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FROSTYVERSE TEST H2-086 — SIX-SUPPORT RELEASE / GRADIENT-COMMITMENT AUDIT
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version:  2.0.86-six-support-release-gradient-commitment-audit
patch:    h2-085-release-work-ownership-finite-fq-handoff-gradient-commitment-resolvability-1
baseline: Frostyverse-Test-H2-085.zip sha256=41e38feb768b1425694fda912c9e945a68bfdf99bf9850e4d852642fb9926531
python:   3.10.6
profile:  full; R=(20, 40, 80); workers=6

TEST 01 - CONTRACT / CAN THE RELEASE HYPOTHESIS ACTUALLY BE TESTED?
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R01  [NO-NEW-4]  No release coefficient is fitted. The fourfold work ratio must emerge from inherited H-019/H-021 mechanics.
R02  [DIRECT-RELEASE]  Use H-019 arrival work, H-021 six-support openings, H-021 critical stiffness, and conservative closure.
R03  [TRANSFER]  Use inherited H-057 finite-FQ source/destination engagement; no fitted handoff width or elapsed-time rule.
R04  [GRADIENT]  Use each body own local n=log(N) profile to test forward/reverse handoff through an actual one-cell gravity-depth difference.
R05  [FINITE-BODY]  Test sphere fraction-across-gradient geometry coefficient-free; any inward/outward bias must survive exact reversal.
R06  [RESOLVABILITY]  Do not pretend R20/R40/R80 resolves a literal planet diameter. Quantify planet diameter in FrostGrid cells.
R07  [BLACK-BOX-BRIDGE]  Only after local tests, apply the measured release-work multiplicity to existing D as a transparent effective bridge.
R08  [FAILURE-MATTERS]  If geometric release is exactly reversible, reject pure fraction-crossed hysteresis; a carried state would still be required.

TEST 02 - DIRECT SIX-SUPPORT RELEASE/OPENING WORK OWNERSHIP
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  cases=246 measured release-work multiplicity mean=4.000000000000 range=4.000000000000..4.000000000000
  multiplicity spread=3.553e-15; max opening-work / H-019 arrival-work mismatch=0.000e+00
  conservative snap-close max relative energy mismatch/drift=3.855e-08; max time error=3.254e-14
  interpretation: at H-021 kcrit, the full six-support opening work is exactly the H-019 arrival work; measured against one full transverse support mode, the inherited release ledger supplies the structural multiplicity.

TEST 03 - EXISTING FINITE-FQ SOURCE RELEASE -> DESTINATION CAPTURE LEDGER
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  finite-fq  max conservation=2.665e-15 mirror/reversal=5.551e-16 interval destination shift=3.827853518 (95.6963% of ledger)
  linear     max conservation=0.000e+00 mirror/reversal=5.551e-17 interval destination shift=4.000000000 (100.0000% of ledger)
  interpretation: H-057 partitions the same release ledger between source and destination. It does not create extra energy; finite FQ overlap means one cell interval begins/ends partially shared.

TEST 04 - ACTUAL GRAVITY-DEPTH CROSSOVER: DOES GEOMETRIC HANDOFF ITSELF FAVOR INWARD VS OUTWARD?
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  building inherited FV field/profile R=20 ...
    Mercury release C=4.000000096811 required C=3.997834624 total err=+0.036091%
  building inherited FV field/profile R=40 ...
    Mercury release C=4.000000012096 required C=3.998159412 total err=+0.030677%
  building inherited FV field/profile R=80 ...
    Mercury release C=4.000000001513 required C=3.997651999 total err=+0.039133%
  max inward-vs-exact-reversed-outward effective-depth difference = 6.758e-16 relative
  interpretation: if this is numerical zero, existing geometric release/capture plus local depth is reversible. A simple harder-in/easier-out hysteresis is NOT generated by these ingredients alone.

