Conservation Laws and Hydrodynamic Fields
Relativistic hydrodynamics evolves expectation values of the stress tensor and conserved currents. A velocity field is introduced to decompose those observables into local energy, momentum, stress, charge, and spatial flux; it is not itself a uniquely defined microscopic observable away from equilibrium.
Required background. Current Sources and Generating Functionals derives currents by varying background sources. Spacetime Currents, Stress Tensors, and Charge Algebras fixes the stress-tensor and charge conventions used here.
Helpful background. Hydrodynamic Effective-Theory Architecture explains the derivative expansion that later closes these equations.
Source-covariant conservation laws
Section titled “Source-covariant conservation laws”For a nonanomalous current coupled to a background gauge field and a stress tensor coupled to ,
The second Ward identity includes the work and force supplied by the external field. In a local inertial frame its time component is the power density and its spatial components are the Lorentz-force density, once the displayed definition of is used consistently. If the current is anomalous, if translations are explicitly broken, or if dynamical electromagnetism is included, the right-hand sides and field content must be changed rather than hidden inside a constitutive coefficient.
Decomposition relative to a velocity
Section titled “Decomposition relative to a velocity”Choose a future-directed unit timelike field , , and the positive rest-space metric . The most general symmetric stress tensor and current decompose as
with
This irreducible decomposition and its relativistic-fluid interpretation are developed in Kovtun 2012, §2.1, pp. 15–21, Open PDF and Rezzolla and Zanotti 2013, ch. 2.
The scalars and fluxes are obtained directly from the physical tensors:
In the local rest frame, , , and . The spatial stress splits into its average and traceless part . These relations are identities for any chosen ; hydrodynamics enters only when the components are expressed locally in terms of slow fields and sources.
Hydrodynamic frame and tensor reference
Section titled “Hydrodynamic frame and tensor reference”The table is the canonical convention and translation reference for Chapters 11–12. Every equality is in the site’s convention; denotes spacetime dimension.
| Object | Definition in this volume | Local-rest-frame or invariant check | Status under a first-order frame redefinition |
|---|---|---|---|
| Metric and velocity | , | Convention fixed; itself is frame dependent | |
| Rest-space metric | , | Changes when changes | |
| Derivatives | , | , at rest | Basis elements mix only at the next retained order |
| Expansion and acceleration | , | Frame dependent | |
| Shear | transverse and traceless; is the usual negative viscous shear stress | Tensor coefficient is invariant at first order | |
| Vorticity | transverse and antisymmetric | Not an independent parity-even first-order stress term | |
| Stress and current | ; | reconstructing must give the original tensors | and are invariant; components are not |
| Ideal data | , | Equation of state is invariant; its field coordinates change | |
| Landau frame | through the chosen order | is the timelike energy-flow eigenvector when it exists | A matching convention, not an observable condition |
| Eckart frame | through the chosen order, requiring | follows charge flow | Singular at and not automatically stable or causal |
| Invariant diffusion current | unchanged when , | Frame invariant through first order | |
| Invariant scalar stress | removes shifts along the equilibrium equation-of-state surface | Frame invariant through first order | |
| Physical linear data | retarded poles, residues of fixed operators, Kubo coefficients | compute from correlators | Invariant through the consistently transformed truncation order |
This is the chapter’s canonical translation table. Its scientific check is reconstruction: after any field redefinition, rebuild and and verify equality through the retained derivative order.
Ideal variables and entropy
Section titled “Ideal variables and entropy”Local equilibrium supplies the zeroth-order functions
and the thermodynamic identities
The entropy current is not an additional exactly conserved microscopic current in a generic interacting theory. At ideal order follows from energy and charge conservation and obeys for smooth solutions. Dissipative corrections produce entropy and allow improvement ambiguities; the inequalities derived from them are treated on Onsager Reciprocity and Entropy Production.
Component check with an external field
Section titled “Component check with an external field”In flat spacetime about rest, take , , and . The Ward identities reduce to
up to the order at which products of perturbations are retained. The first equation checks the sign of external work; the second checks that momentum of the matter sector alone is not conserved in a fixed electromagnetic background. If the electromagnetic field is dynamical, its stress tensor must be included so that the total stress is conserved.
Common pitfalls
Section titled “Common pitfalls”Treating a decomposition as a constitutive law. Writing is kinematics. Predictive content starts only after the components are specified as functionals of the slow fields and sources.
Calling entropy an independently conserved charge. Entropy advection is an ideal, smooth-flow consequence. Dissipation, shocks, and fluctuations change the statement.
Forgetting improvements and magnetization. Local representatives of and can contain identically conserved pieces. Integrated charges and properly defined transport response remain the comparison targets.
Where this leads
Section titled “Where this leads”Local Equilibrium and Hydrostatic Constraints determines which parts of these constitutive tensors follow from a stationary generating functional. Hydrodynamic Frames and Constitutive Data then derives the transformations summarized in the reference table.
The schematic places the Ward identities at the entrance to the constitutive construction. Inspect especially the dashed frame-change branch: it changes the fields used to decompose and , not those physical tensors themselves.
The physical inputs are the source-covariant conservation laws and the tensors and . Local equilibrium and hydrostatics constrain their constitutive form; a hydrodynamic frame only chooses coordinates on that form. The final mode box refers to the ideal-order truncation. The diagram is schematic and does not encode coefficient values or a causal initial-value theorem.
In text: decompose the fixed tensors relative to a chosen , match , , , energy flux, charge flux, and viscous stress, and translate those components order by order under field redefinitions. Ward identities and observable correlators survive that translation even though individual constitutive coefficients need not.