Panoramica

Coherence Map — Thermodynamics

TriadicFrameworks /docs/theories/thermodynamics/coherence_map.md#

This map defines how coherence behaves across temperature, entropy, free energy, flows, equilibrium, and RTT regimes.


1. Coherence Dimensions#

Thermodynamic coherence is evaluated across five substrate‑level dimensions:

1.1 Constraint Coherence#

  • validity of state variables
  • consistency of constraints (T, S, F, U, V, P)
  • non‑negativity of entropy
  • ensemble‑consistent definitions

1.2 Potential Coherence#

  • convexity of free‑energy surfaces
  • stability of minima
  • well‑defined gradients
  • ensemble‑appropriate potentials (F, G, Ω)

1.3 Gradient Coherence#

  • flows follow gradients
  • directionality preserved
  • no oscillatory or mechanical drift
  • monotonic relaxation

1.4 Entropy Coherence#

  • monotonicity (dS/dt ≥ 0)
  • valid regime boundaries
  • correct open‑system behavior
  • irreversibility structure

1.5 Equilibrium Coherence#

  • fixed‑point structure
  • ∇F = 0
  • dS/dt = 0
  • stability via second‑derivative tests

2. Coherence Levels (C0–C4)#

C0 — Incoherent#

  • constraints violated
  • entropy negative or undefined
  • free‑energy surfaces non‑convex
  • flows not gradient‑aligned

C1 — Weak Coherence#

  • constraints partially valid
  • entropy monotonicity fragile
  • gradients noisy or inconsistent
  • equilibrium unstable

C2 — Moderate Coherence#

  • constraints valid
  • free‑energy surfaces mostly convex
  • flows gradient‑aligned
  • equilibrium stable but sensitive

C3 — Strong Coherence#

  • full constraint integrity
  • convex potentials
  • monotonic flows
  • stable equilibrium fixed‑points

C4 — Perfect Coherence#

  • idealized constraint geometry
  • perfectly convex potentials
  • exact monotonicity
  • globally stable equilibrium

C4 is theoretical; real systems approach C3.


3. Coherence Field#

The coherence field is a gradient over:

  • constraint validity
  • potential convexity
  • gradient alignment
  • entropy monotonicity
  • equilibrium stability

High gradients indicate coherence instability, typically near:

  • phase transitions
  • constraint changes
  • ensemble switches
  • environment coupling

4. Collapse Modes#

Thermodynamic coherence fails through four canonical collapse modes:

M1 — Constraint Collapse#

  • invalid state variables
  • negative entropy
  • inconsistent ensembles

M2 — Potential Collapse#

  • non‑convex free‑energy surfaces
  • unstable minima
  • undefined gradients

M3 — Gradient Collapse#

  • flows not aligned with −∇F or −∇T
  • oscillatory or mechanical drift
  • loss of directionality

M4 — Entropy Collapse#

  • dS/dt < 0
  • irreversibility violated
  • open‑system inconsistency

5. RTT Regime Coherence#

R1 — Constraint Substrate Regime#

Coherence strongest.

  • constraints fundamental
  • entropy monotonic
  • free‑energy convex
  • flows gradient‑aligned

R2 — Statistical Mechanics Regime#

Coherence refined.

  • microstates explicit
  • partition functions define potentials
  • fluctuations appear

R3 — Field‑Theoretic Regime#

Coherence embedded.

  • free energy field‑dependent
  • phase transitions field‑level
  • vacuum structure influences stability

R4 — Cosmological Regime#

Coherence geometric.

  • temperature geometric
  • entropy horizon‑scale
  • equilibrium cosmological

6. Diagnostics#

A thermodynamic system is coherent when:

  • S ≥ 0
  • dS/dt ≥ 0
  • free‑energy surfaces convex
  • flows follow gradients
  • equilibrium is a fixed‑point

A system is incoherent when:

  • constraints violated
  • entropy decreases
  • potentials non‑convex
  • flows misaligned
  • equilibrium unstable

Summary#

Thermodynamic coherence is:

  • constraint‑first
  • potential‑structured
  • gradient‑aligned
  • entropy‑monotonic
  • equilibrium‑fixed‑point
  • RTT‑dependent

Coherence is strongest in R1, refined in R2, embedded in R3, and geometric in R4.