Directed walks shape a universal square-root law of entropy production rate in nonreciprocal systems
Authors: Thiparat Chotibut, Ewa Gudowska-Nowak, Maciej A. Nowak
Organizations: Chula Intelligent and Complex Systems Center of Excellence, Department of Physics, Faculty of Science, Chulalongkorn University, Bangkok 10330, Thailand · Institute of Theoretical Physics and Mark Kac Center for Complex Systems Research, Jagiellonian University, 30-348 Krak´ow, Poland
The entropy production rate (EPR) quantifies irreversibility of a nonequilibrium steady state, yet standard formulas obscure how a complex interaction network generates it. For multivariate Ornstein-Uhlenbeck dynamics on such networks, we express the EPR as a quadratic form in antisymmetric matrices measuring the nonreciprocity of aggregate directed walks at every length, and, equivalently, as two weighted-walk quantities: pairs of directed walks sharing both endpoints, and directed closed walks. For diagonalizable interactions, an exact correspondence translates these walk quantities into eigenvalues and biorthogonal eigenvector overlaps. Across dense, sparse, and deep acyclic random interactions satisfying matched-walk conditions, the mean EPR per node universally follows the square-root law φ∗(g)=1−1−g2, where g∈[0,1) parametrizes the interaction strength. Deep acyclic interaction matrices are nilpotent, with all eigenvalues fixed at zero for every g, yet, as their depth increases, their mean EPR per node approaches φ∗(g). Thus, the square-root law arises from directed walk properties, rather than from a shared spectral density or specific network topology.
Figures & tables
Figure 1: The matched-walk prediction and the square-root law. Numerical ensemble mean EPR per node (symbols) for acyclic networks and large- N contractive recurrent ensembles agree with the analytic predictions shown in curves. The finite-depth feedforward curves follow Eq. ( 21 ) and converge to the square-root law ϕ∗(g) as L→∞ . The vertical dashed line at g2=1 marks the radius-of-convergence boundary of the Catalan series resummation over all walk lengths, indicating the divergence of the susceptibility d(g2)dϕ∗=21−g21 as g→1− . Table 2 summarizes the ensemble construction. Numerical details are in SM M.
Figure 2: Dissipation is non-monotonic in edge probability. For centered dense Erdős-Rényi networks the effective interaction is g2=g02p(1−p) , so the EPR rises then falls with edge probability, peaking at p=1/2 : beyond half-filling, adding edges dilutes the effective interaction strength and lowers dissipation. The square-root law ϕ∗(g) predicts the full EPR (solid lines) at fixed g02∈{1.502,1.752,1.902,1.942} . Symbols are large- N ensemble means from direct Lyapunov solution, conditioned on ρ(W)<1 , with error bars showing SD across retained realizations. The dashed g02=4 envelope touches the Catalan-series convergence boundary g2=1 at p=1/2 ; see SM M. This is an analytic benchmark for the edge-probability dependence reported numerically in [ 36 ] .
Ensemble
Construction
Details
Real Gaussian
Wij=gZij/N for i=j , Zij∼iidN(0,1) , Wii=0
SM I
Rademacher
Wij=gεij/N , P(εij=±1)=1/2 , Wii=0
SM I 4
Centered dense ER
Wij=g(Aij−p∗)/Np∗(1−p∗) for i=j , Aij∼Bernoulli(p∗) , Wii=0 ; p∗=1/4 in Fig. 1
SM I 3
Sparse directed ER
Wij=Aijξij for i=j , with Aij∼iidBernoulli(c/N) ; the ξij are iid, independent of the Aij , and satisfy Eξij=0 and Eξij2=g2/c . Fig. 1 uses the mean degree c=8 and ξij∼N(0,g2/c) ; Wii=0
SM J
Layered feedforward
N=Ln : L ordered layers V1,…,VL of width n ; the only nonzero blocks are the forward blocks Vℓ→Vℓ+1 , Gℓ:=Wℓ+1,ℓ=gXℓ/n for ℓ=1,…,L−1 , where Xℓ∈Rn×n and each element in {(Xℓ)ij} is iid N(0,1)
SM K 1
Oriented out-tree
Rooted tree with edges directed parent-to-child and We=gξe ; the ξe are iid, and Eξe2=1 . Fig. 1 uses uniform Cayley trees with ∣ξe∣=1
SM K 2
Table 2: Ensembles used in Fig. 1 . Each realizes the common asymptotic mean-squared interaction strength per node g2 in Eq. ( 24 ). The last column lists the corresponding section number in the SM.
Dynamical systems studies how states evolve over time, including stability, feedback, chaos, and transitions in physical, biological, and engineered systems.
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