The marginal substrate: why a jammed arrangement flows
A jammed packing at the isostatic margin z=2d has zero shear reserve—the relaxed shear modulus vanishes, G_relaxed∝(z-2d)→0, while the bulk modulus stays finite—so it shears freely, resists compression, and carries one elastic speed c_s²=B/ρ: it is a fluid. [GATE]
A jammed packing at the isostatic margin z=2d has zero shear reserve—the relaxed shear modulus vanishes, G_relaxed∝(z-2d)→0, while the bulk modulus stays finite—so it shears freely, resists compression, and carries one elastic speed c_s²=B/ρ: it is a fluid. We reproduce this locally (bootstrap z₀=5.99, CI [5.49,6.29]ni 6) and inherit the companion's five-observable verification; rotation, costing a rigid packing nothing yet shearing a differential one, is the unjamming switch. The same two rules fix the laminar–turbulent transition's universality class as directed percolation—confirmed by experiment (2016–2024) and by five exponents measured in this bundle.
A0 calls the medium "a coarse-grained, jammed configuration of finite-volume particles." Before the axioms say how such a configuration interacts, there is a prior question the rest of the document silently leans on: why should a jammed configuration flow at all? Jammed packings are, after all, solids. This section answers it with the central inherited result of the companion whitepaper (VP Theory, concept DOI 10.5281/zenodo.17932566), reproduced locally, at reduced size, inside this bundle: a packing at the isostatic margin is the special solid whose shear rigidity is exactly zero while its compressive rigidity is not—which is the mechanical definition of a fluid. Everything in this section is dimensionless; nothing imports the companion's dimensional anchor (Section §14).
Counting constraints: where
comes from
Let a packing of frictionless particles in
dimensions touch through
contacts; the mean coordination is
. Each contact is one scalar
constraint (it fixes one inter-particle gap); each particle carries
degrees
of freedom. For the packing to be rigid the constraints must pin the
degrees of freedom (global rigid motions aside, an
correction
at large
):
is isostatic: exactly enough contacts to be rigid, with
not one to spare—rigid the way a structure with zero redundancy is rigid;
remove anything and it moves. The whole section lives on the distance to this
margin,
The fluidity theorem: zero shear reserve at the margin
Two moduli describe the linear mechanics of a packing. The affine
(Born) moduli are what the contact network would resist if every particle
followed the imposed strain homogeneously; the relaxed moduli let the
particles re-equilibrate after the strain (the non-affine relaxation),
is the Hessian of the contact energy on the rigid backbone and
is the force mismatch the affine
strain leaves behind. The relaxed modulus is what a rheometer measures.
[DERIVE] (inherited locally reproduced) — the marginal packing is a fluid
As the margin is approached, the relaxed shear modulus vanishes linearly while
the bulk modulus stays finite:
and
deforms under arbitrarily small shear yet resists
compression and transmits longitudinal sound: that is a fluid, by mechanical
definition. Fluidity is therefore not an assumption of A0; it is a
property the marginal arrangement earns.\\
Provenance. Verified in the companion bundle (jamming-spine
verification v0.4, concept DOI 10.5281/zenodo.17932566) on five independent
observables (table below), and reproduced locally at reduced
by
marginal_fluidity.py (box below).\\
Failure mode. A correctly prepared, accepted ensemble whose bootstrap
excludes
as
grows, or whose
collapses together with
,
falsifies the statement (Section §14, row 0).
The companion's verification is worth tabulating, because its strength is the independence of the observables that all point at the same margin:
| Observable (companion) | Behaviour at the margin | Measured |
|---|---|---|
| Relaxed shear modulus | ||
| Soft-mode onset | vanishes at isostaticity | |
| Viscosity proxy | diverges as | confirmed |
| Quasistatic yield stress | ||
| Athermal stress relaxation | residual | confirmed |
| Bulk modulus (the contrast) | stays |
Local reproduction — marginal fluidity at reduced (
marginal_fluidity.py)
D bidisperse harmonic spheres,
,
packing fractions
seeds
packings; Born moduli, mismatch vector and Hessian
assembled analytically and self-verified against finite differences (Born
,
,
); the
non-affine term by a pinned positive-definite Cholesky solve with
iterative refinement—never an eigendecomposition pseudoinverse (the soft-mode
over-subtraction trap; algorithm box, Appendix Appendix B).
