1. Introduction
An equation of motion able to model nonequilibrium relaxations at any scale must balance two competing demands, namely: (i) be sufficiently microscopic to respect the laws of conservation as well as the second law of thermodynamics, yet (ii) have a sufficiently reduced description in terms of a small number of physically interpretable variables. Without the latter, it becomes unusable for systems with large state spaces, while the former suggests that it should be thermodynamically self-consistent, i.e., able to evolve from any initial nonequilibrium non-zero-entropy state to stable equilibrium.
Within the unified quantum theory of mechanics and thermodynamics proposed by Hatsopoulos and Gyftopoulos [
1,
2,
3,
4], the two steepest-entropy-ascent (SEA) equations of motion proposed for nonequilibrium quantum thermodynamics (QT) in [
5,
6,
7] and developed in several papers thereafter (see, e.g., [
8,
9,
10,
11]) satisfy the first of these demands. These SEAQT evolution equations, one for an unstructured quantum system and the other for a structured composite of quantum subsystems, augment the unitary quantum evolution of the von Neumann equation of motion [
12,
13] with a dissipative term constructed so that entropy production is non-negative, while the relevant dynamical invariants (e.g., normalization and energy and, when present, other commuting generators of the motion) are preserved by the dissipative part of the motion. In its compact quantum form, each equation evolves the density operator
through a nonlinear law governed by a generalized Massieu-type operator, which encodes both the entropy and relevant conservation constraints [
8,
9,
14]. The resulting dynamics is thermodynamically structured and thermodynamically self-consistent, but, nonetheless, a dynamics on the full space of density operators [
15,
16,
17,
18,
19,
20].
Note that the standard equation of motion widely used by the quantum thermodynamics community is the Kossakowski–Lindblad equation [
21] or more precisely the Gorini–Kossakowski–Sudarshan–Lindblad (GKSL) equation [
22,
23,
24]. The basis of this equation is the generator of a completely positive dynamical semigroup, which results in a large class of quantum master equations for which Kossakowski provides the necessary and sufficient generator conditions [
25] and Ingarden and Kossakowski the consistency condition for the macroscopic observables of open quantum systems [
26]. An equivalent approach is the Kraus-operator or operator-sum formalism [
27,
28,
29] of trace-preserving linear completely positive definite maps introduced by Kraus [
30,
31]. Unlike the SEA equations of motion, which are
inherently quantum mechanically and thermodynamically self-consistent, the GKSL equation is only
inherently the former since as pointed out by Spohn [
32,
33], whether or not this equation evolves thermodynamically depends on the choice of Kraus operators for which the corresponding semigroup has a unique final stable equilibrium (Gibbs) state to which every initial state evolves. Thus, the dissipative path predicted by the GKSL equation is a thermodynamic path only if it obeys the “unital” condition [
34] and that depends on the Kraus operators employed. In contrast, the dissipation operator of the SEAQT equations, which is constructed based on the SEA principle and a set of operators called the generators of the motion, always evolves towards stable equilibrium independent of the choice of these operators. This is what is meant by being
inherently thermodynamically self-consistent. An example of this is seen in the application of both formalisms to the evolution of slightly perturbed Bell diagonal states given in Chapter 12 of [
35].
Now, regarding the second demand, using the equations of motion for systems with large state spaces becomes impractical due to the high dimensionality of the microscopic description unless a low-dimensional manifold can be identified that is both (i) physically meaningful and (ii) dynamically consistent with the SEA evolution. The hypoequilibrium (HE) concept provides such a principled reduction [
36,
37,
38,
39,
40,
41]. Using this concept, the Hilbert space is decomposed into an orthogonal direct sum of a finite number of coarse spectral sectors
. Each sector is the subspace spanned by a subset of the eigenspaces of the Hamiltonian operator, for which the total probability and mean energy (together with other moments if needed) are tracked. In this representation, each nonequilibrium state is described as a mixture of the density operators associated with the coarse spectral sectors, weighted by the respective total probabilities. When the Hilbert-space decomposition is generated by partitioning the set of energy eigenvalues into contiguous energy intervals, the coarse spectral sectors reduce to what are commonly called “energy shells.” The HE approximation then postulates that the density operator for each spectral sector is canonical (or grand canonical), and, thus, has its own inverse temperature (or temperature and chemical potential) different from the other spectral sectors. Each state of the system is, therefore, represented by a set of “spectral-sector temperatures” (or “spectral-sector temperatures and chemical potentials”) and the corresponding set of “spectral-sector total probabilities.” This is not merely a numerical convenience. It is instead a way of encoding far-from-equilibrium structure while retaining an equilibrium-like form locally on each coarse spectral sector. The HE concept for quantum systems parallels the lower-dimensional-manifold-approximation philosophy of several model reduction approaches, notably, the “rate-controlled constrained-equilibrium” (RCCE) method in chemical kinetics [
42,
43,
44], the “quasi-equilibrium” approximation in dynamical systems [
45,
46] and in complex biological models [
47] (characterized by a variety of empirical [
48,
49] and geometrical [
50,
51,
52,
53,
54,
55,
56] methods to identify the most effective slow invariant manifold for each given class of problems), or systematic coarse-graining techniques [
57,
58,
59,
60].
