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Network-Independent Synchronous Stability Boundary and Spontaneous Synchronization

Yu Yuan  *

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26 November 2025

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28 November 2025

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Abstract
Synchronization is a fundamental phenomenon in complex systems, with conventional theory positing that its stability crucially depends on network topology and system parameters. However, these information often incomplete in real world scenarios. Here, we derive a elegant boundary equation for synchronous stability and report a new type of spontaneous synchronization near the boundary. Simulation experiments and mathematical proofs demonstrate that both the boundary and spontaneous synchronization are independent of the network. These results challenge the structural foundation of synchronization on complex networks. The framework establishes that the emergence of synchronization phenomena originates from fundamental principles transcending network. This work offers a novel unified perspective on synchronization phenomena in diverse fields.
Keywords: 
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Subject: 
Physical Sciences  -   Other

1. Introduction

Synchronization occurs when interconnected units—from fireflies to generators—adjust their rhythms to act in concert. This collective behavior is crucial for understanding the function of diverse complex systems [1]. Current research relies on a traditional framework to constructively understand synchronization. This framework posits that knowledge of the network architecture (e.g., the adjacency matrix) and each unit’s dynamics is a prerequisite for predicting collective outcomes [2,3].
This framework, however, faces some fundamental obstacles in real world systems: interactions are difficult to fully observe, structural data are incomplete, and exceedingly large networks lead to prohibitive computational costs [4,5,6]. These issues are compounded by higher-order interactions, nonlinear dynamics, and parametric uncertainties [7]. Power grids exhibit key complex network features and the dynamics of generators, described by the swing equation, is equivalent to the well-studied Kuramoto model [1,2]. Additionally, the very real world attributes of power grids, their vast scale, structural complexity, and dynamic nonlinearity, make them a domain where obtaining the requisite information is profoundly challenging. These factors make the power grid a suitable test bed for the synchronization of complex networks [8,9,10,11]. Currently, prevailing analytical methods for power systems have made significant progress, yet they remain constrained by these challenges [1,12,13,14,15,16]. Among these, two prominent strategies are the identification of the synchronous stability boundary, a cornerstone concept in grid stability defined as the union of critical points beyond which the system desynchronizes [15,17,18], and the study of spontaneous synchronization conditions, wherein systems self-organize without external guidance [2,16,19].
Here, we introduce a novel framework grounded in a principle (or consensus) regarding synchronization. This framework reveals that synchronous stability is governed by boundary. We derive and rigorously prove an elegant equation that universally describes this boundary for power systems. A pivotal insight is that this equation is independent of any specific network, providing a general criterion for stability. Here, the network encompasses both the network topology and the system parameters (e.g., line impedance, inertia constants and damping). To enable its application to multigenerator systems, we developed a novel and effective reduction method for higher-order interactions. This algorithm also holds potential for interdisciplinary applications. The validity of this boundary equation and the reduction algorithm is confirmed through mathematical proofs and simulation experiments.
This work also yielded other significant results. First, the boundary equation unifies the seemingly contradictory phenomena of symmetry and asymmetry, showing that both can enhance synchronization. Second, we identify a new type of spontaneous synchronization that emerges exclusively near the stability boundary and is therefore likewise independent of the network. Most significantly, these findings, particularly the network-independent nature of both the stability boundary and the associated spontaneous synchronization, challenge the structural basis of synchronization on complex networks. This framework provides a unified and powerful approach to studying synchronization amid real-world complexity and uncertainty, with conclusions that have direct implications for a wide range of disciplines.
Stability boundary
Synchronization emerges when the suppression (of the loss of synchrony) dominates the dissimilarity, a simple principle regarding synchronization from which we derive the synchronization stability boundary equation [2]. The system is synchronous and stable when the suppression term P Δ u , exceeds the dissimilarity term P u and loses synchronization when P Δ u < P u . Consequently, the condition P Δ u = P u defines the synchronous stability boundary, described by the following equation (see appendix B):
u K = u L u L / u K = 2 cos δ K , L 1
Strictly speaking, this equation defines the boundary of the physically admissible domain—that is, the set of all possible system states that comply with fundamental physical laws (see appendix D). In this paper, we interpret this physically admissible domain as representing the system’s synchronization stability region. This explanation is reasonable for two reasons: 1) physical existence is a prerequisite for stability; 2) for power systems, our experiments confirm that the two boundaries are indistinguishable in all tested scenarios.
In power systems, the voltages u K and u L of the Kth and the Lth generators, and the angle difference δ K , L of their rotation rates (where δ K , L = δ K δ L 0 ) are considered. Here, the rotation rate of a generator is characterized by an angle of rotation rate (ARR) δ K (not the phase angle), and synchronization corresponds to δ 1 = = δ K = δ L = = δ n . The voltage has been previously overlooked for simplicity [16,20] but is crucial for the synchronization stability of the grid [refer to Figure 1(c)].
Eq. (1) actually defines the synchronous stability boundary for two generators. For multigenerators systems, since all boundary equations of pairs of generators share identical forms, the visualized graphs completely coincide, as shown in Figure 1(a).
The expression in Eq. (1) establishes a formal link between synchronous stability and “pairwise interactions.” It is crucial to note, however, that the interactions among generators are inherently higher order. Therefore, to enable stability analysis within this framework, our method employs a mathematical transformation (Eq. S2) that maps these higher-order interactions into pairwise interactions between meta-generators. The meta-generator is the direct result of this transformation, and its successful application (as detailed in Figure 1 and Figure 2) validates its functional equivalence to an effective reduction method. Unlike the generator system, for the Kth and the Lth meta-generator, L=K+1. Unlike the generator perspective (Figure S2), the meta-generator framework endows the “synchronization stability” relation with the property of an equivalence class. This crucial property thereby provides a rigorous foundation for analyzing synchronization stability at the subsystem level and for investigating phenomena such as partial synchronization (Figures 1(b) and 2(a)).
Critically, this transformation preserves synchronization stability (see appendix F), which ensures a strict equivalence in the stability states between the generator and meta-generator systems. This equivalence establishes a powerful validation framework: demonstrating that the stability boundary correctly classifies the meta-generators (Figure 1 and Figure 2) directly confirms its validity for the original generator system. This algorithm has no direct connection to specific physical scenarios, and therefore can be applied directly across different disciplines.
