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PreprintarXiv licencearXiv

The price of locality: Maxwell-Cattaneo charge transport in Schwinger-Keldysh effective field theory

Abstract

We determine the conditions under which the nonlinear Maxwell-Cattaneo theory of charge transport admits a local Gaussian Schwinger-Keldysh embedding with a particular modified dynamical KMS symmetry. We show that treating the additional vector as intrinsically dissipative fundamentally modifies the entropy-current analysis: the hydrostatic generating functional no longer fixes all entropy-current improvements, which must instead be supplied independently. Subsequently we discuss the additional constraints not contained in the hydrodynamic analysis that are imposed by the modified KMS transformation becoming a symmetry of the action. We both interpret and supply the corresponding stochastic quasi-hydrodynamics.

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BibTeX
@misc{amoretti2026price,
  title = {{The price of locality: Maxwell-Cattaneo charge transport in Schwinger-Keldysh effective field theory}},
  author = {Andrea Amoretti and Matteo Anselmi and Daniel K. Brattan},
  howpublished = {arXiv},
  year = {2026},
  month = sep,
  doi = {10.48550/arxiv.2609.13378},
  eprint = {2609.13378},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2609.13378},
}
RIS
TY  - UNPB
TI  - The price of locality: Maxwell-Cattaneo charge transport in Schwinger-Keldysh effective field theory
AU  - Andrea Amoretti
AU  - Matteo Anselmi
AU  - Daniel K. Brattan
PY  - 2026
DA  - 2026/09/24
PB  - arXiv
DO  - 10.48550/arxiv.2609.13378
UR  - https://arxiv.org/abs/2609.13378
AB  - We determine the conditions under which the nonlinear Maxwell-Cattaneo theory of charge transport admits a local Gaussian Schwinger-Keldysh embedding with a particular modified dynamical KMS symmetry. We show that treating the additional vector as intrinsically dissipative fundamentally modifies the entropy-current analysis: the hydrostatic generating functional no longer fixes all entropy-current improvements, which must instead be supplied independently. Subsequently we discuss the additional constraints not contained in the hydrodynamic analysis that are imposed by the modified KMS transformation becoming a symmetry of the action. We both interpret and supply the corresponding stochastic quasi-hydrodynamics.
ER  -