Of course, to be physically relevant, the HE manifold of constrained-equilibrium (or quasi-equilibrium) states must be invariant with respect to the SEA dynamics. In other words, when evolved according to the SEA dynamics, any initial HES must remain within the HE manifold at all times. This dynamical consistency is important since otherwise the evolution risks being an uncontrolled approximation. If indeed it is consistent (under clearly stated assumptions) as suggested by the proof provided in [
36], then the HE–SEAQT model becomes a legitimate reduced model with the SEA principle providing the irreversible dynamics and the HE concept providing the reduced-order description.
The HE concept has also been applied to the SEAQT equation for a general structured composite of quantum subsystems [
61] and to ad hoc extensions of the SEAQT equation tailored to model heat, diffusion, and heat-and-diffusion interactions between systems as well as provide non-Hamiltonian (NH) extensions of the Onsager reciprocity relations to the non-near-equilibrium nonlinear domain as well as models of system–bath interactions [
37,
38,
39]. Applications with experimental validations include (see, e.g., Chapters 10 to 23 of [
35]) predicting electrical, thermal, magnetic, and mechanical transport properties; the chemical and electrochemical kinetics of reacting mixtures; ferromagnetic eddy current losses; nonequilibrium size and concentration effects on heat and mass diffusion; the kinetics of surface adsorptions and contamination; discontinuous and continuous phase decompositions; ordering and phase separation; atomistic spin relaxations; thermal expansions; microstructural evolutions; cell membrane lipid diffusion; defect formation and migration; the nonequilibrium behavior of nonquasiequilibrium thermodynamic cycles, etc.
To clarify what is new here, a brief description of the HE concept’s original introduction [
36,
37,
40] by Li and von Spakovsky is needed. In particular, those authors used a very simple mathematical proof to show that the HE concept is consistent with the dynamics of the SEAQT equation of motion for simple (i.e., unstructured) quantum systems both in its canonical and grand canonical realization, demonstrating its usefulness for modeling heat, mass, and work interactions as well as chemical reactions. Using this concept, Li and von Spakovsky also demonstrated that the Onsager relations, the quadratic dissipation potential, Gibbs relation, and a fundamental definition of thermodynamic intensive properties based on binary extensive property fluctuations can be extended to the far-from-equilibrium region. The latter are, in fact, shown to reduce to the well-known intensive properties of classical thermodynamics (i.e., the temperature, chemical potential, pressure, etc.) at stable equilibrium. In contrast, the present paper provides a much more extensive mathematical proof as well as the underlying geometrical basis in state space for the HE concept and does so for both the SEAQT equation of motion for simple (i.e., unstructured) quantum systems as well as that for general (i.e., structured) quantum systems. The focus is, thus, on providing a precise and detailed mathematical formulation of the HE–SEAQT model for the simplest unstructured quantum systems and of the NH–HE–SEAQT model of non-Hamiltonian heat interactions between unstructured systems. For these models, the HE subspace is proven to be an invariant-manifold within the SEA dynamics. The HE formalism is then rigorously extended to structured composite systems (i.e., general quantum systems). Excluded from the present treatment is a discussion of variations of the NH–HE–SEAQT model such as those used in [
61,
62,
63,
64,
65,
66] to heuristically model the time evolution of coherences and correlations as well as energy, entropy, and particle exchanges between subsystems in the presence of interaction Hamiltonians. These variations involve hybrid equations of motion including the simultaneous effects of the von Neumann, Lindblad, and SEAQT terms as well as a continuous projection of the state operator onto an HE manifold.
In the present work, hypoequilibrium states (HES) are first formulated in compact operator language consistent with the SEAQT equation of motion for a simple quantum system, using a general decomposition of the Hilbert space and the corresponding HES variables. Next, based on the simplifying but important practical regime in which the dissipative SEA term acts on states commuting with the Hamiltonian (so that the dynamics reduces to a closed evolution of eigenlevel populations), the reduced evolution for the HE parameters is derived and the associated entropy production structure identified. Addressing the invariant-manifold property next, an initial
M-th-order HES representing a “mixture of canonicals” is used to show how the SEA evolution preserves the order of the initial state, demonstrating that the evolving states remain within the same
M-th-order HE family. The HE representation is also shown to lie within the logic of the RCCE [
42,
48,
49] model reduction concept, since the HES can be viewed as a maximum-entropy state relative to a chosen set of coarse constraints so that the evolving intensive parameters acquire the meaning of constraint potentials. Without shifting the focus away from the HES–SEA dynamical consistency, the RCCE connection unifies terminology and situates the HE concept within a broader literature on reduced-order modeling.
The paper is organized as follows.
Section 2 defines the tenets of the HE concept and describes the Hilbert space decomposition induced by a specific partitioning of the set of energy eigenvalues.
Section 3 formally defines the HE ansatz, derives the reduced evolution in terms of HES variables, and isolates the minimal relations needed for later proofs. The HE formalism is then extended to structured composite systems in
Section 4.
Section 5 follows with a discussion of the consistency of the HE concept with the RCCE approach.
Section 6 outlines the implementation of the HE approximation into the original SEAQT dynamical structure in terms of the notation reviewed for completeness and consistency in
Appendix A and
Appendix B and prove that the HE subspace is an invariant-manifold within the SEA dynamics.