A New England test system was used. A three-phase short-circuit ground fault occurred at node 18. The data in Figure 1 are derived from numerical simulation experiments. Δ t represents the fault clearing time, and d ( Δ t ) = 0.001   s denotes the step length typically used in power system studies.
(a). Visualization of the stability boundary. The stability boundary in Eq. (1) (blue surface and dark green plane) and the pink planes 0 u L δ K , L , u K 0 δ K , L and u K u L 0 collectively define the boundaries and enclose the stability domain. The identical boundary form enables a unified stability assessment.
(b). Synchronization stability and partial synchronization. ( u K , u L , δ K , L ) represents the three-dimensional (3D) coordinate point formed by the Kth and Lth meta-generators. ( u K , u L , δ K , L ) are calculated via Eqs. (S3) and (S4). At fault clearing time Δ t = 0.154 s , all coordinate points cluster near the boundary (cyan). At Δ t = 0.155   s , three coordinate points [ ( u 1 , u 2 , δ 1 , 2 ) , ( u 2 , u 3 , δ 2 , 3 ) , and ( u 9 , u 10 , δ 9 , 10 ) ] deviate outside the boundary, whereas the others remain clustered near it (magenta). The position of the point relative to the boundary directly diagnoses the synchronization state.
(c). Tracking the onset of desynchronization. The temporal trajectory of coordinate point u 1 , u 2 , δ 1 , 2 is shown for the unstable case ( Δ t = 0.155   s ). The calculation range is 6 s T 9 s . Each cyan point represents the mean position of u 1 , u 2 , δ 1 , 2 for a period of 1 second. The time T and the time interval d T = 1 s are defined in Eq. (S5). The trajectory crosses the stability boundary outwardly [(7 s, 8 s)], preceding a rapid increase in the angle difference δ K , L [(9 s,10 s)]. The outward crossing of a trajectory across the boundary pinpoints the onset of synchronization loss.
(d) and (e). Experimental validation of the stability ( Δ t = 0.154 s and Δ t = 0.155   s ). The horizontal axis represents the time. The vertical axis represents the value of δ i ( t ) . δ i ( t ) are calculated with simulation software and Eq. (S2). The maximum value is represented by δ max ( t ) (magenta), and the minimum value is represented by δ min ( t ) (cyan). In the stable case ( Δ t = 0.154 s ), δ max ( t ) δ min ( t ) 1 ° , indicating sustained synchronization. In the unstable case ( Δ t = 0.155   s ), δ max ( t ) δ min ( t ) increases sharply after 9 s ( 14 ° ), confirming system desynchronization.
(f). Experimental verification of partial synchronization. Δ t = 0.155   s . Meta-generator 1 (cyan line) desynchronizes after ~9 s, followed by meta-generators 2 (orange dashed line) and 10 (magenta line). Meta-generators 3~9 form a synchronized cluster (green lines). This pattern matches the cluster prediction from the spatial distribution in (b).
Figure 1(a) visualizes Eq. (1) within a three-dimensional (3D) coordinate system. Geometrically, the surfaces defined by Eq. (1) are fixed, which provides an intuitive indication of its independence from network topology and system parameters. We now proceed to validate this conclusion experimentally. Three lines of evidence confirm that Eq. (1) universally describes the synchronization stability boundary: 1) it distinguishes stable from unstable states [see Figures 1(b) and 2(a)], 2) it captures the stability of multiple swings [see Figures 1(c) and 2(b)], and 3) it explains partial synchronization patterns [see Figures 1(f) and 2(e)].
The boundary equation provides a definitive geometric criterion for power system stability. For a system with n meta-generators, the state is represented by n-1 points in a 3D coordinate space. This representation reveals a powerful discriminative capability: as shown in Figure 1(b), a minute increase in fault clearing time Δ t from Δ t = 0.154   s to Δ t = 0.155   s , a change of merely 0.001 s, causes a dramatic shift in system behavior. Under stable conditions ( Δ t = 0.154   s , cyan), all points cluster at the boundary, whereas at the instability threshold ( Δ t = 0.155   s , magenta), specific points ( ( u 1 , u 2 , δ 1 , 2 ) , ( u 2 , u 3 , δ 2 , 3 ) , and ( u 9 , u 10 , δ 9 , 10 ) ) deviate outside it. This spatial deviation is the direct geometric manifestation of the condition P Δ u < P u , signifying a loss of synchronization. The definitive correspondence between a point’s position relative to the boundary and the system’s physical state is rigorously validated by time-domain simulations: the clustering of cyan points coincides with a bounded difference in δ K in Figure 1(d), whereas the deviation of points from the boundary predicts the large, growing desynchronization evident in Figure 1(e). The reproducibility of this exact discriminative function in the topologically distinct 3-generator system (Figure 2(a), (c) and (d)), along with analogous results under varied fault scenarios (Figure S5), provides robust, multiscenario evidence that the boundary’s role as a stability criterion is an inherent property, independent of the network topology or perturbation [2,21,22]. To thoroughly validate the universality of the boundary equation, we conducted tests on all 39 nodes of the New England test system (Table S1 for details). Across all 78 stable and unstable cases, Eq. (1) achieved discrimination with an accuracy of 100%.
Furthermore, Figure 1(b) provides a novel and direct geometric diagnosis of partial synchronization. The positions of the 9 coordinate points reveal distinct synchronization clusters. Specifically, points ( u 1 , u 2 , δ 1 , 2 ) , ( u 2 , u 3 , δ 2 , 3 ) , and ( u 9 , u 10 , δ 9 , 10 ) residing outside the boundary indicate that the corresponding meta-generators (1st, 2nd, and 10th, respectively) have lost synchronization stability. This result effectively divides the system into four synchronization groups: three desynchronized individual units (1st, 2nd and 10th) and one synchronized cluster comprising meta-generators 3rd through 9th. The time-domain results in Figure 1(f) are in perfect agreement with this diagnosis, confirming the manifestation of cluster synchronization[23,24]. Our approach thus offers a unified geometric interpretation for this phenomenon: cluster synchronization arises from the localized loss of synchronization stability between oscillators when their representative coordinate points lie outside the universal boundary[25,26]. This mechanism, which improves our understanding of partial synchronization, is further corroborated by additional data (Table S1). Critically, this diagnostic framework is universally applicable in power systems, as demonstrated by the consistent combination of geometric diagnosis in Figure 2(a) and time-domain validation in Figure 2(e) for the completely different 3-generator systems.
