Diffeomorphism Noether Currents and Charges
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A diffeomorphism generated by a vector field has a Noether current even though diffeomorphisms are gauge transformations in the bulk. Diffeomorphism covariance makes that current a sum of field-equation constraints and an exact form. On shell the constraint term vanishes, so the current is locally the exterior derivative of an -form . The integral of alone is not automatically the Hamiltonian charge; boundary variations and integrability still have to be included.
Required background. The Gibbons–Hawking–York Boundary Term supplies the action and its surface variation; Presymplectic Potentials and Currents supplies field-space differential forms; and Killing Fields and Isometry Groups supplies the diffeomorphism generator and exact symmetries.
Helpful background. The Einstein Equation supplies the bulk equations; Hypersurface Normals and Tangential Projectors supplies surface orientation; and Formulations of General Relativity locates Noether charges within this volume.
Current associated with a diffeomorphism
Section titled “Current associated with a diffeomorphism”Start from
For the field variation , covariance of the Lagrangian -form gives
The diffeomorphism Noether current is therefore
Taking an exterior derivative and comparing the two variations yields
Thus is closed when the equations of motion hold. Iyer and Wald derive these identities in Iyer and Wald 1994, §4, eqs. (49)–(51), pp. 10–11, PDF.
Constraints plus an exact form
Section titled “Constraints plus an exact form”Noether’s second theorem gives the stronger off-shell organization
where is linear in the Euler–Lagrange expressions and vanishes on solutions. In a 3+1 decomposition, its lapse and shift coefficients become the Hamiltonian and momentum constraints. Hence
where means equality on shell. Exactness here is local in spacetime; global cohomology can add closed representatives, and itself is defined up to an exact -form.
For Einstein gravity with , a standard representative is
This is the Komar two-form with the normalization arising from the Einstein–Hilbert Lagrangian. It depends on the first derivative of , not only on the value of the vector at the surface. The explicit Einstein current and charge appear in Iyer and Wald 1994, §5, eqs. (61)–(64), pp. 12–13, PDF.
From Noether form to Hamiltonian variation
Section titled “From Noether form to Hamiltonian variation”Let satisfy the linearized equations and keep field independent. Combining the current variation with the presymplectic current gives
on shell, with the site’s ordering . The order of the two arguments is essential. For a covariant potential and fixed , Cartan’s identity gives the short derivation
Thus, with this ordering, define the generator by . Integrating over gives the candidate Hamiltonian variation
after fixing the compatible orientation. This expression shows why is generally incomplete: the potential term is required, and the result must be an exact one-form on the allowed solution space before a finite exists.
If is an exact symmetry, , then the bulk presymplectic pairing vanishes. The boundary integrals on distinct components must balance. This is the mechanism behind relations between a charge at infinity and a horizon contribution, but no black-hole thermodynamic law is assumed on this page. Wald identifies the horizon Noether charge entering the stationary first law in Wald 1993, pp. R3428–R3430.
Ambiguities and boundaries
Section titled “Ambiguities and boundaries”The shifts and induce corresponding shifts in and . An exact shift of vanishes on a closed integration surface, but corner terms, nonclosed cuts, or field-dependent generators can retain it. Physical comparison therefore requires the same Lagrangian representative, potential prescription, boundary conditions, and generator normalization.
Common pitfalls
Section titled “Common pitfalls”On-shell exactness is local. It does not declare every integrated charge zero; the integral is over a codimension-two boundary where need not be globally exact.
Noether charge is not automatically Hamiltonian charge. The term and integrability condition are essential.
A vector normalization is physical boundary data. Rescaling an asymptotic time translation or horizon generator rescales its charge.
Exercise: exact symmetry balance
Section titled “Exercise: exact symmetry balance”Let be an exact symmetry and let satisfy the linearized equations. Suppose has two closed boundary components and . Show the relation between their infinitesimal charge forms.
Solution
Because , the left side of the fundamental identity vanishes, and therefore
Stokes’ theorem on gives
where the minus sign reflects the induced orientation of the inner component. The two charge variations agree after both surfaces are assigned a common outward-normal convention.