Section 7 then introduces a modification of the original SEAQT equation of motion for composite systems that models, in a thermodynamically consistent manner, energy and entropy (and mass) exchanges between subsystems as non-Hamiltonian (NH-SEAQT) dissipative effects. This is followed by
Section 8, which shows the compatibility of the NH-SEAQT model with the notion of a heat interaction between two systems, while
Section 9 formulates the model for a system in contact with two other systems that could model heat baths.
Section 10 then presents final conclusions.
2. Preliminary HE Assumptions: Partitioning the Energy Spectrum
The technical assumptions underlying the HE concept are stated first. Only density operators on the system Hilbert space that belong to the special class defined by the following conditions are considered:
- (HE1):
commutes with H (at all times t), i.e., ;
- (HE2):
is full rank, i.e., has no zero eigenvalues, so that , where is the projection operator onto the range of ;
- (HE3):
assigns equal probability to each of the corresponding eigenstates of each degenerate eigenvalue of H.
To be more explicit, the
N-energy-eigenlevel system Hamiltonian in spectral form is written as
where
denotes the
i-th distinct system energy eigenvalue with degeneracy
(
); and
is the projector onto the corresponding eigenspace
so that
is the spectral decomposition of
induced by
H and
is the corresponding resolution of the identity operator. With these assumptions, the density operator has the spectral form
and
is the occupation probability of the
i-th energy eigenlevel and the entropy operator
defined according to [
5,
6,
8] is given by
where
is the Boltzmann constant and
In general, for any trace-preserving dynamics, i.e., with
,
(see footnote 7 of [
8] for a proof).
The next assumption is:
- (HE4):
The set of N eigenvalues of is arbitrarily partitioned into M disjoint subsets.
Each subset defines a subspace of the Hilbert space obtained as the span of the corresponding energy eigenspaces. This induces an orthogonal direct–sum decomposition of the Hilbert space
so that the resolution of the identity
I and the spectral forms of
H and
can be written as follows:
where clearly
,
and
Following [
36,
37] and in anticipation of the additional assumptions introduced in
Section 3, the subspace
is called the
K-th hypoequilibrium spectral sector (HESS); and the total probability
and the mean energy
of the
K-th HESS are defined as
Here,
, and the probability associated with the
-th energy eigenlevel of the
K-th subset is not
but
.
The
K-th
HESS density operator on
is defined by
where, by construction,
To compute how each HESS contributes to the overall entropy, the logarithms of these density operators are needed. Defining
the
proper HESS entropy operator
and the
local HESS entropy
are given by
where Equation (
13) and the fact that the projector
is an idempotent operator (see [
8]) are used to derive this last equation. Furthermore, the term
local denotes a single HESS, i.e., a coarse spectral sector
;
is the
partitional HESS entropy; and
Now, following the definition of the HESS and using Equation (
7),
where the HESS
partial entropy operator, its expectation value, and its expected covariance with the
local Hamiltonian,
, are given by
The HESS
proper energies and entropies are then expressed as
A summary of the various energy and entropy definitions provided thus far is given in
Table 1.
Although at first glance Assumption HE1 (
) may appear to be overly restrictive, it is a deliberate modeling choice with wide applicability for which HE is a statement about coarse-grained equilibration of eigenenergy populations. In particular, the defining signature of an HE sector is, as seen below (Equation (
47)), that the sector entropic coordinates
are affine maps on
. Once the HES manifold is established and shown to be dynamically consistent in this minimal setting, one can ask how coherences and additional generators deform or enlarge that manifold. Furthermore, under the simplifying assumptions made in this section, a full description of the time evolution of the state operator
still requires the time dependence of all the
’s or equivalently the
’s, whose number is
N, and for practical systems may still be very large. Additional methods for dealing with this—such as the density of states method developed in [
36] and the approach used for phonons in [
41]—can be employed.
In the next two sections, a set of assumptions is introduced to reduce the number of independent variables from
N to
, where
M is the number of assumed HESS’s. As shown in
Section 5, these assumptions are often physically justifiable and are conceptually aligned with a model-reduction strategy widely used in chemical kinetics.
3. Main HE Assumption: Canonical HESS Density Operators
The HE approximation results when the HESS density operators are constrained to take a canonical or grand canonical form. The grand canonical case is not treated here. The formal assumption is as follows:
- (HE5):
A state
is an “HE state” of order
M with respect to the chosen partition
if, for each HESS
K, there exists an inverse temperature
such that
or, equivalently, using Equations (
6) and (
13)
The kinetic justification of assumption HE5 is discussed in
Section 5. Note that Assumption
HE3 is a corollary of Assumption
HE5. It is also noteworthy that the symmetric compression of the exponential terms via the projector
in Equation (
27) restricts the operator’s support to the subspace
. This ensures that
acts nontrivially only within its respective sector. Without
, the term would reduce to the identity on all other subspaces
, leading to unphysical contributions in the global sum.