Figure 1(C) captures the system’s transition from stability to instability, showing coordinate point ( u 1 , u 2 , δ 1 , 2 ) crossing the boundary outwardly during the time interval (8 s,9 s). This event is the direct precursor to the subsequent physical response: a dramatic increase in the angle difference δ 1 , 2 during (9 s,10 s), which leads to the eventual loss of synchronization, as confirmed by the time-domain simulation in Figure 1(E). The consistent temporal sequence—boundary crossing preceding desynchronization—establishes that this crossing marks the real-time onset of synchronization loss. This demonstrates the boundary’s capacity as a dynamic predictor, capable of discriminating the complex phenomenon of multiswing stability for multiple generators[27,28]. Critically, this entire sequence of events, from boundary crossing to desynchronization, is replicated in the completely different 3-generator system (Figures 2(b) and (d)), underscoring universality of the predictive power across networks. Furthermore, the critical role of the voltage term in this predictive boundary suggests that the common assumption of disregarding voltage variations [8] may be inadequate when the system approaches the stability boundary, even for short-term dynamic studies. Ultimately, the synergy between the long-term stability assessment in Figure 1(b) and the short-term transient prediction in Figure 1(c) confirms that the same boundary equation governs stability across different time scales and operational scenarios. This coherence underpins a unified framework for synchronous stability analysis in power systems.
The same analysis as in Figure 1 is applied to the 3-generator system. A three-phase short circuit to a ground fault occurred at the 4-node.
(a). Synchronization stabilization discrimination and partial synchronization. Two coordinate points cluster at the boundary when stable ( Δ t = 0.244   s , cyan dots). u 1 , u 2 , δ 1 , 2 is outside the boundary and away from ( u 2 , u 3 , δ 2 , 3 ) when unstable ( Δ t = 0.245   s , magenta dots).
(b). Stability of multiple swings for multiple generators. Δ t = 0.245   s . Mirroring the dynamics in Figure 1(c), u 1 , u 2 , δ 1 , 2 crosses the boundary outwardly in the time interval 2   s ,   3   s , and δ 1 , 2 rapidly increases in the time interval 4   s ,   5   s . These findings are in good agreement with the results presented in Figure 2(d).
(c) and (d) show the experimental validation of the synchronous stability and the stability of multiple swings for multiple generators. The time-series data corroborate the state predictions in (a), showing maintained synchrony at Δ t = 0.244   s ( δ max ( t ) δ min ( t ) 3 ° ) and loss of synchrony at Δ t = 0.245   s ( δ max ( t ) δ min ( t ) 28 ° ).
(e). The phenomenon of partial synchronization. ( Δ t = 0.245 s ). After approximately 4 s, the system splits into two synchronized clusters. Meta-generator 1 disengages from the cluster (black line). Meta-generators 2 and 3 form a synchronized cluster (red line and blue line).
The 10-generator New England system and the 3-generator system are two canonical test systems recognized as completely distinct in scale, topology, and system parameters, such as line impedance and generator inertia [29,30]. The successful replication of the boundary’s core functions, stability discrimination, multigenerator and multiswing instability prediction, and partial synchronization diagnosis, across these disparate systems provides a formidable foundation for a robust and universal conclusion. Together, this robust, multifaceted validation rigorously demonstrates the recognition that the synchronization stability boundary is independent of network topology, system parameters, and perturbation locations. We demonstrate that the emergence of the stability boundary, as a key function of the network, can be directly established on a simple principle rather than being governed by structural details. This independence between function and network challenges the structural foundations in complex networks [2,21,22]. This finding is further underpinned by rigorous mathematical proof which directly links the emergence of synchronization to the fundamental principle (see appendix D).
By bypassing reliance on network structure and parameters, this framework can judge stability directly from individual state measurements. It thus offers a radically simplified approach to analyzing stability in complex systems. It is particularly noteworthy that the boundary equation u / Δ u = 1 was identified prior to its physical interpretation (Appendix B). This sequence of discovery suggests that the boundary may be rooted in an origin more fundamental than any specific disciplinary context. A key piece of evidence lies in the fact that the generator swing equation used in this work for independent validation is equivalent to the Kuramoto model [1,2]. This equivalence implies that our findings reveal a universal law applicable to all oscillator networks of the same type. Furthermore, the stability boundary derived in this paper, along with its network-independent nature, fundamentally defines the synchronous stability limits for a broad class of oscillator networks. Based on this, extending the “amplitude–frequency” framework (such as u i ( t ) and δ i ( t ) in this work) established in this study to other disciplines such as biological rhythms and chemical oscillators has become a highly promising direction for future research [31,32,33].
This line of inquiry, in turn, leads us to more profound questions: Do other features, similarly independent of structure, exist in complex systems? If so, what is their physical origin? And could their existence imply an underlying, unified description of complex systems?. Seeking answers to these questions is precisely the crucial step toward a new cognitive landscape centered on emergence.
Important implications can be derived from the expression of Eq. (1). Specifically, the left-hand side of Eq. (1) represents the global stability domain [21] (i.e., when u K = u L , δ K , L 0 , P Δ u = P u ).
u K = u L
represents a manifestation of the symmetry of the system. Such symmetry typically originates from underlying topological symmetries in the network and the homogeneity of the oscillators. This finding explains why high symmetry can facilitate synchronization in complex networks and aligns with established understanding [34,35].
Conversely, the variant form of the right-hand side of Eq. (1) is as follows:
δ K , L c r = arccos ( 1 u K u L 2 u K )
reveals that asymmetry can also enhance stability. Such asymmetry often stems from topological asymmetries or heterogeneity. Here, δ K , L c r represents the stability margin of the Kth and Lth meta-generator angle difference of the rotation rate; that is, for ( u K , u L , δ K , L ) , the system remains synchronously stable when δ K , L c r > δ K , L . When u K , u L are sufficiently close [36], δ K , L c r tends to 0. Crucially, δ K , L c r increases with increasing voltage asymmetry u K u L , indicating that the stability domain expands as the system becomes more asymmetric. This finding explains the recently observed synchronization facilitation phenomenon in highly asymmetric systems [37,38]. These findings suggest a practical advantage: because perfect symmetry is fragile under perturbation, designing for controlled asymmetry can be a preferable strategy for maintaining stability. When δ K , L > π 3 , the Kth and Lth meta-generators are not synchronized. Thus, the range of the synchronous stability domain is finite under asymmetric conditions.
