
recover
β
. Per radial shell the fitted
β
drifts from 0
.
03 to 0
.
74 (Fig. 3a), and the even residual at
β
= 1 remains 81–90% of the
β
= 0 signal. That residual is exactly second order: its ratio between
M
= 0
.
4 and
M
= 0
.
2 is 4
.
01–4
.
07. It also falls as
r
−4
, like the
β
signal itself, and not like a lattice
correction.
The residual lies in the non-geometric directions of Sec. 2.3. Grouping the fifteen edges at
each vertex and projecting onto the
k →
0 subspaces of Sec. 2.3, the even residual at
β
= 1
has 2–9% of its squared norm in the metric subspace, falling with
r
; 27–35% along the two stiff
non-geometric modes; and 63–64% in the three-dimensional complement of the stiff modes within
the non-geometric subspace, where the non-gauge null directions of
S
2
predominantly lie (10 938
vertices at 4
≤ r <
10). The
β
signal, by contrast, is 75% metric. The nonlinear terms of Eq.
(2)
therefore drive the non-geometric directions at the order of the signal, while the metric projection
of the residual is small. Along the stiff modes the lattice solution can absorb this residual through a
length correction of relative size (
a/r
)
2
. Along the other three directions, which are null at quadratic
order, linear response cannot absorb it; their amplitudes in the lattice solution would be fixed at
second order, as in degenerate perturbation theory. This is the
D
4
form of the known failure of
the Regge equations to converge pointwise on sampled solutions [
8
]. Brewin and Gentle showed,
for the Kasner cosmology, that simplicial solutions can converge while the residual of the Regge
equations evaluated on the continuum solution does not [
9
]; the same distinction underlies the weak
form below.
Variational meaning of the weak form. Which equation should a sampled continuum metric
satisfy? The first variation of the lattice action is, exactly,
δS
=
P
e
E
e
δℓ
2
e
, by Eq.
(2)
. A continuum
metric variation
δg
induces edge variations through Eq.
(4)
. At linear order in
δg
these are
δℓ
2
e
=
R
1
0
d
e
·δg
(
x
e
(
s
))
·d
e
ds
, since the affine energy is linear in the metric, plus a variation of the
geodesic correction that is suppressed by
a
2
/
(
r
Λ) for
δg
varying on a scale Λ. Up to corrections of
relative order (a/Λ)
2
this is d
e
·δg(x
e
)·d
e
. For smooth δg, therefore,
δS
smooth δg
=
X
e
E
e
d
e
·δg(x
e
)·d
e
≡ P [δg]. (9)
The continuum field equations,
δS
EH
/δg
= 0, state that the action is stationary under metric
variations. Their lattice counterpart is
P
[
δg
] = 0 for all smooth
δg
: the first variation must vanish
against metric-induced edge variations. It need not vanish separately along each of the fifteen edge
directions per vertex. Ten of these are metric patterns; the other five are degrees of freedom of
the discretization, with no counterpart in the continuum metric. The full lattice equations E
e
= 0
impose those five conditions as well. They constrain the non-geometric amplitudes discussed above,
and whether satisfying them feeds back on the metric projection is the open question stated in
Sec. 6.
P
[
δg
] = 0 is thus the lattice form of the weak, or distributional, Einstein equations. This is
also the sense in which finite-element discretizations approximate their continuum equations, and
Regge calculus admits a finite-element interpretation [
15
]. It is not a projection chosen after the
fact: it is the equation whose continuum limit is Einstein’s, and the per-edge equations contain it
together with five further conditions that have no continuum counterpart.
We impose Eq.
(9)
with static test variations
δg
=
f
(
r
)
w
(
z
)
T
, twenty-seven in all. Here
T
is
one of
ˆrˆr
, 1
3
− ˆrˆr
, or
e
4
e
4
;
f
is a
cos
2
radial bump of half-width 2
.
5 centered at
r
0
∈ {
5
,
5
.
5
, . . . ,
9
}
;
and
w
is a
cos
2
window of half-width
Z ∈ {
1
.
5
,
2
.
0
}
in
z
, taken over one period in
x
4
. All test
supports lie entirely within the interior edges. In weak form the residual at
β
= 1 falls to 1
.
8% of
the β = 0 signal (M = 0.4, Z = 2.0).
9