Combining Equations (
13) and (
27), it is evident that the HE approximation consists of assuming that the states at any time are of the form
Note that, since by construction the ranges of operators
and
are entirely contained in subspace
and the
’s are orthogonal to each other so that
, the HE density operator
can be compactly rewritten by absorbing the normalization factors and the sector probabilities into the exponential such that
where the coefficients
are defined by the relation
In this representation,
acts as a sector-dependent normalization constant (effectively a free energy shift) that ensures the correct weighting of each subspace. The HE manifold is therefore characterized by the following equivalent relations:
The set
of HE density operators of form Equation (
29) is an “invariant manifold of the dynamics” if the underlying equation of motion evolves any density operator initially in
along a path that remains within
at all future times (“strongly” invariant if this holds also backwards in time as is later proven to be the case under HE–SEAQT dynamics; see Equation (
94)). A sufficient condition for this to hold true is that the equation of motion entails rates of change of the
’s compatible with Equation (
32), i.e., that the following
or, equivalently,
are satisfied.
By exploiting the fact that the
are mutually orthogonal projectors that resolve the identity
within the subspace
, the exponential terms in Equation (
30) can be decomposed into a sum of spectral components such that
Note that if the
’s (and hence the
’s) are time-independent, then the time evolution
of the state is parametrized by only
variables, namely, either
and
(Equation (
29)) or, equivalently,
and
(Equation (
30)). This is an important simplification that, as already referenced in
Section 1, when combined with the SEAQT dynamical equations has enabled the successful modeling of a broad range of mesoscopic systems. As shown below in
Section 5, the HE approximation is equivalent to the translation into the nonequilibrium quantum thermodynamic framework of the constrained equilibrium approximation in the chemical kinetics framework and the quasi-equilibrium approximation in the dynamical systems framework.
The HE family in Equation (
31) is now parametrized by
subject to
or, equivalently, by
subject to the constraint
induced by normalization. Hence, the HE manifold has dimension
.
Taking the logarithms of the HESS density operators (Equation (
27)) and using Equation (
37) yields for
a remarkably simple block-diagonal form where each sector
contributes an effective Hamiltonian term
shifted by the sector-specific normalization
. As a result the following relations hold for each sector:
and for the overall system,
so that, for arbitrary parameters
and
, the following “nonequilibrium Massieu operator” can be defined:
Furthermore, following [
36,
37], it is important to observe that Equation (
28) implies
and, therefore, rewriting it for the index
j and subtracting and dividing by
yields the relations
expressing a fingerprint feature of stable equilibrium, which here (by Assumption HE5) holds only locally within each HESS but not globally. For a global HES
to approach a stable equilibrium state
, all the inverse temperatures
must converge to a common value
, all
’s converge to the common value
, and the
’s converge to
.
If an HE sector contains only a single distinct energy eigenlevel so that
, then Equation (
28) is satisfied identically for any
. Such sectors carry population information but no meaningful internal temperature. In applications, partitions with
for all sectors are typically chosen and, thus, carry a nontrivial internal equilibration structure.
When no decomposition is assumed, i.e., the whole Hilbert space is viewed as a single sector so that
, then assumption HE5 corresponds to a locally stable equilibrium state. In this trivial case,
K only takes the value 1,
,
,
,
, and
5. Consistency of the HE Approximation with the RCCE Approach
In this section, the HE approximation is shown to fit precisely within the framework of the RCCE method for model reduction. This method was introduced and applied by Keck and coworkers [
42,
43,
48,
49,
67] as a thermodynamically consistent method for obtaining accurate results in combustion modeling applications that involve complex chemical kinetic schemes. Many others have worked on variations, improvements, generalizations, and geometrizations of this model reduction technique [
44,
45,
46,
51,
57,
58,
59].
In the present HE framework, it is assumed that the dynamics has bottlenecks associated with the flow of probability and energy between different HESS’s so that the irreversible redistribution of probabilities
and partial energies
among different HESS’s is much slower than the probability redistribution within each HESS. As a result of the rapid equilibration within each HESS, each density operator
rapidly relaxes towards the maximum
proper entropy
compatible with the local normalization condition
and the current value of the
proper mean energy
, namely, towards the
given by Equation (
27).
Figure 1 provides a pictorial representation of the HE approximation with the help of the energy-vs-entropy diagrams developed in [
68,
69].
In terms of RCCE terminology, it is assumed that the relatively slow, rate-controlling constraints associated with the bottlenecks of the overall dynamics are the spectral-sector total probabilities
and partial mean energies
. Therefore, at any given time during the evolution, the state
is assumed to be well approximated by the state that maximizes the overall entropy
subject to these constraints. The constrained maximization can be written as
Introducing the Lagrange multipliers
and
(in the RCCE approach
and
are called “constraint potentials”) and using Equations (
9), (11), and (
23), the equivalent unconstrained maximization becomes
The solution is readily found to be
Substituting this into the constraints yields the Lagrange multipliers in terms of
and
. From the first constraint,
Equation (
31), i.e.,
where
follows so that Equation (
67) can be rewritten as
and, therefore,
which coincides with Equation (
29). Substituting into the second constraint yields the relation
which can be solved to obtain
and together with Equation (
68) yields
.
Recalling that
(Equation (
25)), these relations can be rewritten in terms of the
proper mean HESS energy instead of the
local mean HESS energy since
and
. Within the RCCE method, adopting the constraint potentials (here
and
) as the independent variables [
43] avoids having to solve the above system of equations to obtain the values of
and
from the current values of
and
at every time step during the integration of the evolution equation.