Consequently, both high symmetry and high asymmetry may promote synchronization. The expression of Eq. (1) is very simple, however, it harmonizes these two contradictory conclusions well and requires no prior analysis of the network structure.
Spontaneous synchronization in a power system
To understand how systems fail, it is equally important to investigate the behavior of a disturbed system at the stability boundary [39]. When perturbed and near this brink, the system’s trajectory, described by the polar coordinate variable ( u i , δ i ) of the meta-generators, reveals a surprising structure indicative of spontaneous synchronization.
The fault clearing time Δ t increases from 0.140 s to 0.155 s. The 18-node three-phase short circuit to the ground fault. d ( Δ t ) = 0.001   s .
(a). Spontaneous synchronization of meta-generators. The horizontal axis represents the fault clearing time. The vertical axis represents the standard deviation of δ . The yellow area indicates the thin layer where spontaneous synchronization occurs. Here, the standard deviation σ δ i begins to decrease at 0.147 s (magenta) and increases by 1300% at 0.155 s (cyan) when the system is unstable. σ δ i can be calculated via Eq. (S6).
(b). Phenomenon of the potential barrier. Δ t increased from 0.140 s to 0.154 s. The black arrow indicates the direction in which Δ t increased. From Δ t = 0.147   s (the magenta dots) onward, the distance between neighboring points decreased in the direction of the black arrow (elliptical shaded area).
(c). Starting points of spontaneous synchronization. The horizontal axis represents the fault clearing time. The amplified points indicate the starting points of spontaneous synchronization. All the starting points appear at Δ t = 0.147   s . The trends of all δ i were almost identical. Combining (b) and (c) reveals that in this case, the structures in (b) exist between any two meta-generators.
We report a phenomenon of spontaneous synchronization that occurs as the system approaches the stability boundary. This is evidenced by a decrease in the standard deviation σ δ i (Figure 3(a)), indicating that the subsystems’ velocities spontaneously converge toward the mean value, a hallmark of synchronization [13,40]. Crucially, this self-organization is confined to a thin layer (yellow region in Figure 3(a)) immediately preceding the eventual loss of stability at Δ t = 0.155   s . The phenomenon of spontaneous synchronization has been observed across different fault locations (Figure S4) and in distinct test systems (Figure S1), confirming its universality as an intrinsic characteristic of systems approaching the stability boundary. For power systems, this spontaneous synchronization provides a built-in and additional protection for grid stability.
The system’s trajectory in state space reveals a unique structural signature associated with this phenomenon. For a constant step size d ( Δ t ) = 0.001   s , the distance between successive states decreases within the shaded area of Figure 3(b), forming a structure termed a “potential barrier” that exhibits a collective decelerating motion. This spatial manifestation of deceleration emerges precisely at the temporal onset of spontaneous synchronization, i.e., when σ δ i begins to decrease at Δ t = 0.147   s (the magenta dots correspond exactly to Δ t = 0.147   s in Figure 3(b).). To our knowledge, this structure has not been previously reported. A comparison between Figure S3(a) and Figure 3(b) confirms that this barrier structure is not a misleading result introduced by Equation (S2), as it is also present in the generator’s dynamic data. We hypothesize that the formation of ‘barriers’ may be related to the long-range correlations emerging near critical points within the system. This global cooperative dynamics manifests here as trajectory clustering and deceleration.
The precise timeline of spontaneous synchronization is delineated by a distinct transition in the indicator d 2 δ i d ( Δ t ) 2 . As shown in Figure 3(c), the value of d 2 δ i d ( Δ t ) 2 for all meta-generators undergoes a simultaneous and coherent shift at Δ t = 0.147   s (amplified points). This timing coincides exactly with the moment when the standard deviation σ δ i begins to decrease in Figure 3(a), unambiguously linking the reversal in d 2 δ i d ( Δ t ) 2 to the onset of spontaneous synchronization. Prior to this moment, d 2 δ i d ( Δ t ) 2 remains positive; immediately afterward, d 2 δ i d ( Δ t ) 2 becomes negative and remains so. This system-wide reversal indicates that Δ t = 0.147   s is the starting point of the spontaneous synchronization phase. The phase end is clearly indicated by the system’s loss of synchronization at Δ t = 0.155   s , a state change that is demonstrated by the dramatic increase in the standard deviation σ δ i in Figure 3(a) and the corresponding time-domain simulation results in Figure 1(e). Thus, the metastable window of spontaneous synchronization is bounded between Δ t = 0.147   s and Δ t = 0.154   s .
This newly identified spontaneous synchronization constitutes a distinct phenomenon, separate from those previously reported in power grids [11,16]. Existing phenomena typically describe how systems self-organize into synchronized states. In contrast, the novel spontaneous synchronization is uniquely characterized by its occurrence during a forward, perturbation-driven process toward instability and its association with the novel “potential barrier” structure. Second, and more critically, its emergence is strictly confined to the immediate vicinity of the synchronous stability boundary, as evidenced by experimental results under multiple fault scenarios (Figures 3(a) and S4). This refers to the situation where, during spontaneous synchronization, the position of the coordinate point ( u K , u L , δ K , L ) in the 3D coordinate system u K u L δ K , L lies on the boundary. The intimate link between spontaneous synchronization and the stability boundary leads to a profound implication: spontaneous synchronization is independent of the underlying network. Specifically, this independence refers to the fact that its locus within the 3D coordinate system is independent of the network. We corroborate this conclusion by demonstrating the recurrence of the phenomenon in an entirely different 3-generator test system (Figure S1(a)). This independence directly undermines the traditional viewpoint in which spontaneous synchronization is fundamentally governed by network structure [41]. Moreover, the coemergence of this phenomenon with the boundary suggests that they may share a common, deep physical origin.
Our findings, particularly the diversity of behaviors near the stability boundary (e.g., contrasting outcomes in Figures 3 and S1), highlight a crucial question: how to understand the behavior of coupled oscillators before instability occurs. Key questions remain, including the specific conditions for the formation of the potential barrier and the physical determinants of the thickness of the spontaneous synchronization layer. Resolving these questions will be a primary objective of our future research.
