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Derivative Expansion and Tensor Decomposition

At a fixed derivative order, constitutive data must be expanded in a complete set of irreducible scalars, transverse vectors, and transverse traceless tensors. Equations of motion and hydrodynamic field redefinitions remove redundant structures; discrete symmetries, dimension, curvature, sources, and anomalies determine which structures are actually allowed.

Required background. Hydrodynamic Frames and Constitutive Data supplies the field-redefinition quotient. Representations, Intertwiners, Invariants, and Tensor Decomposition explains the irreducible-representation logic.

Helpful background. Relativistic Dissipative Hydrodynamics applies the basis to physical transport.

For a normal charged fluid in four spacetime dimensions, define

D=uμμ,μ=Pμνν,θ=μuμ,aμ=Duμ.D=u^\mu\nabla_\mu, \qquad \nabla_\perp^\mu=P^{\mu\nu}\nabla_\nu, \qquad \theta=\nabla_\mu u^\mu, \qquad a^\mu=Du^\mu.

The velocity gradient decomposes into expansion, shear, vorticity, and acceleration. With the positive rest-space tensor Pμν=uμuνgμνP^{\mu\nu}=u^\mu u^\nu-g^{\mu\nu},

σμν=PμαPνβ(αuβ+βuα+23Pαβθ),\sigma^{\mu\nu} = P^{\mu\alpha}P^{\nu\beta} \left( \nabla_\alpha u_\beta+\nabla_\beta u_\alpha +\frac{2}{3}P_{\alpha\beta}\theta \right), ωμν=12PμαPνβ(αuββuα).\omega^{\mu\nu} = \frac12P^{\mu\alpha}P^{\nu\beta} \left( \nabla_\alpha u_\beta-\nabla_\beta u_\alpha \right).

The shear is transverse and traceless; the vorticity is transverse and antisymmetric. The background field supplies

Eμ=Fμνuν,Bμ=12ϵμνρσuνFρσ,E^\mu=F^{\mu\nu}u_\nu, \qquad B^\mu=\frac12\epsilon^{\mu\nu\rho\sigma}u_\nu F_{\rho\sigma},

with ϵ0123=+1\epsilon^{0123}=+1. BμB^\mu is a pseudovector, so parity determines whether it can enter an ordinary transport term.

The covariant derivative basis and its on-shell reductions are reviewed in Kovtun 2012, §2.2, pp. 21–25, Open PDF and Romatschke and Romatschke 2019, chs. 2–3.

Before using equations of motion, the parity-even candidates include

  • scalars: DTDT, DμD\mu, and θ\theta;
  • transverse vectors: aμa^\mu, μT\nabla_\perp^\mu T, μμ\nabla_\perp^\mu\mu, and EμE^\mu;
  • symmetric traceless tensor: σμν\sigma^{\mu\nu}.

Vorticity is antisymmetric and cannot directly supply the symmetric traceless viscous stress at first order. Curvature begins at two derivatives in the ordinary counting. In four dimensions BμB^\mu is parity odd; anomalous or parity-violating fluids require a separate enlarged basis.

This raw list is overcomplete.

The ideal conservation equations, including a background electric field counted at first derivative order, imply

Dϵ+wθ=0,Dn+nθ=0,waμ+μp=nEμ.D\epsilon+w\theta=0, \qquad Dn+n\theta=0, \qquad wa^\mu+\nabla_\perp^\mu p=nE^\mu.

If the susceptibility matrix

(ϵ,n)(T,μ)\frac{\partial(\epsilon,n)}{\partial(T,\mu)}

is nonsingular, the first two equations express DTDT and DμD\mu in terms of θ\theta. The momentum equation expresses aμa^\mu as a combination of spatial thermodynamic gradients and EμE^\mu; for vanishing sources its right-hand side is zero. A convenient gauge-invariant transverse force is

Vμ=EμTμ ⁣(μT).\mathcal V^\mu = E^\mu-T\nabla_\perp^\mu\!\left(\frac{\mu}{T}\right).

Thus a parity-even isotropic charged fluid has one independent first-order scalar, vector, and tensor channel:

θ,Vμ,σμν.\theta, \qquad \mathcal V^\mu, \qquad \sigma^{\mu\nu}.

The hydrodynamic frame and tensor reference fixes their signs and invariant interpretation.

Using lower-order equations inside an O()O(\partial) constitutive relation changes the stress and current only at O(2)O(\partial^2). At second order the same replacement generates definite new terms and must be performed consistently. Near a thermodynamic singularity the susceptibility matrix may fail to be invertible; then the reduction itself signals that an additional slow mode may be required.