Finally, the RCCE description of nonequilibrium states (and hence also the HE description) follows the same logic as the standard model for chemically reacting systems where nonequilibrium states are assigned the properties of the stable equilibrium state of a “surrogate” system (see [
68,
70]) with the same composition, volume, and energy, but with all reactions frozen. This amounts to treating the chemical reactions as the bottlenecks of the dynamics, the corresponding set of constraints being the set of all species amounts.The success of the RCCE method, thus, hinges on the ability to identify the bottleneck constraints. Equivalently, in the present SEAQT context, the key to successful model reduction is the ability to identify the
M subsets of energy eigenvalues subject to rapid irreversible redistribution within each HESS so that the focus can be on the slow (bottleneck) dynamics that controls the energy and entropy exchanges between the different HESS’s.
6. HE–SEAQT for an Unstructured and Isolated System
Appendix A provides a review of the foundational assumptions of the original SEAQT formalism for a general system with internal structure, while
Appendix B merges these assumptions with the HE assumptions discussed in
Section 4 and completes them with two additional assumptions to obtain the HE–SEAQT formulation for a system with noninteracting subsystems. Under this set of HE–SEAQT assumptions, there is no interaction Hamiltonian and each subsystem evolves independently of the others. It, therefore, suffices to consider a single, unstructured system that can be modeled without internal subdivision into separated, noninteracting, and uncorrelated subsystems. The HE–SEAQT equation of motion takes the same form as Equations (
A35)–(A40) but without the
super- and subscripts, i.e.,
and the SEA nonequilibrium potentials
and
are functions of all the constraint potentials
and
which may be written as
where
Here,
,
, and
denote overall weighted averages and covariances with respect to the dimensionless weights
and the weighted deviations (from the overall weighted average)
defined as follows:
Denoting by
the eigenvalues of the local nonequilibrium Massieu operator of sector
K,
, and recalling Equations (
32) and (
33), the following relations corresponding to normalization, mean-energy conservation, and entropy production rate are readily verified:
Note that the overall nonequilibrium Massieu operator
has zero-weighted mean value but a nonzero-weighted variance proportional to the overall entropy production rate, which vanishes only at stable equilibrium.
Recalling that
,
,
,
, and
, Equation (
72) yields the following relations:
where
and the systems of Equations (
91) and (
92) for normalization and the conservation of mean energy are entirely equivalent to the system of Equations (
74) and (75).
It is evident from Equation (
89) that if a
is zero at one time then it must be zero at all times. In other words, an unpopulated HE sector remains unpopulated under SEA dynamics, a feature that extends to the HE framework the known feature of SEA dynamics [
6] whereby zero eigenvalues of the density operator remain zero and nonzero ones remain nonzero (although they can approach zero much like
as
). This feature holds also for Equation (
87) and implies that if the
’s start all positive, as is required for the density operator to be strictly positive, they can never cross zero, whether the equation of motion is evolved forward or backward in time. Since the right-hand side of Equation (
93) is non-negative, it follows that under HE–SEAQT the rate of change of the overall system’s entropy is non-negative in forward time and non-positive in backward time.
Subtracting from Equation (
88) the same equation written for another energy eigenlevel
in the same sector
K, and recalling Equation (
32), yields
which reduces to
Similarly, dividing Equation (
88) by
, subtracting the resulting equation written for another energy eigenlevel
in the same sector
K, and again using Equation (
32) yields
which reduces to
Note that the overall energy spectrum can be shifted by a constant for Hamiltonians with zero eigenenergies so that the new
’s are nonzero. Together with Equations (
74)–(79)—which give
and
in terms of the
’s and
’s—Equations (
95) and (
97) form a differential-algebraic system of nonlinearly coupled equations that automatically satisfies the normalization and energy conservation constraints. For a given set of initial values
, which identify an initial HES, this system can be readily solved numerically to yield the time evolution of the
HE constraint potentials
and
, along with that of the overall system’s SEA nonequilibrium potentials
,
. It is clear from Equations (
95) and (
97) that the time evolution does not end until (i)
and all the
’s converge to the same value,
, and (ii)
and all the
’s converge to the same value,
. This observation corroborates the interpretation of
as playing the role of a dynamic nonequilibrium inverse temperature.
As the state evolves toward the canonical Gibbs state with inverse temperature identified by the initial mean energy , the values of the SEA potentials and keep changing as the local energies are redistributed among the HE sectors.
Substituting Equations (
95) and (
97) into (
88) yields
which coincides with Equation (
35) and, therefore, proves that the HE manifold is invariant under the SEAQT equation of motion. It is in fact a strongly invariant manifold, because, as noted above, every density operator in
belongs to a trajectory lying entirely within
and well defined in the interval
, evolving in forward time from a minimum value to a maximum value of the entropy. As emphasized and exemplified in [
58], this feature of SEAQT, which extends to HE–SEAQT, can be interpreted as implementing a strong version of the principle of causality, whereby knowing the state at time
identifies a unique trajectory in state space covering the future as well as the past. Mathematically, the time evolution is governed by a temporally reversible one-parameter group (not a semigroup as in the GKSL equation), which nevertheless describes a thermodynamically irreversible evolution, establishing as dynamical theorems both the principle of entropy non-decrease in forward time and the Hatsopoulos–Keenan statement of the second law, i.e., the conditional stability of the maximum entropy (Gibbs) states (‘conditional’ in the technical sense detailed in [
71]).