Appendix A: Power grid datasets
This study validates the proposed method using two standard and entirely distinct power grid test systems, namely, the WECC 3-generator (3-gen) and the New England 10-generator (10-gen) systems, which differ in network topology, scale, and system parameters. The use of these fundamentally different networks is critical, as it demonstrates the broad applicability of our approach beyond any single, specific system.
For each system, the datasets comprise the dynamic parameters of the generators, the net injected real power at the generator buses, the load demand at the nongenerator buses, and the parameters of all the transmission lines and transformers. This information is sufficient for performing standard power flow and subsequent stability analyses [37].
WECC 3-generator test system (3-gen) [29]. This system represents the Western System Coordinating Council (WSCC), which is part of the region now named the Western Electricity Coordinating Council (WECC) in the North American power grid. There are 3 generators in the system.
New England test system (10-gen) [30]. The IEEE 39-bus system is the 10-machine New England Power System. The prototype of the IEEE 39-node system is a model of an actual power grid in New England. There are 10 generators in the system.
The simulation results from these datasets are presented throughout the paper, with the New England system results primarily shown in Figures 1, 3, and S2-S5, and Table S1, and the 3-generator system results in Figures 2 and S1.
Appendix B: Derivation of the boundary equation
The boundary equation with ω 0
Synchronization emerges when the suppression (of the loss of synchrony) dominates dissimilarity. This is a simple principle (or consensus) regarding synchronization [2]. Here, suppression includes the effects of coupling and dissipation.
The suppression strength between the nodes is quantified by P Δ u , and the dissimilarity between the nodes is quantified by P u . P Δ u and P u have the same dimension and can be directly compared in size. As a natural corollary of the consensus, the boundary is defined by the equality between the suppression and the dissimilarity. Thus, the synchronization stability boundary equation is expressed as P Δ u = P u . When P u P Δ u , the system is synchronous and stable. Conversely, when P u > P Δ u , the system is out of synchronization and unstable.
Figure 1. Schematic representation of the key quantities Δ u and u in the polar coordinate system.
Figure 1. Schematic representation of the key quantities Δ u and u in the polar coordinate system.
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Fig. B1 provides an analogical interpretation using a phasor diagram for power system analysis. Δ u represents the “suppression potential difference”, while u represents the “dissimilar potential difference” between the K-th and L-th generators. Δ u and u are calculated via Eq. (B3).
(a). Steady state during synchronous operation. Each magenta dot represents the coordinate of the i-th meta-generator u i δ i . The cyan line has a length equal to the generator’s voltage u i . The angle of rotation rate (ARR) δ i of this line is defined by the generator’s rotation rate, which is calculated as δ i = 2 arctan ( ω i * ) = 2 arctan ( ω i ω 0 ) . Here, ω i * is the normalized rotation rate, where ω i is the actual value and ω 0 is the power system base frequency. When all the generators are synchronized, the case is characterized by δ K , L = 0 , Δ u u = 0 .
(b). State during asynchronous operation. The length of the orange dotted line between the magenta square dots represents the magnitude of Δ u , and the length of the solid blue line between the cyan dots represents the magnitude of u . When the generator frequencies differ, the case is characterized by δ K , L > 0 , Δ u > 0 , u > 0 .
The algebraic and geometric models of the voltage phasor diagram, which plays a critical role in power system analysis, provided inspiration for the expressions of P Δ u and P u . The expressions for P Δ u and P u are analogous to those of P K , L = U K U L 2 Z K , L , which represents the rate of energy dissipation between the nodes in a power system.
P Δ u = u K u L 2 Z K , L = Δ u 2 Z K , L
and
P u = u K u K u L u L 2 Z K , L = u 2 Z K , L
[see Fig. B1(b)]. Z K , L represents the impedance between the Kth and the Lth generators. The difference between u i and U in a physical sense is that the ARR δ i of u i is defined by the frequency ω i , whereas the angle θ i of U represents the phase angle.
The expressions of P Δ u and P u indicate that they are related to the network because information about the network is contained in Z K , L (e.g., the adjacency matrix and system parameters). However, for any two generators K and L, Z K , L is the same in the expressions of P Δ u and P u . P u / P Δ u = 1 eliminates Z K , L . Therefore, the boundary equation P u / P Δ u = 1 is independent of disturbances, network topology, and system parameters. Although these factors collectively determine the system’s dynamic trajectory and generator operating points, the mathematical form and geometrical shape of the stability boundary itself remain invariant. Combining Eqs. (B1) and (B2), it is observed that P u / P Δ u = 1 u / Δ u = 1 . The set of points for which u = Δ u is the synchronous stability boundary.
As shown in Fig. B1(b),
Δ u = u K u L = u K 2 + u L 2 2 u K u L cos δ K , L , u = u K u K u L u L = 2 u K 2 ( 1 cos δ K , L ) .
The symbols “∆” and “ “ are for distinction only and have no mathematical significance. Thus, the boundary equation is obtained via derivation from u K 2 + u L 2 2 u K u L cos δ K , L = 2 u K 2 ( 1 cos δ K , L ) . The only variables in the boundary equation are u K , u L and δ K , L . These physical quantities are all representations of individual behavior.
f u K , u L , δ K , L = u / Δ u = 1 is the stability boundary equation. When u / Δ u < 1 , the system is stable. When u / Δ u > 1 , the system is unstable. Geometrically, f u K , u L , δ K , L = 1 describes exactly curved surfaces that, together with ( 0 , u L , δ K , L ) , ( u K , 0 , δ K , L ) and ( u K , u L , 0 ) enclose a stable domain.
The boundary equation
u K = u L u L u K = 2 cos δ K , L 1
where u K u L 0 , δ K , L 0 . This is Eq. (1) in the main text.
The coordinate system u K u L δ K , L is established, and the boundary is visualized (Figure 1(a)).
It should be noted that this boundary equation originated from physical intuition and the analysis of simulation data. We observed from the data that the quantity defined by Eq. (B3), where u = Δ u , precisely determines power system stability. This regularity suggested that it could be incorporated into the established physical consensus that “synchronization is determined by a balance between the suppression and the dissimilarity.” Based on this insight, we developed a theoretical framework for P Δ u and P u . The construction of this framework yields an immediate theoretical consequence: the parameter Z K , L , which contains network information, is naturally eliminated under the condition P u / P Δ u = 1 , which is equivalent to u / Δ u = 1 . Consequently, the framework presented in this paper not only unifies empirical observations with physical principles but also reveals the profound property that the stability boundary is independent of the network.
