The quadratic gravitational effective stress-energy tensor depends on the split between the fixed background and the metric perturbation. A residual gauge symmetry of linearized gravity changes without changing the first-order tidal field, but generally changes and hence the local value of . At second order the compensating change of restores the same physical geometry; assigning only the quadratic term to an energy density loses this compensation.
Moreover, a stress-energy superpotential can change the local energy expression while preserving its divergence and, with suitable boundary behavior, its integrated charges. Symmetry and flat conservation do not make a unique, gauge-independent local gravitational energy density. Averaging in an appropriate short-wavelength regime can lead to a useful physical gravitational-wave energy flux, but that is a qualified approximation, not a cure for the local definition requested here.
Expand the Einstein tensor about the Minkowski metric, keeping a second-order metric perturbation as well:
Here includes all quadratic terms from the Einstein tensor, including the inverse-metric corrections in its contractions. In vacuum, the first-order Linearized Einstein equations give , while the next order gives . Define the quadratic gravitational effective stress-energy tensor by
It is symmetric because the Einstein tensor is symmetric, and is quadratic in and its derivatives. The linearized contracted Bianchi identity is the off-shell identity . The second-order vacuum equation therefore implies
One can obtain the same conclusion directly by expanding the full contracted Bianchi identity to second order: every correction to the flat divergence multiplies and vanishes on the first-order vacuum solution. Thus conservation holds for vacuum solutions of linearized gravity, rather than for an arbitrary off-shell . Relative to the fixed Minkowski background, is a tensor under background changes of coordinates, but this does not make it invariant under the perturbative gauge freedom.