Now, recalling Equations (41) and (42) and using Equations (
95) and (
97), the rates of change of the sector energies and entropies during the irreversible redistribution of populations may be computed from the relations
Furthermore, it is worth emphasizing another important feature of the HE (and RCCE) approximation, namely, that even though it reduces the description of the dynamics from the full set of differential equations for the
real parameters needed to determine a state operator
to the possibly much smaller set of
constraint potentials
and
, it does not reduce the state description. At any instant of time, via Equation (
32), the values of the
’s and
’s determine the full density operator and, therefore, allow computation of the mean values of all the system’s properties.
The SEA potentials
and
can be interpreted as the effective nonequilibrium properties that mediate the relaxation of the entire system. Their final values emerge from a competitive consensus between sectors, where each sector
K exerts a “leverage” proportional to its statistical weight
, its internal energy fluctuations, and its relaxation speed
. To formalize this, the numerators and denominators of Equations (75) are rewritten as follows:
where the following local weighted averages are defined:
This decomposition reveals that the SEA global inverse temperature
is shaped by two distinct physical contributions. The first term represents a weighted average of the HESS local
values where the importance of each sector is scaled by its energy fluctuations. This implies that sectors with broader energy distributions (i.e., higher heat capacities) contribute more significantly to the instantaneous value of
which, as shown by Equations (
95) and (
97), acts as a common attractor for the local
values. The second term accounts for the entropy–energy covariance between sector weighted averages. It captures how the displacement of a sector’s mean energy and mean entropy from the respective global averages affects the overall target slope of the entropy–energy relation.
Given these relations, a single sector L can dominate the global and impose its local value —thus acting as an internal heat bath—under three specific conditions: (i) Statistical Weight: when , meaning the sector encompasses nearly the entire system; (ii) Fluctuation Dominance: when the internal variance of sector L is much larger than that of all other sectors combined, effectively overwhelming their contributions and cross-couplings; (iii) Geometric Leverage: when sector L is located at an extreme energy mean (), acting as a “leverage point” that pivots the global regression line toward its own local parameters. In these cases, sector L acts as a stabilizer: its high “nonequilibrium thermal inertia” allows it to absorb significant energy fluctuations without shifting its own local potentials, effectively “pinning” the global and to its local values. Consequently, the heat bath dictates the target temperature of the system, forcing smaller, more volatile sectors to align and equilibrate. In the quasihomogeneous near-equilibrium limit, where , the second term vanishes if the sector averages align perfectly along the global equilibrium line, effectively realizing a form of energy equipartition across the HE ensemble.
7. NH-HE–SEAQT: Model of Non-Hamiltonian Heat Interaction Between Unstructured Systems
Building on the sectoral decomposition developed for an isolated system in
Section 6, the model is now extended to describe heat interactions between two or more systems. The suggestions in [
36,
41] for a heuristic extension of the SEA and HE mathematical frameworks are followed to develop an effective and thermodynamically consistent model of heat interactions between systems. This approach is fundamentally different from that discussed in
Section 6 and
Appendix A and
Appendix B, where energy exchanges between subsystems can only occur via the effects of an interaction Hamiltonian
V through the von Neumann (Hamiltonian) term in the equation of motion (Equations (
A1) and (
A2)). Here, instead, energy exchanges between subsystems are modeled via “entropic coupling” provided by a less-constrained SEA dissipative term in the equation of motion.
All the HE assumptions discussed so far and the SEA assumptions reviewed in
Appendix A and
Appendix B are adopted except for the following important modification. As detailed in
Appendix A, the variational principle that leads to the composite-system version of the SEA equation of motion is stated as follows:
- (SEAQT3):
The dissipative part of the evolution equation ensures that, with respect to a local dissipative metric , the direction of the local trajectory , maximizes the local contribution, , to the overall system’s entropy production rate. Under the constraints , which guarantee that the dissipative part of the dynamics does not contribute to the rates of change of the locally perceived global charges (so that these emerge as constants of the motion if they are conserved also by the Hamiltonian part, i.e., if ).
The rates of change of the overall system entropy,
, and of the overall system mean value of
Q linear charges
, are written as
exhibiting additive contributions from the
subsystems. Introducing the Lagrange multipliers
and
for the constraints, the SEAQT
’s are found by solving the
local maximization problems
where the last constraint corresponds to the condition
, necessary for maximizing with respect to direction only (see [
9,
17,
18] for more details). Since the local maximization problems (
105) are independent, they can also be rewritten as a single, equivalent overall maximization problem, namely,
The first two charges are always the identity operator,
, which implements the
constraint and the Hamiltonian operator, for
, which implements the
constraint. The Lagrange multiplier
(usually renamed
) plays the role of “local nonequilibrium inverse temperature” conjugated with the locally perceived energy, and for the stable equilibrium states of the SEA dynamics, it coincides with the thermodynamic inverse temperature.
The present heuristic model of heat interaction proposed in [
37], instead, adopts the following modified assumption, which is called non-Hamiltonian (NH) here because it results in energy and entropy exchanges between subsystems that are driven directly by the SEA dissipative term in the equation of motion.