Appendix C: The boundary equation without ω 0
As mentioned in the derivation above, δ i = 2 arctan ( ω i * ) = 2 arctan ( ω i ω 0 ) , where ω 0 represents the power system base frequency and ω i denotes the actual value. ω 0 is constrained to positive real numbers. For a power system, the base frequency generally coincides with the rated frequency of the system(50 Hz or 60 Hz in most power grids globally). As previously stated in this paper, ω 0 = 50 H z . ω 0 is used extensively in power system analysis. However, to some extent, the selection of ω 0 remains “anthropic selective”. Additionally, ω 0 may be unknown before synchronization emerges. Can ω 0 be eliminated from the boundary equation (i.e., is there a synchronization stability boundary independent of ω i for power systems)?
When δ i = 2 arctan ω i ω 0 is substituted into Eq. (1),
1 2 ( u L u K + 1 ) = cos [ 2 ( arctan ω K ω 0 arctan ω L ω 0 ) ]
Considering cos 2 α = 1 tan 2 α 1 + tan 2 α and tan ( α β ) = tan α tan β 1 + tan α tan β ,
1 2 ( u L u K + 1 ) = ω 0 2 + ω K ω L 2 ω 0 2 ω K ω L 2 ω 0 2 + ω K ω L 2 + ω 0 2 ω K ω L 2
By setting A = u K u L 3 u K + u L , B = ω L ω K , C = ω L ω K u K u L 3 u K + u L , Eq. (C2) becomes A ω 0 2 + B ω 0 + C = 0 . Therefore,
ω 0 1 , 2 = ω K ω L ± ω K ω L 2 4 u K u L 3 u K + u L ω L ω K 2 u K u L 3 u K + u L
For real-world systems, both ω 01 and ω 02 must be real numbers. This fact provides the basis for proving the boundary equation (see appendix D). There is a constraint that ω K ω L 2 4 u K u L 3 u K + u L ω L ω K 0 . Therefore, the power system is synchronously stable when
0 1 4 ω K ω L 2 ω K + ω L 2 u L u K 1 .
In Eq. (C4), Condition 0 1 4 ω K ω L 2 ω K + ω L 2 , which is derived from Constraint A ω 0 2 + B ω 0 + C 0 and is ultimately driven by the requirement of u L u K 2 cos δ K , L 1 .
1 4 ω K ω L 2 ω K + ω L 2 = u L u K
is the stability boundary without ω 0 . When u K = u L , any value chosen for ω K ω L 0 satisfies Eq. (C4). u K = u L is exactly the left side of Eq. (1). When u K u L , Eq. (C5) is equivalent to the right side of Eq. (1). Eq. (1) and Eq. (C5) are equivalent [see appendix E]. This boundary equation is still determined by the behavior of individuals in the system and is independent of the network.
A comparison of Eq. (1) indicates that Eq. (C5) has a larger range of applicability because Eq. (1) requires prior knowledge of the value of ω 0 . However, for convenience, this paper still uses Eq. (1) for visualization, as shown in Figure 1(a).
This boundary equation originates from physical intuition and analogy. Its rigor was subsequently established through experimental validation and mathematical proofs. The experimental validation results are provided in Figures 1, 2, S2, S3(b) and S5, among others.
Appendix D: Proof of the boundary equation
We prove that Eqs. (1) and (C5) describe the stability boundary. The proof proceeds as follows:
The proof proceeds in two steps. First, we prove that Eq. (C5) represents the boundary. We then prove that Eq. (1) is equivalent to Eq. (C5). Therefore, Eq. (1) is also shown to represent the boundary.
Definitions:
A Domain: Variables are ω K , ω L R , with ω K > ω L > 0 . ω K , ω L represents the frequency of the generator.
B Domain: Variables are ω 01 , ω 02 . ω 01 , ω 02 are the two roots of a quadratic equation A ω 0 2 + B ω 0 + C = 0 . ω 0 represents the common frequency of the power system. The quadratic equation originates from an independent consensus: Synchronization emerges when the suppression dominates dissimilarity.
There exists a pair of invertible algebraic maps, F (see Eq. C3) and F 1 , that establish complete equivalence between the two domains: Let A = 2 u K u L 3 u K + u L .
Forward Map F : ( ω K , ω L ) ( ω 01 , ω 02 ) ,
ω 0 1 = F 1 ( ω K , ω L , A ) = ω K ω L + ω K ω L 2 4 A 2 ω L ω K 2 A , ω 0 2 = F 2 ( ω K , ω L , A ) = ω K ω L ω K ω L 2 4 A 2 ω L ω K 2 A .
Inverse Map F 1 : ( ω 01 , ω 02 ) ( ω K , ω L ) ,
ω K = f 3 ( ω 01 , ω 02 , A ) = A 2 ω 01 + ω 02 2 + 4 ω 01 ω 02 + A ( ω 01 + ω 02 ) 2 , ω L = f 4 ( ω 01 , ω 02 , A ) = A 2 ω 01 + ω 02 2 + 4 ω 01 ω 02 A ( ω 01 + ω 02 ) 2 .
The Principle of Real Numbers: The value of the common frequency ω 0 must be a real number. This stems from an uncontested consensus: For each generator, the measured frequency value must be a real number. Since the common frequency emerges from these individual frequencies, it must consequently be real.
Proof:
The maps F and F 1 establish one-to-one correspondence between the A domain and the B domain within their domains of definition. Thus, the two systems are algebraically equivalent. The analysis of the A domain can be transformed entirely equivalently into the analysis of the B domain.
Define the discriminant: Δ = ω K ω L 2 4 A 2 ω L ω K .
From the expressions of map F , ω 01 R and ω 02 R are real if and only if ω K ω L 2 4 A 2 ω L ω K 0 , i.e., Δ 0 . If Δ < 0 , ω 01 , ω 02 are complex numbers.
In according with the principle of real numbers, the common frequency ω 0 must be a real number. ω 01 , ω 02 are two solutions to ω 0 . This strictly requires that both ω 01 R and ω 02 R must be true. This requirement defines a boundary for the physically admissible region in domain B. The boundary is described by Δ = 0 . Therefore, all physically realizable states must and can only lie within the region satisfying Δ 0 (Physically Admissible Domain).
On the basis of the principle of real numbers and the equivalence of the A and B domains, we can rigorously define the existence limit of synchronization:
Admissible domain: Regions in the A domain that are equivalent to those in the B domain where Δ > 0 .