In Landau frame, the reduced parity-even constitutive relation can be written

Tμν=ϵuμuν+pPμν+ησμνζPμνθ+O(2),Jμ=nuμ+σQVμ+O(2).\begin{aligned} T^{\mu\nu} &= \epsilon u^\mu u^\nu+pP^{\mu\nu} +\eta\sigma^{\mu\nu} -\zeta P^{\mu\nu}\theta +O(\partial^2),\\ J^\mu &= n\,u^\mu+\sigma_Q\mathcal V^\mu+O(\partial^2). \end{aligned}

In the local rest frame, ησij\eta\sigma^{ij} equals minus the conventional shear-gradient stress, so η>0\eta>0 damps velocity gradients. ζ\zeta controls expansion, and σQ\sigma_Q controls charge flow relative to energy flow. The tensor counting determines that these coefficients exist; it does not compute their values.

For multiple charges, VAμ\mathcal V_A^\mu and JAμJ_A^\mu carry charge-space indices and conductivity becomes a matrix. With broken parity, rotation, or anomalies, vorticity and magnetic-field pseudovectors can contribute nondissipative terms. A superfluid adds a Goldstone gradient and changes the representation content rather than merely adding coefficients.

A proposed basis should pass five tests:

  1. Rest-frame representation. Scalars, vectors, and tensors must transform irreducibly under the unbroken spatial rotations.
  2. Transversality and trace. Contract every vector or tensor with uμu^\mu and trace every tensor.
  3. Equation-of-motion quotient. State which lower-order equations removed each convective derivative.
  4. Frame quotient. Reconstruct TμνT^{\mu\nu} and JμJ^\mu after a general O()O(\partial) field redefinition.
  5. Source completeness. Include EμE^\mu, curvature, boundary, and anomaly structures whenever the declared background permits them.

These checks are dimension sensitive. In two spatial dimensions, identities involving the Levi-Civita tensor reduce the parity-odd basis. In curved spacetime, commuting derivatives generates curvature. A flat-space list cannot simply be declared complete on a general background.

The constitutive box in the schematic is where this page operates. Inspect the incoming hydrostatic constraints and the outgoing frame branch: a complete derivative basis must incorporate the former and quotient the latter before its coefficients are interpreted as transport data.

Hydrostatic constraints feed a box labeled constitutive tensors, frame, and derivative basis; a dashed branch removes field-redefinition data, while a separate endpoint displays ideal sound, shear, and charge modes.

The derivative basis is constrained by equilibrium variation, symmetries, equations of motion, and order-by-order frame redundancy. For the parity-even charged fluid considered here, those reductions leave one first-order scalar, vector, and transverse-traceless tensor channel. The diagram is schematic; it does not display dimension-specific identities, parity-odd sectors, anomalies, or curvature terms.

In text: enumerate all covariant first-derivative structures, decompose them into irreducible rotational sectors, eliminate ideal-equation and algebraic redundancies, and then remove frame-redefinition directions. Only after those steps may the surviving coefficients be matched to ζ\zeta, σQ\sigma_Q, and η\eta.

Verify that Vμ\mathcal V^\mu is transverse and gauge invariant, and evaluate it in a static rest frame with no electric field.

Solution

Both Eμ=FμνuνE^\mu=F^{\mu\nu}u_\nu and μ(μ/T)\nabla_\perp^\mu(\mu/T) are transverse, so uμVμ=0u_\mu\mathcal V^\mu=0. FμνF_{\mu\nu} is gauge invariant and T,μT,\mu are gauge-invariant local thermodynamic variables once the thermal twist is used, so Vμ\mathcal V^\mu is gauge invariant. In a static rest frame with E=0\mathbf E=0,

Vi=Ti(μ/T).\mathcal V^i=-T\,\partial_i(\mu/T).

The current flows down the electrochemical-potential gradient when σQ>0\sigma_Q>0, with the sign fixed by the constitutive convention above.

Counting before declaring symmetry. Parity, time reversal, dimensionality, anomalies, and background fields change the basis.

Using first-order equations as exact identities. Equation-of-motion elimination is an order-by-order field-basis choice. It changes the omitted higher-order completion.

Calling vorticity dissipative because it contains a derivative. Derivative order and entropy production are distinct classifications.

Ideal Relativistic Hydrodynamics first solves the zeroth-order nonlinear system. Relativistic Dissipative Hydrodynamics then derives attenuation and diffusion from the reduced first-order basis.

  • Kovtun, Pavel. 2012. “Lectures on Hydrodynamic Fluctuations in Relativistic Theories.” Journal of Physics A: Mathematical and Theoretical 45: 473001. DOI. Open PDF.

  • Romatschke, Paul, and Ulrike Romatschke. 2019. Relativistic Fluid Dynamics In and Out of Equilibrium. Cambridge University Press. DOI.