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Thermal classes either fill the domain or split an adiabat

Statement

Let Γ⊂Rn+1 be a simple domain satisfying the forward-sector hypotheses and T1–T4. Let S be the additive extensive entropy supplied by Additive extensive representation of compound comparison after CH for its finite scaled products is proved by Reference-strip gluing proves comparison for scaled copies. Then either all pairs of states in Γ are thermally equivalent, or there are x,y on one entropy level (equivalently, one adiabat ∂Ax by Nesting and comparison of simple-system states) with x̸∼Ty.

Facts & Assumptions

Given: The same-type accessibility relation, the thermal relation, the hypotheses in the Statement, and the current entropy representation.

[A1]

Forward-sector hypotheses for a simple state domain: A1–A7 and S1–S3 hold; the sector theorem supplies a constant fixed-work energy orientation for each type.

[A2]

Thermal joins and conditional contact hypotheses: T1–T4 hold and thermal equivalence is transitive.

[F1]

Reference-strip gluing proves comparison for scaled copies: every equal-mass finite compound comparison of this simple type is complete.

[F2]

Additive extensive representation of compound comparison: under that comparison property, an additive extensive entropy represents every same-type finite-compound comparison.

[F3]

Forward orientation and the Lipschitz boundary graph: each simple domain has a constant orientation sign for fixed-work energy comparisons; in coordinates oriented in that sign, sector boundaries are the stated graphs.

[F4]

Finite convex functions are locally Lipschitz: a finite concave entropy is continuous on the open domain.

[F6]

Nesting and comparison of simple-system states: a boundary point y∈∂Ax has Ay=Ax; strict accessibility is interior membership. Together with [F2], this identifies entropy levels with sector boundaries.

[F7]

Thermal joins force a common mathematical energy orientation: T1 and the reversible-split existence in T2 force a common orientation sign; the common affine proof-coordinate change preserves all energy-sum joins and does not redefine physical energy.

Proof

1.1A1F1F2F3F7

Use [F7]'s common mathematical energy orientation for the proof coordinates. Apply [F2] using [F1] after dividing represented coefficient maps by the fixed positive type weight wΓ, as specified in [A1]. Multiply the resulting unit-state entropy by wΓ to evaluate represented states; this positive factor preserves all same-type order comparisons. Write S(x) for that represented-state value. The convex-combination access hypothesis in [A1] and additivity imply concavity: for 0<t<1, accessibility of (tx,(1−t)y) to tx+(1−t)y gives tS(x)+(1−t)S(y)≤S(tx+(1−t)y). By [F3], S is strictly increasing in energy at fixed work coordinate.

1.2A1F3F4algebra

Fix a work coordinate v and let Jv:={u:(u,v)∈Γ}, an open interval. The restriction sv(u)=S(u,v) is finite, concave, continuous by [F4], and strictly increasing by [F3]. For an interior u, concavity makes the right secant slopes nonincreasing as the secant endpoint moves right, and the left secant slopes monotone as the endpoint approaches u; hence the one-sided derivative limits sv,+′(u) and sv,−′(u) exist. Choose a<u<b in Jv: the secants to a,b bound those limits, so they are finite, and concavity gives s−′≥s+′. Monotonicity gives nonnegative slopes. If s+′(u)=0, then for every z>u concavity bounds (sv(z)−sv(u))/(z−u)≤s+′(u)=0, contradicting strict increase. Thus s−′≥s+′>0. Define Θ(u,v)=[1/sv,−′(u),1/sv,+′(u)], a nonempty compact interval of positive finite reciprocal slopes.

1.3A1A2F1F2F3F4F6

Suppose the second alternative fails, so each adiabat contains one thermal-equivalence class. By [F1]–[F2], Ax={y:S(y)≥S(x)}. Continuity of S and strict increase in energy at fixed work coordinate imply that every point with S=σ has arbitrarily nearby points with larger and smaller entropy; hence each entropy level Eσ={x:S(x)=σ} is a forward-sector boundary. The supposition makes each Eσ lie in one thermal class. Let R=S(Γ) and, for each thermal class Cα, put Rα={S(x):x∈Cα}. These sets partition R: two distinct classes cannot share a level under the supposition. The range R is an interval, since any two points of the convex domain are joined by a segment and the continuous entropy takes every intermediate value along it.

