Conservation follows through an explicit double-divergence chain, with its volume defect retained. Matter and gravitational contributions exchange equal and opposite amounts on the selected sector.
10. Total conservation, exchange and boundary flux
The original double-divergence chain
To follow Einstein’s actual §17 argument, define
Pμασ=qσβΓEαμβ−21δμσVα,Vα=qλβΓEαλβ.(10.1)
Here V is the indicated contraction of ΓE, distinct from the boundary vector in (7.15). Trace reversal of (9.8) gives
∂αPμασ+κJσμ=qσβJg(U)μβ.(10.2)
On U=0,ν=1 this is Einstein (52a).
Theorem 10.1 (Double divergence with its volume defect)
On the compatible metric-calculus domain in arbitrary coordinates,
∂α∂σ(qσβΓEαμβ)∂α∂σPμασ=21∂α∂β∂μqαβ,=−21∂μ∂α(qαβcβ).(10.3)(10.4)
Proof.
Expansion of the recovered Christoffel expression gives
qσβΓEαμβ=21∂μqσα+Lμασ,Lμασ=21qαλqσβ(∂λgμβ−∂βgμλ).(10.5)
Exchange α,σ and relabel λ,β to see that L is antisymmetric in its upper pair. Its double divergence vanishes, proving (10.3). Inverse compatibility gives Vα=∂βqαβ+qαβcβ. Insert this in (10.1); the triple derivatives cancel and the displayed defect remains. No field equation has been used.
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The first identity is Einstein (54); the second reduces to Einstein (55) at ν=1. Combining with (10.2) yields the full off-shell relation
κ∂σJσμ=∂σ(qσβJg(U)μβ)+21∂μ∂α(qαβcβ).(10.6)
Consequently the selected original sector obeys
∂σ(tσμ+Tσμ)=0,(10.7)
recovering Einstein (56). Outside the volume specialization the extra term is real: E=diag(1,1,1,ex3), where x is the first spatial coordinate, gives ∂α∂σPμασ=(3,0,0,0)μ.
An antisymmetric representation can replace P for this operation, but only after its difference has been accounted for. Define
Aμασ=Lμασ+21δμα∂βqσβ−21δμσ∂βqαβ.(10.8)
It is antisymmetric, and direct differentiation gives
∂αPμασ=∂αAμασ−21δμσ∂α(qαβcβ).(10.9)
At ν=1 their divergences agree. Pointwise equality of the potentials is not claimed. This is an instance of operation-specific information removal in Lemma 2.1.
Opposite matter and gravitational exchange
Define
eμ=21Tρσ∂μqρσ.(10.10)
Substitute W=U−κJg(T) into (8.3) and use gρσ∂μqρσ=−2cμ. The complete identity is
∂αtαμ=eμ+21τcμ−2κ1Uρσ∂μqρσ.(10.11)
On the coupled unit-volume sector this becomes
∂αtαμ=eμ,∂αTαμ=−eμ.(10.12)
The second equality follows from total conservation and is numbered Einstein (57). For symmetric stress, CραμTαρ=−eμ by (5.15), so
∂αTαμ=−ΓEαμβTβα,(10.13)
recovering Einstein (57a). The inconsistent unnumbered gravitational line before Einstein (57) has the opposite sign in the supplied copy; its nonzero test is included below and in Appendix A.
At the source level put Σab=ηacΣcb and
Cb=DaΣab=a,μ∑(E−1)μa(∂μΣab+ωacμΣcb−ωcbμΣac).(10.14)
The tensor-derivative intertwiner and contraction give
EbμCb=∇αTαμ=ν−1∂α(νTαμ)+eμ.(10.15)
Thus the matter conservation statement is DaΣab=0, equivalently ∇αTαμ=0. In a general chart its density expression is ∂α(νTαμ)=−νeμ, not the formula with the volume factor omitted.
A separate curvature-identity proof
The source comparison also supplies an independent algebraic route, without replacing the original argument above. Expansion gives
DF=dF+ω∧F−F∧ω=0,F∧θ=DΘ=0.(10.16)
The first follows by the product rule, d2=0 and associativity; the second uses zero torsion. Their coordinate readouts give the differential and algebraic Bianchi identities. To make the contraction explicit, metric compatibility and zero torsion give the lowered curvature pair symmetries. They can be verified at a point where C=0: there
Rρσμν=21(gρν,μσ−gσν,μρ−gρμ,νσ+gσμ,νρ),
which is antisymmetric in each pair and invariant under pair exchange. Tensor character extends the identity to every chart. Contracting ∇λRρσμν+∇μRρσνλ+∇νRρσλμ=0 first in λ,ρ and then in σ,μ yields
2∇ρRicρν=∂νR,∇αGαμ=0.(10.17)
Consequently the complete coupled residual satisfies
∇αKαμ=−κ∇αTαμ,Da(G−κΣ)ab=−κCb.(10.18)
This proves covariant matter conservation on every coupled configuration, in every chart, while preserving the distinct chart-tagged total-current construction.
Finite regions and explicit coupled checks
For a fixed bounded spatial coordinate region V in a unit-volume chart,
dtd∫VJ4μd3xdtd∫VT4μd3xdtd∫Vt4μd3x=−∫∂VJiμnioutdS,=−∫∂VTiμnioutdS−∫Veμd3x,=−∫∂VtiμnioutdS+∫Veμd3x.(10.19)(10.20)(10.21)
These follow by differentiation under the finite integral and the divergence theorem. No boundary field is required to vanish for the balance identities; constancy of a regional total requires zero net flux. The exchange cancellation requires the same realization in both summands.
A same-realization nonzero-exchange witness is
Ed=diag(r2/9,r2/9,r2/9,r−2/3),ϵd=27κ4r−2/3,Σd=diag(0,0,0,ϵd),x4=r>0.(10.22)
The stress is specified before computing curvature. The calculation gives ν=1, G=κΣd, Tαμ=diag(0,0,0,ϵd) and tαμ=diag(ϵd,ϵd,ϵd,−ϵd). In particular
e4=81κ8r−5/3,∂αtα4=e4,∂αTα4=−e4.(10.23)
This distinguishes the exchange signs in a way a zero-exchange fixture cannot.
For a finite-flux test apply the determinant-one affine transformation X=x+t, R=x+2t, Y=y, Z=z to (10.22). Recompute from Ed(R)J and Σd(R). The total current has J44=−ϵd(x+2t) and J14=2ϵd(x+2t). On the unit spatial cube,
Q4=−9κ4[(1+2t)1/3−(2t)1/3],Φ4out=2[ϵd(1+2t)−ϵd(2t)],Q4′+Φ4out=0(10.24)
for t>0. The primitive and endpoints verify the integral rather than assuming flux vanishes.
Conservation is not the full field equation. Constant nonzero stress on a flat calibration is conserved but has G−κT=0. Doubling the stress in (10.22) preserves its covariant conservation and breaks the gravitational equation. Conversely, ordinary matter divergence can vanish for a special varying metric and stress: (7.12) with Σ=η/(3κ) has Tαμ=δμα/(3κ) and e=0. A constant metric is sufficient to eliminate all such exchange terms, not necessary for every individual stress cancellation. Finally, four divergence equations do not determine ten arbitrary stress functions. Constitutive variables and their laws are addressed next rather than inferred from an equation count alone.