilton's principle/Mathematics/The Euler-Lagrange equation and Hamilton's principle/Mathematics/The Beltrami identity as the one-dimensional case of a single theorem.

The two-step structure is the theorem's real content. Symmetry alone gives an identity. Symmetry plus the equations of motion gives a conservation law. The identity is the stronger statement and it survives where the field equations do not hold.

The symmetry-to-conservation table

symmetry generator conserved quantity
time translation Δt=ε energy
space translation Δxk=ε momentum, component k
rotation Δθ=ε angular momentum
Galilean boost Δx=εt centre-of-mass motion
phase rotation of a complex field Δψ=iεψ charge
scaling, when L admits it Δx=εx virial quantity

The first three rows are the classical integrals, and Hamilton derived exactly them from his characteristic function in 1834, obtaining the law of motion of the centre of gravity and the law of description of areas by considering common translations and rotations of the whole system.[1] That is Noether's theorem for a particular group, eighty-four years early, and it shows how natural the reasoning is once the action is the object of study.

Two cautions

Independent symmetries need not give independent conservation laws. Noether says so explicitly, and gives an example where the first integrals obtained satisfy a nonlinear dependency. The free particle of Hamilton's principle/Mathematics/Several dependent variables is the elementary case: energy conservation there follows from momentum conservation and is not new information.

The symmetry must be a symmetry of the action, not of the equations of motion. These differ. Equations of motion can have symmetries the action lacks, and those produce no conservation law by this theorem. The hypothesis is invariance of I.

A third point deserves its own page. Noether's theorem gives nothing useful when the group depends on arbitrary functions rather than on parameters. The "conserved" quantities then turn out to vanish identically or to be mathematically trivial. That failure is not a defect of the theorem; it is the content of the second one, and it is why there are two theorems rather than one.

Next

Hamilton's principle/Mathematics/Noether's second theorem treats the infinite-parameter case and its consequence for general relativity.

References

  1. ↑ Hamilton, On a General Method in Dynamics (1834), §6, equations (O.), (P.), (15.) and (16.). His argument is that V cannot change under a motion that alters neither configuration nor their mutual relation. ESTABLISHED source.