- Fluidity intercept: pooled fit
gives
, bootstrap
CI
(
); per size,
:
,
:
. PASS
- Monotone:
over
-quartiles
. PASS
- Bulk survives: lowest-
quartile
vs
—the shear reserve dies an order of magnitude ahead of the compressive one. PASS
- Acoustic:
is size-independent to
(
vs
in bundle units), softened below the affine Born value by the non-affine relaxation,
(companion, larger
:
). PASS
- Ledger:
accepted (jammed, positive-semidefinite, residual force
); negative
kept-not-clamped:
occurrences here (
kept in the companion's larger runs). PASS
Rotation is the unjamming switch
The margin does not only make the medium shearable; it singles out rotation as the operation that fluidizes it—the substrate-level origin of this document's rotational theme.
Two elementary facts, both verified in unjam_inflow.py. (i) A
rigid rotation changes no
bond length at first order, identically:
(measured
)—rotation per se costs the packing nothing.
(ii) Any differential rotation is locally a shear, and the strain a
shear can impose before breaking a contact is bounded by that contact's
overlap. Across the ensemble the overlap distribution collapses with pressure
(quantile correlations
,
; densest-to-marginal ratio
): the shear reserve is the overlap, and it vanishes at the
margin. Hence at
any rotational shear, however small, exceeds
the reserve, breaks contacts, and unjams the neighbourhood: rotation is
the fluidization switch. The unjammed material then moves along the one
direction the rotating demand leaves open—inward—which is the geometric
origin of the directed-inflow nozzle (
) that Mechanism M and gate
G-Q use downstream (Section §11); there it now enters as
derived geometry, not as a postulate.
The acoustic face: one speed survives
At the margin the packing keeps exactly one stiffness, , hence exactly one
elastic wave—longitudinal sound at
): the defining acoustic
signature of a fluid. The local measurement above puts numbers on it (
size-independent to
; non-affine softening
), and Pillar I
derives the same speed from the balance laws by linearization
(Section §6). What is not done here: the companion's
identification of the full-jamming elastic speed with the invariant speed of
light rests on its dimensional anchor and is neither used nor claimed in this
document (Section §14).
The constitutive ladder: where each closure lives
The margin organizes the constitutive zoo of continuum mechanics on a single
axis. Reading downward:
- Deep in the jammed phase (
large): finite
and finite yield stress—an elastic/plastic solid.
- Approaching the margin:
and
vanish while the viscosity proxy grows—yield-stress and shear-thinning rheology; this is the regime where the Newtonian gate of Pillar I fails in exactly the long-memory, force-chain way it names.
- At and just past the margin (
): zero shear reserve, finite
—the Newtonian fluid is the leading small-Deborah, locally isotropic response of the barely unjammed medium. The Newtonian-closure gate of Pillar I is thereby located on this axis rather than free-floating (its content and [GATE] status are unchanged; its position is the new information).
Why a driven medium sits at the margin (G-SOC)
One gate remains, and it is the hinge between this section and the dissipation pillar: why should a flowing medium be at the margin at all times?
[GATE] G-SOC: driven marginality (self-organized criticality)
Statement. Drive unjams (pushes down toward
); rest re-jams
(pulls
up). A continuously driven medium is squeezed from both sides and
pins at marginal coordination—self-organized criticality with
as the critical manifold. If true, the substrate of any flowing medium is
permanently marginal, and the event channel of Pillar IV is permanently
available.\\
Status. The companion verification observes the pinning: under slow
shear with re-jamming, the steady contact pressure parks at
–
regardless of the starting point (concept DOI
10.5281/zenodo.17932566). What is demonstrated is pinning near the
margin; what is not demonstrated—there or here—is arrival
exactly at
under drive. The companion flags this as its own open
loop; we inherit the flag, not the conclusion.\\
Falsification route. Drive a marginal packing at a fixed slow rate
with re-jamming and track the steady
(equivalently
) across drive
amplitudes and seeds. Systematic drift of the steady value with drive or
preparation—instead of pinning—falsifies self-organized marginality, and
with it the identification of sustained flow with sustained criticality.