- (NH-SEAQT3):
The dissipative part of the evolution equation ensures that, with respect to a local dissipative metric
, the direction of the local trajectory
, maximizes the local contribution,
, to the overall system’s entropy production rate, under local conservation constraints
of the locally perceived global charges
, for all
q’s except
corresponding to the Hamiltonian
, for which the conservation constraint is global (not local). [To model heat-and-diffusion interactions, the same exception is also extended in [
40] to the number-of-particle operator(s)
(
).
Therefore, the less-constrained overall maximization problem,
is adopted so that the constraints of the locally perceived mean energy conservation within each subsystem are replaced by a single constraint of global mean energy conservation.
Setting the variational derivatives of
with respect to each
equal to zero, yields, in terms of the “locally perceived nonequilibrium Massieu operators”
,
where the local Lagrange multipliers
(
) and the global
, dubbed “NH-SEA potentials,” are the solution of the system of equations obtained by substituting Equation (
108) into the conservation constraints,
for
and
, such that
The same set of assumptions detailed in
Appendix A and
Appendix B and
Section 4 are adopted with regard to (i) the local metrics
(Assumptions SEAQT5-7); (ii) the absence of interaction terms in the overall system’s Hamiltonian and correlations between subsystems (Assumption CSHE1); (iii) the HE decomposition of the Hilbert space of each subsystem (Assumptions CSHE2-4); (iv) the CSHE assumption (CSHE5) on the state; (v) the minimal set of generators of the motion, i.e.,
,
and
, and the corresponding renaming of the Lagrange multipliers,
and
. As a result,
and the system of equations that determines the Lagrange multipliers becomes
It may be rewritten as
and has the solution
where the
’s and the weighted averages
are defined as in Equations (
76)–(81).
The rates of change of the HE constraint potentials are still given by relaxation equations like (
95) and (
97), and the subsystems’ energies and entropies by relations similar to (
99) and (
100). Thus,
These equations indicate that—while the overall system relaxes (with possible overshooting during the process) towards the stable equilibrium state in which all the
’s have converged to a common value equal to
—the various sectors exchange energy and entropy, both within each subsystem and across subsystems. In
Section 9, this model is detailed for the case of a composite of three systems
,
, and
, where
and
are assumed to be in locally stable equilibrium states, and could be heat baths if their heat capacities are very large.
The same concept outlined in this section has been implemented for systems with variable amounts of constituents. In addition to globally constraining the mean energy, the mean number of particles of each type are globally constrained so that the dissipative term in the NH-SEAQT equation of motion results in effective exchanges of energy and entropy as well as particles between subsystems. As discussed in [
35], this approach extends the modeling of heat-diffusion, mass-diffusion, and heat-and-mass-diffusion interactions to the nonequilibrium domain in which subsystems are in local equilibrium or in HES’s that are not necessarily close to mutual equilibrium.
8. NH-SEAQT Model of Heat Interaction Between Two Systems in Local but Not Mutual Equilibrium
To illustrate the applications allowed by the NH-SEAQT framework just outlined in
Section 7, the simplest case of a composite of only two subsystems
and
each with a single HE sector is considered (hence the subscript 1, used below for notational consistency). Under these conditions, the general relations of
Section 7 reduce to
The overall entropy production is non-negative until
and
equalize. Energy flows from
to
when
. Using standard thermodynamic notation (see, e.g., [
69,
72]), it is denoted as
and is taken to be positive in the direction of the arrow.
An effective temperature
—where the subscript
Q indicates a quantity associated with the heat interaction—can also be identified and an entropy flow related to the energy flow via the heat-interaction expression defined, i.e.,
Here,
gives physical meaning to the SEA nonequilibrium potential
, namely, that it is the weighted average of the inverse temperatures of the two interacting systems, as defined in Equation (
121), where the weights
and
change in time and are related to the heat capacities and relaxation times of the respective systems. With this identification of the entropy flow, the local rates of entropy production within the two systems can be identified and the energy and entropy balance equations written as
Notice that Equation (
128) is cast as a Fourier-law-like linear-looking relation between the energy flow and the finite difference in inverse temperatures of the two systems. It is, however, a highly nonlinear relation since the proportionality coefficient
is a nonlinear function of the inverse temperatures.
In the near-equilibrium limit as
and
approach each other so that
; the model is consistent with the strict definition of a heat interaction at temperature
—as given in [
68] (Section 12.3) and [
69] (Section 40)—as well as with the linear Fourier-like law with coefficient
.
9. NH-HE–SEAQT Model of SEA-Driven Energy and Entropy Exchange Between a System and Two Other Systems in Local but Not Mutual Equilibrium
As a further illustration, consider the case of a composite of three subsystems , , and , where and are each assumed to have a single HE sector (hence the subscript 1) (and could represent heat baths if their heat capacities are very large), while system is assumed to be in HES’s with respect to a HESS decomposition. The additional assumptions are as follows: (i) uncorrelated states (i.e., ); (ii) no interaction Hamiltonians (i.e., , , and ); (iii) time-independent Hamiltonians for and (i.e., and , so that the only way the composite system can interact with other systems—such as a work element—is via the time dependence of control parameters in the Hamiltonian operator ).
