Gravitational anomaly

In theoretical physics, a gravitational anomaly is an example of a gauge anomaly: it is an effect of quantum mechanics — usually a one-loop diagram—that invalidates the general covariance of a theory of general relativity combined with some other fields.^{[citation needed]} The adjective "gravitational" is derived from the symmetry of a gravitational theory, namely from general covariance. A gravitational anomaly is generally synonymous with diffeomorphism anomaly, since general covariance is symmetry under coordinate reparametrization; i.e. diffeomorphism.

General covariance is the basis of general relativity, the classical theory of gravitation. Moreover, it is necessary for the consistency of any theory of quantum gravity, since it is required in order to cancel unphysical degrees of freedom with a negative norm, namely gravitons polarized along the time direction. Therefore, all gravitational anomalies must cancel out.

The anomaly usually appears as a Feynman diagram with a chiral fermion running in the loop (a polygon) with n external gravitons attached to the loop where ${\displaystyle n=1+D/2}$ where ${\displaystyle D}$ is the spacetime dimension.

Gravitational anomalies

Consider a classical gravitational field represented by the vielbein ${\displaystyle e_{\;\mu }^{a}}$ and a quantized Fermi field ${\displaystyle \psi }$. The generating functional for this quantum field is

${\displaystyle Z[e_{\;\mu }^{a}]=e^{-W[e_{\;\mu }^{a}]}=\int d{\bar {\psi }}d\psi \;\;e^{-\int d^{4}xe{\mathcal {L}}_{\psi }},}$

where ${\displaystyle W}$ is the quantum action and the ${\displaystyle e}$ factor before the Lagrangian is the vielbein determinant, the variation of the quantum action renders

${\displaystyle \delta W[e_{\;\mu }^{a}]=\int d^{4}x\;e\langle T_{\;a}^{\mu }\rangle \delta e_{\;\mu }^{a}}$

in which we denote a mean value with respect to the path integral by the bracket ${\displaystyle \langle \;\;\;\rangle }$. Let us label the Lorentz, Einstein and Weyl transformations respectively by their parameters ${\displaystyle \alpha ,\,\xi ,\,\sigma }$; they spawn the following anomalies:

Lorentz anomaly

${\displaystyle \delta _{\alpha }W=\int d^{4}xe\,\alpha _{ab}\langle T^{ab}\rangle }$,

which readily indicates that the energy-momentum tensor has an anti-symmetric part.

Einstein anomaly

${\displaystyle \delta _{\xi }W=-\int d^{4}xe\,\xi ^{\nu }\left(\nabla _{\nu }\langle T_{\;\nu }^{\mu }\rangle -\omega _{ab\nu }\langle T^{ab}\rangle \right)}$,

this is related to the non-conservation of the energy-momentum tensor, i.e. ${\displaystyle \nabla _{\mu }\langle T^{\mu \nu }\rangle \neq 0}$.

Weyl anomaly

${\displaystyle \delta _{\sigma }W=\int d^{4}xe\,\sigma \langle T_{\;\mu }^{\mu }\rangle }$,

which indicates that the trace is non-zero.

See also

• Mixed anomaly
• Green–Schwarz mechanism
• Gravitational instanton

References

• Luis Álvarez-Gaumé; Edward Witten (1984). "Gravitational Anomalies". Nucl. Phys. B. 234 (2): 269. Bibcode:1984NuPhB.234..269A. doi:10.1016/0550-3213(84)90066-X.
• Witten, Edward (1985). "Global gravitational anomalies". Commun. Math. Phys. 100 (2): 197–229. Bibcode:1985CMaPh.100..197W. doi:10.1007/BF01212448. S2CID 9145165.

External links

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This page was last edited on 21 July 2022, at 11:43