The transition test: a 140-year problem lands where the substrate says
The G-SOC rules are not decoration; they make a parameter-free, checkable statement about one of fluid mechanics' oldest unsolved problems. The laminar–turbulent transition has resisted classification since Reynolds (1883). Its structure is peculiar and well documented: laminar pipe flow is linearly stable at every Reynolds number, so turbulence cannot arise spontaneously—it spreads only by contact from regions already turbulent—and it can locally die. "Drive unjams, rest re-jams," read at the scale of turbulent patches, is this structure: an absorbing (laminar) state, local contagion, local recovery.
[DERIVE] — the substrate rules fix the universality class of the transition
A locally interacting system with a unique absorbing state and no additional
symmetry has, generically, one continuous-transition universality class:
directed percolation (DP). The G-SOC dynamics of \S§3 is such a
system, so the framework fixes the class in advance, with no fluid
input. This is the class the experiments found: quasi-1D Couette (2016,
), channel flow (2016, four exponents and a scaling relation),
and—closing the question—pipe flow itself (2024), whose authors name the
phase above threshold a jammed phase of puffs. A hard problem, solved by
others, lands exactly where the substrate says it must.\\
Local verification. The rules were transcribed literally to a lattice
(pseudogap reserves
, demand-exceeds-reserve unjamming,
probabilistic re-jam) and five independent exponents were measured with no
tuning (
transition_dp.py, three stages; box below). All five land on
DP; mean-field and compact-DP are excluded.\\
Falsification route. A subcritical shear-flow transition conclusively
shown to lie outside DP breaks the category claim; within the lattice, any of
the five gates failing on rerun breaks the transcription.
Transition class — five exponents, no tuning (transition_dp.py
_refine
_final)
1D ring; per-site reserve from the marginal pseudogap (,
flagged); inactive site unjams when demand
exceeds
its reserve; active site re-jams with probability
; toggled sites
redraw.
by curvature-minimised bisection.
| exponent | measured | DP ( | |
|---|---|---|---|
| decay | PASS | ||
| lifetime | PASS | ||
| hyperscaling | PASS | ||
| spreading | PASS | ||
| activity corr. | PASS |
The pseudogap exponent is a flagged parameter precisely because the class must
not depend on it; that independence is the content of universality. (The SOC
avalanche exponent at below threshold has a cutoff exceeding
and is reported with thin statistics, not gated.)
One of these predictions is now closed and one boundary stated. (i) At
transitional criticality the turbulent-fraction box roughness decays as
, an exponent that must track the spatial dimension of the
DP class. Running the same G-SOC rules on a 2D lattice (4 neighbours
d DP) and measuring the box roughness in the critical
quasi-stationary state gives the result below.
Transition roughness in quasi-2D — d DP (
transition_dp_2d.py)
The 1D ring of the box above becomes an lattice; the absorbing laminar
state, the marginal-stability reserves (
) and the re-jam
are
unchanged — only the dimension changes, which is the universality statement.
is located by the survival transition; in the critical state the
box-roughness
is a clean
power law in
.
- Quasi-2D roughness.
(6 realisations,
), against the
d DP value
. PASS
- Dimensional scaling captured. With the quasi-1D measurement
(
) the measured 2D/1D ratio is
against the DP ratio
; both dimensions sit
5–7% low — a single, consistent finite-size bias, not a class mismatch.
(ii) The superexponential puff lifetimes are the extreme-value (Gumbel)
statistics of the weakest reserve inside a puff. And one boundary, stated plainly:
the transition fixed point does not give the intermittency of developed
turbulence ( against the
d DP value
).
Developed flow is the driven phase beyond the transition; its exponents
belong to the event RG and stand as that program's open problem.
What is inherited, what is local, what is not imported
For auditability, the boundary of this section in one place. Inherited
and locally reproduced: the fluidity theorem and the acoustic ratio
(Table §3 and the box above). Inherited as derived
geometry: rotational unjamming and the directed inflow
(\S§3); the forced-radius attractor structure
(Section §8). Inherited as a graded gate: G-SOC
(\S§3). Deliberately not imported: the companion's mass
ladder, its and
derivations, its absolute (dimensional)
anchors, and its speed-of-light identification. Citations use the concept DOI
only; the companion's grades translate by the rule stated in "How to read
this document."