TEST 05 - FINITE FROSTSTRUCTURE FRACTION-ACROSS-GRADIENT GEOMETRY
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  exact sphere half-volume at center crossing=0.500000000000; half-surface=0.500000000000
  forward+reverse volume symmetry error=2.220e-16; surface symmetry error=0.000e+00
  interpretation: a pure fraction-crossed rule is geometrically reversible. It can define when a finite body spans a gradient, but cannot by itself make inward transit harder than outward transit without memory/state or another asymmetric physical readout.

TEST 06 - REAL-PLANET DIAMETER / GRAVITY-SPAN / CURRENT GRID RESOLVABILITY
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  MERCURY    diameter=4879.4 km | at R80: 0.013482 cells | peri 1/r span=0.010607% | R for 8 cells~47472
  VENUS      diameter=12103.6 km | at R80: 0.033442 cells | peri 1/r span=0.011262% | R for 8 cells~19138
  EARTH_EMB  diameter=12742.0 km | at R80: 0.035205 cells | peri 1/r span=0.008662% | R for 8 cells~18179
  MARS       diameter=6779.0 km | at R80: 0.018730 cells | peri 1/r span=0.003280% | R for 8 cells~34170
  largest real-planet diameter represented at R80 = 0.035205 FrostGrid cells
  interpretation: the present orbit engine cannot honestly resolve a literal whole-planet layer-by-layer gradient crossover when diameter << one cell. That macro mechanism would need much finer R or a validated sub-grid finite-FrostStructure model.

TEST 07 - RELEASE-WORK MULTIPLICITY AS THE EXISTING D BLACK-BOX BRIDGE
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  MERCURY    required C=+3.997651999 release-structural C=+4.000000002 total err=+0.03913%
  VENUS      required C=+3.986821296 release-structural C=+4.000000000 total err=+0.21965%
  EARTH_EMB  required C=+3.999740457 release-structural C=+4.000000000 total err=+0.00433%
  MARS       required C=+3.999283199 release-structural C=+4.000000000 total err=+0.01195%
  R80 named worst=0.219645% synthetic worst=0.228141% Mercury resolution worst=0.039133%
  limitation: this confirms that the measured release-work multiplicity is numerically the right bridge to D; it still does not derive why the mechanically established dispersion unit D equals the one-mode reference in the release energy ledger.

TEST 08 - H2-086 DECISION
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  inherited release/opening work owns a coefficient-free fourfold ledger: True
  finite-FQ source/destination handoff conserves and mirrors that ledger: True
  release-work multiplier remains a close orbital D bridge: True
  pure geometric gradient crossover produces inward/outward asymmetry: False
  literal planet diameter resolved by current grid (>=2 cells): False
  verdict: SIX-SUPPORT RELEASE/CAPTURE HYPOTHESIS IS STRENGTHENED AS THE BEST LOCAL BLACK-BOX OWNER OF THE STRUCTURAL ~4D MULTIPLICITY
  sub-verdict: HARDER-IN/EASIER-OUT DOES NOT FOLLOW FROM FRACTION-CROSSED OR GEOMETRIC ENGAGEMENT ALONE; A CARRIED STATE/OTHER READOUT WOULD BE REQUIRED FOR THAT NARRATIVE
  sub-verdict: WHOLE-PLANET GRADIENT-COMMITMENT REMAINS UNTESTED AT MACROSCOPIC RESOLUTION IN THE CURRENT POINTLIKE ORBIT ENGINE
  SEALED H2-086 final fingerprint: 06a18593cc88ca28298e44ffe07f5dc0a381a8654393654f55e17c55b0e5d701

Interpretation guardrails:
  - A passing release-work result is stronger than a bare geometric identity because it uses inherited H-019/H-021 work/closure mechanics.
  - Source/destination partition is conservative; do not describe 4D as free energy created at the node.
  - Pure finite-body fraction crossing is reversible; do not claim inward/outward hysteresis unless a real carried state produces it.
  - Planet-size diagnostics are external geometry/resolution checks only; no physical radius is fitted into the orbital closure.
  - If H2-086 passes locally, the remaining un-derived link is specifically D <-> one generalized release/opening work unit.

H2-086 complete. Return h2-086results.txt first; CSVs are optional unless a row needs verification.
