FROSTYVERSE TEST H2-086 — SIX-SUPPORT RELEASE / GRADIENT-COMMITMENT AUDIT

CURRENT WORKING NARRATIVE
-------------------------
The ordinary dispersion response D describes the motion-strain cost carried by the FQ. During FrostTransit, that carried state must be reconciled with the complete six-support 3D FrostNode environment. The squared transverse opening demands of those six supports contain a natural multiplicity of four. At the effective level, this makes the FrostTransit response behave as an additional 4D.

HYPOTHESIS H2-086 TRIES TO TEST
-------------------------------
At FrostTransit start, the six incident FrostSegments collectively participate in releasing/reconciling the FQ/SFN from the source FrostNode and handing the same carried state to the destination FrostNode. The collective six-support release/capture work may be the physical process behind the structural factor four during a gravity-gradient crossover.

WHAT IS NEW VS H2-085
---------------------
H2-085 established the structural identity:

    sum_i [1 - (u . s_i)^2] = 4

for the six incident supports, and showed that it remains effectively 4 in the deformed FrostGrid.

H2-086 asks whether the number also appears in inherited RELEASE WORK:

    q_i = required transverse opening of support i
    E_open = 1/2 k sum_i q_i^2

At H-021's derived critical stiffness kcrit, E_open is compared directly with the inherited H-019 arrival work. The same six-support work ledger is then partitioned through the inherited H-057 finite-FQ source/destination engagement.

A PASS therefore strengthens the narrative from:

    "the geometry has a four"

to:

    "the inherited node-release/opening work and source->destination handoff carry that four conservatively."

FINITE-BODY / GRADIENT IDEA
---------------------------
H2-086 also tests the suggestion that a finite FrostStructure might need some fraction of its body to enter the next gravity-depth region before collective handoff.

A sphere crossing a local gradient surface is tested coefficient-free by its exact deeper-side volume and surface fractions. Forward and reverse traversal are compared exactly.

If those fractions are mirror-symmetric, then a pure "fraction crossed" rule cannot by itself make inward motion harder than outward motion. A real carried state, memory, rate/cadence effect, or other physical readout would be required for such an asymmetry.

IMPORTANT RESOLUTION LIMIT
--------------------------
The current H2 orbit engine is effectively pointlike at the planet/FrostStructure scale. H2-086 freezes approximate terrestrial-planet mean radii ONLY as an external resolution diagnostic. It calculates how many R20/R40/R80 FrostGrid cells span each planet's physical diameter and how fine R would need to be for 4, 8, or 16 cells across the diameter.

Planet radii NEVER enter the perihelion closure or candidate coefficient.

WHAT A SUCCESS WOULD AND WOULD NOT MEAN
---------------------------------------
A strong result would support this provisional chain:

    inherited six-support node geometry
        -> fourfold transverse opening-work ledger
        -> conservative source/destination FrostTransit handoff
        -> effective extra ~4D response

It would still NOT derive the final microscopic equality between one generalized release/opening work unit and the already established dispersion unit D. That last identification remains the narrow black-box bridge unless later mechanics derives it.