Boundary: Regions in the A domain that are equivalent to those in the B domain where Δ = 0 .
Forbidden domain: Regions in the A domain that are equivalent to those in the B domain where Δ < 0 . The system state cannot remain stable.
Thus, the equation is as follows:
ω K ω L 2 4 A 2 ω L ω K = 0
strictly delineates the physically achievable region from the physically unachievable region. It constitutes the admissible boundary of the system. This is precisely Eq. (C5), which is equivalent to Eq. (1) (when ω K ω L is true). Therefore, Eq. (1) is also proven to be the stability boundary.
Explanation:
In fact, the equivalence between the synchronously admissible boundary and the mathematical description of the principle of real numbers is shown here. Eq. (C5) is precisely the mathematical expression of that principle. The boundary of the physically admissible domain defines the existence of system states and thus carries more profound implications. Logically, physical admissibility is the cornerstone for discussing stability: A state must physically exist before its stability can be discussed. Our work not only established this boundary but also revealed its remarkable independence from the network.
In this paper, the physically admissible region is interpreted as the stability region. Although the admissible boundary and the stability boundary are not conceptually identical, their equivalence in the context of power systems does not compromise the rigor of this paper for the following reasons:
1, Stability refers to a system’s ability to return to an equilibrium state after being subjected to a disturbance. As detailed in the “experimental steps” section, a disturbance (fault) is applied to a synchronized power system at an engineering-acceptable step size ( d ( Δ t ) = 0.001 s) until the generator system loses synchronization. This demonstrates that the experimental design aligns with the concept of stability. This experimental design also indicates that even if the two boundaries do not perfectly coincide, their discrepancy falls within the acceptable resolution for power systems.
2, All the experimental results demonstrate the successful application of the boundary to synchronization issues, including stability assessment and the multiswing stability for multiple generators. In experiments with different network topologies and disturbance scenarios, the observed stability discrimination results precisely matches the simulation experiments (refer to Figures 1, 2 and S5).
This study reveals that the synchronization stability boundaries are constrained by the principle of real numbers. Here, the direct contribution of this mathematical proof lies in enabling us to understand a counterintuitive conclusion: the synchronous stability boundary is independent of any particular network. More profoundly, the boundary equation is directly grounded in fundamental principles of physics, thereby transcending specific network structures.
Appendix E: Proof of Equivalence Between Eqs. (1) and (C5)
Proof:
Eq. (1) transforms equivalently to Eq. (C2): The derivation from Eq. (1) to Eq. (C2) is presented in “The boundary equation without ω 0 ”. According to this derivation process, when u K u L , ω K ω L 0 , Eq. (1) is clearly equivalent to Eq. (C2).
Eq. (C5) transforms equivalently to Eq. (C2): Eq. (C5) becomes 1 2 ( u L u K + 1 ) = 1 2 ω K ω L 2 ω K + ω L 2 . Expanding the right-hand side of the above equation yields ω K 2 + 6 ω K ω L ω L 2 ( ω K + ω L ) 2 , which is expressed as = 4 ω K ω L ω K ω L 2 4 ω K ω L + ω K ω L 2 = ω K ω L [ 4 ω K ω L ω K ω L 2 ] ω K ω L [ 4 ω K ω L + ω K ω L 2 ] . Let X = ω K ω L , then 4 X 4 X 2 ω K ω L 2 4 X 4 + X 2 ω K ω L 2 = X 2 + ω K ω L 2 X 2 ω K ω L 2 X 2 + ω K ω L 2 + X 2 ω K ω L 2 . When ω K ω L , that is ω K ω L < < ω L ω K , denote X by ω 0 [when the system is stable, ω K ω L < < ω L ω K is true (see Table K1 and other data in “Data availability”)]. The right-hand side of the above equation coincides with the right-hand side of Eq. (C2), hence 1 2 ( u L u K + 1 ) = ω 0 2 + ω K ω L 2 ω 0 2 ω K ω L 2 ω 0 2 + ω K ω L 2 + ω 0 2 ω K ω L 2 . Eq. (C5) is equivalent to Eq. (C2).
Both Eqs. (1) and (C5) are both equivalent to Eq. (C2). Therefore, when u K u L , ω K ω L 0 , and ω K ω L < < ω L ω K , Eq. (1) and Eq. (C5) are equivalent.
Appendix F: Proof that Eq. (S2) does not alter the stability criterion of the system
The section on “Stability Boundary” employs meta-generators to validate the boundary equation. This raises a critical question: could the transformation from a generator to a meta-generator introduce erroneous results that invalidate the verification? In other words, regarding the criterion for synchronous stability, are the two models equivalent before and after the application of Eq. (S2)?
Definitions:
Definition 1: All analyses are conducted within any fixed time window T , T + T . During this time window, define α T as the total duration of periods where δ i ( t ) > δ j ( t ) , and conversely, define ( 1 α ) T as the total duration of periods where δ i ( t ) < δ j ( t ) . Then, α 0 , 1 and T = α T + ( 1 α ) T . δ i ( t ) represents the instantaneous values of the ARR of ith generator.
Definition 2 (the stability of the generator system): The difference in the ARR of generator is defined as δ i δ j = 1 T I [ δ i ( t ) δ j ( t ) ] d t . For ε > 0 , the stability criterion is ε > 0 and the system is stable if and only if δ i δ j ε .
Definition 3 (the stability of the meta-generator system): According to Eq. (S2) and Definition 1, the ARRs of the meta-generator are defined as δ i = 1 T I [ α δ i ( t ) + ( 1 α ) δ j ( t ) ] d t (the ith meta-generator) and δ j = 1 T I [ ( 1 α ) δ i ( t ) + α δ j ( t ) ] d t (the jth meta-generator). Their difference is δ i δ j . The stability criterion uses the same ε as definition 2 does. The system is stable if and only if δ i δ j ε .
Proof:
From the definitions above, it is directly derived that: δ i δ j = 2 α 1 δ i δ j . According to Eq. (S2), δ i δ j 0 . We assume that within the time window, δ i ( t ) > δ j ( t ) holds most of the time, implying that α 1 2 , 1 . For any two generators, δ i ( t ) and δ j ( t ) can always be selected. Therefore, this assumption does not lose generality and is always reasonable.