The Hilbert space, overall Hamiltonian operator, and overall state operators of the composite system are
The key assumption that distinguishes this SEA model from that discussed in
Appendix A is that the equation of motion is obtained from a less-constrained variational principle than (SEAQT3). Instead of a local maximization problem for each subsystem (see Equation (
A10)), a single global entropy production maximization problem for the overall system is assumed, subject to the following nine constraints: (i) normalization for each subsystem (three constraints); (ii) mean energy conservation for each interacting pair
-
and
-
(two constraints); (iii) a direction constraint for each separate dissipative contribution
,
,
,
(four constraints) where
and therefore
,
,
,
are given by the solution of the following maximization problem (in terms of the nine Lagrange multipliers
,
,
,
,
,
,
,
,
):
The last four constraints correspond to the conditions necessary for maximizing with respect to local directions only. They are computed for systems
and
with respect to a uniform Fisher–Rao metric and for the two contributions
-
and
-
with respect to a metric compatible with assumptions SEAQT5 of
Appendix A and HE–SEAQT6 and HE–SEAQT7 of
Appendix B.
A distinctive feature of this maximization problem is the double energy conservation constraint: one ensuring that the contribution conserves the overall + mean energy and the other that the contribution conserves the overall + mean energy. This less-restrictive hybrid assumption is crucial because it results in non-Hamiltonian energy exchanges between and and between and but not directly between and .
Taking the variational derivatives of
with respect to
,
,
, and
and setting them equal to zero yields, in terms of the local nonequilibrium Massieu operators,
and, therefore,
The Lagrange multipliers
,
,
,
,
are found from the solution of the system of equations obtained by substituting Equations (
142) and (143) into the conservation constraints such that
Under the stated HE assumptions (SEAQT5, HE–SEAQT6, HE–SEAQT7), the above equations reduce to the following for the local density operators and are similar to Equation (
A35) except for the double
’s, i.e., the two SEA potentials
and
instead of a single one:
Using the same procedure as in the derivation of Equations (
87) and (
88) from Equation (
72), Equation (
148) together with
and
yields the following relations:
where
so that the equivalent expressions of Equations (
95) and (
97) become for the present case
The system of equations that determines the Lagrange multipliers
,
,
,
,
is then written as
and, using Equations (
153), may be rewritten as
Recalling the definitions of
and
(Equation (116)),
and defining
the solution to the system of Equations (
158)–(
160) for the multipliers
is given by
The rate of change of the energy of
is now expressed as
and the energy balance equations for the three subsystems (recall that the notation adopted is [
69],
and
) are
The rates of change of the entropy of
,
, and
are given by
which identifies
as the effective inverse temperature of the HE system
, relating its energy and entropy changes through a stable-equilibrium Gibbs-like relation.
Two other effective temperatures,
and
, define the ratio of energy to entropy flows between
and
, and between
and
, respectively, via the typical heat-interaction expressions expressed as
As a result, the following consistent entropy balance equations for the three subsystems are written as
where the expressions for the entropy generation rates in the three systems, clearly
, are
These relations, for example, show that a steady state for
, defined by the condition that
and
, requires that
obey the following weighted sum of the inverse temperatures of
and
:
The two limiting cases—when
relaxes much faster than
and
and when
relaxes much more slowly—are highlighted by the limit expressions in that equation.
Another important special case arises when
and
. In this limit,
,
,
,
, and systems
and
model the behavior of heat baths. Furthermore, by adjusting the time dependence of the parameters
and
and the HE Hamiltonians
, the NH-HE–SEAQT equations (
147)–(149) can model a quantum thermal machine
coupled to two reservoirs within a fully thermodynamically consistent framework (see, e.g., [
38,
73]).
10. Conclusions
In this work, a rigorous mathematical foundation for the HES concept within the framework of SEAQT is established. Using a general Hilbert space decomposition, a precise operator-level definition of HES’s is provided, and the reduced dynamical equations for their associated intensive parameters derived. A central result of this work is the proof of the invariant-manifold property, which demonstrates that the SEAQT equation of motion preserves the M-th-order HE structure. This justifies the use of HE variables as a consistent reduced-order representation of full quantum dynamics, ensuring that an initial “mixture of canonicals” remains within its own family during evolution.
The HE–SEAQT framework is also extended to model composite systems via an NH–SEAQT approach. Unlike standard models where energy exchange is restricted to interaction Hamiltonians, the NH–SEAQT approach uses an ‘entropic coupling’—a direct dissipative driving of energy exchange between subsystems via the less-constrained SEA dissipative term. This allows for a thermodynamically consistent description of heat-diffusion, mass-diffusion, and heat-and-mass-diffusion interactions between subsystems even in the far-from-equilibrium domain. When mean energy and particle numbers are constrained globally, the NH–SEAQT equation effectively captures the exchange of energy, entropy, and constituents between subsystems that are not necessarily close to mutual equilibrium.
Finally, the theoretical positioning of the HE–SEAQT model is clarified by establishing its formal consistency with the rate-controlled constrained equilibrium (RCCE) method. This connection identifies the evolving HE parameters as physical constraint potentials, unifying the SEAQT dissipative structure with maximum-entropy principles. These links validate the HE–SEAQT approach as a robust, computationally efficient framework for reduced-order modeling of complex, far-from-equilibrium phenomena. The mathematical consistency demonstrated here supports its ongoing application to diverse problems in quantum transport, chemical kinetics, and microstructural evolution, providing a bridge between fundamental quantum dissipation and macroscopic nonequilibrium thermodynamics.