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The Lagrange expressions and the first variation

From The Invariance Itself


Plain-language counterpart: Nudging a path and seeing what changes.

This page does the work of the ordinary calculus of variations and stops one step short of where textbooks stop. That step is the whole point.

The first variation

Take any integral of the form (2) on the previous page — invariant or not. Form its first variation δI and reduce it by integration by parts. Assuming δu and all its derivatives that appear vanish on the boundary, and are otherwise arbitrary, this gives

δI=∫…∫δfdx=∫…∫(∑ψi(x, u, ∂u∂x,…)δui)dx(N2)

The ψi are what Noether calls the Lagrange expressions. They are the left-hand sides of the Lagrange equations of the associated variational problem δI=0.

They are expressions, not equations. Setting ψi=0 is what physics calls imposing the field equations. Noether does not do it here and does not do it in either proof. Everything up to and including both theorems is carried with the ψi left standing. That is why her results are identities, and it is the reason the second theorem says anything at all.

The integral-free identity

Relation (N2) holds only under the boundary assumption. Drop the assumption and write the boundary terms out, and what results is an identity in δu and its derivatives, with no integral sign anywhere.

Integration by parts shows those boundary terms to be integrals over divergences, that is, over expressions of the form

DivA=∂A1∂x1+…+∂An∂xn(1)

with A linear in δu and its derivatives. Therefore

∑ψiδui=δf+DivA(N3)

This is the workhorse. It holds identically, for every integral, invariant or not, on-shell or off. Both theorems are obtained by combining it with an invariance condition and nothing else.

The three special cases

Noether writes (N3) out in three cases, and the third is the one that fixes the generality of her result.

For a simple integral with f containing only first derivatives, (N3) becomes the relation Heun called the Lagrangian central equation:

∑ψiδui=δf−ddx(∑∂f∂u'iδui),(ui′=duidx)(N4)

For the n-fold integral:

∑ψiδui=δf−ddx1(∑∂f∂∂ui∂x1δui)−…−ddxn(∑∂f∂∂ui∂xnδui)(N5)

For a simple integral with ϰ derivatives of the u:

∑ψiδui=δf−ddx{∑((11)∂f∂ui(1)δui+(21)∂f∂ui(2)δui(1)+…+(ϰ1)∂f∂ui(ϰ)δui(ϰ−1))}+…+(−1)ϰdϰdxϰ{∑(ϰϰ)∂f∂ui(ϰ)δui}(N6)

A corresponding identity holds for the n-fold integral, and there A contains δu up to the (ϰ−1)th derivative.

A transcription note. In the electronic text of the German original the first bracket of (N5) reads with xi where the pattern d/dx1,…,d/dxn requires x1. It is written x1 above. Whether the slip is the 1918 printing's or the transcription's has not been checked against the page images, and Sources records it as open.

Why these define the Lagrange expressions

Noether points out that (N4), (N5) and (N6) actually define the ψi, and gives the reason in one sentence: the combinations on the right eliminate all higher derivatives of the δu, while relation (N2), to which integration by parts leads uniquely, is satisfied.

That is worth restating because it is the licence for everything after. The ψi are not postulated and are not borrowed from physics. They are whatever the reduction produces, and the reduction is unique.

Provenance: (N2) to (N6) are Noether's equations (2) to (6), reproduced in her notation from the public-domain German original, with the one deviation noted above. Equation (1) is her definition of a divergence, set as a numbered display by this volume. Her prose is paraphrased. See Sources.