2.1A1A2F1F2step 1.2

Fix x=(u1,v1) and y=(u2,v2) of this same simple type, and let U=u1+u2. The admissible energy splits form the open interval D={w:(U−w,v1)∈Γ, (w,v2)∈Γ}, which contains u2. Define g(w)=sv1(U−w)+sv2(w). For the join state J(x,y), T2 gives an admissible split q whose pair is reversible with the join. For every other split p, T1 gives p≺J(x,y)≺q, so p≺q. The pair states p,q are finite compounds of two copies of this same simple type; [F1]–[F2] and their entropy representation therefore give g(p)≤g(q). Thus q maximizes g. If the initial split x,y is reversible with the join, it is equivalent to q; entropy representation gives equal entropy, so it too maximizes g. Conversely, if u2 maximizes g, then g(u2)=g(q), and [F1]–[F2] make the initial pair reversible with q; composing with q∼J(x,y) shows x∼Ty. For a concave function at an interior point, maximality is equivalent to g+′(u2)≤0≤g−′(u2): right secants are bounded above by the right derivative and left secants below by the left derivative. Here g+′(u2)=−sv1,−′(u1)+sv2,+′(u2),g−′(u2)=−sv1,+′(u1)+sv2,−′(u2). The two inequalities are exactly sv1,+′(u1)≤sv2,−′(u2) and sv2,+′(u2)≤sv1,−′(u1), which say the positive slope intervals intersect; reciprocal reverses their endpoints, so this is equivalent to Θ(x)∩Θ(y)≠∅.

3.1A2F5step 2.1

Let Tα be one thermal class. The compact intervals Θ(x), x∈Tα, pairwise intersect by step 2.1. For any finite subfamily, pairwise intersection implies common intersection: the largest left endpoint is no greater than the smallest right endpoint, since the intervals attaining those two endpoints intersect. Fix x0∈Tα; the sets Θ(x)∩Θ(x0) are closed subsets of the compact interval Θ(x0) and have the finite-intersection property. Compactness [F5] gives a common point, so Iα:=⋂x∈TαΘ(x) is a nonempty compact interval. If distinct classes had intersecting common intervals, representatives x,y would have intersecting Θ intervals and would be thermally equivalent by step 2.1, a contradiction. Thus the intervals Iα for distinct classes are disjoint and strictly ordered on the real line; use this as the order of the classes.

4.1A1F3F4F5step 1.2step 1.3step 3.1

For each work coordinate v, strict continuity of sv maps the open interval Jv onto an open interval Rv⊂R. On Rv, the level-to-class map is nondecreasing: as u increases, concavity makes both one-sided slopes nonincreasing, so both endpoints of Θ(u,v) are nondecreasing. If two such intervals Θ are disjoint, monotonicity of both endpoints forces the earlier interval to lie strictly below the later one; by step 3.1, this is the class order. The local class maps agree on overlaps of Rv because each entropy level lies in one class. The open intervals Rv cover R. Any compact subinterval of R has a finite subcover by these intervals by [F5]; its intersection graph is connected, since otherwise the connected subinterval would be split into two disjoint nonempty relatively open sets. Chaining the local orders through overlaps proves that the class map is nondecreasing on all of R.

5.1A2F2step 4.1∎

Fix σ∈Rα and x∈Eσ. T4 gives x0≺≺x≺≺x1 with x0∼Tx1. Entropy representation gives S(x0)<σ<S(x1), and their levels belong to the same class Rα. The global nondecreasing order from step 4.1 forces every level between them, including an open neighborhood of σ, into Rα. Thus each class set is open in the interval R. Since these disjoint open sets partition connected R, only one nonempty class exists. Under the supposition, all states are thermally equivalent, proving the dichotomy.

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