Theorem (stability assessment equivalence): Under the framework of Definitions 1–3, the generator system is synchronously stable if and only if the meta-generator system is synchronously stable.
The proof is completed by demonstrating the following two corollaries.
Corollary 1 (preservation of stability): If the generator system is stable ( δ i δ j ε ), then the meta-generator system is stable ( δ i δ j ε ).
Proof: From δ i δ j = 2 α 1 δ i δ j and the fact that α 1 2 , 1 implies 2 α 1 1 , it follows that δ i δ j = 2 α 1 δ i δ j ε . Therefore, the meta-generator system is stable.
Corollary 2 (preservation of instability): If the generator system is unstable ( δ i δ j > ε ), then the meta-generator system is unstable ( δ i δ j > ε ).
Proof: The instability of the generator system ( δ i δ j > ε ) physically corresponds to a significant difference in the frequencies of the two generators, i.e., a loss of synchronization. This loss of synchronization implies that the state of one generator is persistently greater than that of the other for the vast majority of the observation window, indicating that the parameter α 1 . Substituting α = 1 into the core identity δ i δ j = 2 α 1 δ i δ j yields δ i δ j = δ i δ j [refer to Figures 1(f), 2(e), S5(c), (f) and (l)]. Therefore, δ i δ j = δ i δ j > ε , and the meta-generator system is unstable.
The two systems are equivalent in stability assessment; that is, Eq. (S2) does not change the stability discrimination of the system. The proof applies to a two-generator system.
Definitions:
Depending on the fault and network conditions, a multigenerator system may form completely different synchronous clusters upon instability, which greatly complicates the analysis of its synchronous stability.
We now prove that the generator system and the meta-generator system retain the same stability even when extended to multiple generators.
Definition 4 (the α matrix): In the case of multiple generators, α in Definition 1 is replaced by the α matrix α = ( α i j ) n × n . There is
δ 1 δ 2 δ n = α 11 α 12 α 1 n α 21 α 22 α 2 n α n 1 α n 2 α n n δ 1 δ 2 δ n
The matrix α = ( α i j ) n × n satisfies all α i j 0 . For any i: α i 1 + α i 2 + + α i n = 1 and α 1 i + α 2 i + + α n i = 1 .
Definition 5 (the stability of the multigenerator system): The power system comprises n generators, which form the set G = { G 1 , G 2 , G n } . For ε > 0 , the stability criterion is ε > 0 . The system is synchronously stable if and only if for any subset { G i , G j } , δ i δ j ε holds. For a power system with n generators, there are n ( n 1 ) subsets.
Definition 6 (the stability of the n meta-generator system): By definition, there are also n meta-generators. These meta-generators form an ordered set, M G = { M G 1 , , M G K , M G L , M G n } . Adjacent meta-generators are defined as ordered subsets { M G K , M G L } within this set. L=K+1. The stability criterion uses the same ε as definition 5 does. The meta-generator system is stable if and only if all adjacent meta-generators { M G K , M G L } are stable, i.e., δ K δ L ε . There are (n-1) ordered sets of { M G K , M G L } .
Proof:
Theorem (stability assessment equivalence): The multigenerator system is synchronously stable if and only if the n meta-generator system is synchronously stable.
The proof is completed by demonstrating the following two corollaries.
Corollary 1 (preservation of stability): If the multigenerator system is stable, then the n meta-generator system is stable.
Proof: For any two generators { G i , G j } , δ i δ j ε holds when the system is stable. That is, max δ min δ ε . Let M = max δ , m = min δ ; then, M m ε .
For the ith and i+1th meta-generators, δ i = k = 1 n α i k δ k and δ i + 1 = k = 1 n α ( i + 1 ) k δ k . Therefore, δ i δ i + 1 = k = 1 n [ α i k α ( i + 1 ) k ] δ k . Let d k = α i k α ( i + 1 ) k ; then, k = 1 n d k = 1 1 = 0 . Let δ k = m + t k ( M m ) , where 0 t k 1 and M m ε . Substitute: δ i δ i + 1 = k d k [ m + t k ( M m ) ] = ( M m ) k d k t k .
Let S + = { k : d k > 0 } , S = { k : d k < 0 } . From k = 1 n d k = 0 , we obtain k S + d k = k S d k = Φ , where Φ = 1 2 k = 1 n d k . Then k d k t k k S + d k * 1 + k S d k * 0 = Φ and k d k t k k S + d k * 0 + k S d k * 1 = Φ . so that k d k t k Φ .
For the vectors α i and α ( i + 1 ) , k = 1 n α i k α ( i + 1 ) k 2 . Thus Φ = 1 2 k = 1 n d k 1 . Therefore δ i δ i + 1 ( M m ) * Φ ε * 1 = ε . According to the Definition 6, the meta-generator system is stable.
Corollary 2 (preservation of instability): If the multigenerator system is unstable, then the meta-generator system is unstable.
Proof: According to definition 5, the multigenerator system instability indicates that at least one generator G k has lost stability relative to all the other generators, i.e., for all k j : δ j δ k > ε . In this scenario, the frequency of G k is significantly faster or slower than that of the remaining generators. Without loss of generality, we assume that this generator runs faster than the others do. By definition of the mate-generator, the natural consequence of this assumption is that G k is directly defined as the mate-generator M G 1 and α 1 k = 1 ( δ 1 = j = 1 n α 1 k δ j = δ k ). It follows that: α i k = 0 for all i 2 .
For i 2 , δ i = j k α i j δ j , since α i k = 0 , and the row sum is 1: j k α i j = 1 . Given δ k δ j > ε for all k j , δ i < ( δ k ε ) j k α i j = δ k ε , while δ 1 = δ k .
since i 2 and δ i < δ k ε = δ 1 ε , it follows that δ 1 δ 2 > ε . The adjacent meta-generators { M G 1 , M G 2 } are out of synchronization. According to definition 6, the meta-generator system is unstable.
The proof applies to a two-generator system when n=2. For the scenarios of a two-generator system and a multigenerator system, the meta-generator system and the generator system are equivalent in terms of synchronous stability assessment. Therefore, for any specific stability analysis tool and stability criterion, we can study the synchronous stability of the original generator system through the meta-generator system.
Explanation:
From the proof, the following conclusions can be derived:
1. The n ( n 1 ) subsets in the generator system are reduced to just n 1 ordered sets in the meta-generator system. This result significantly simplifies the analysis of synchronous stability. This equivalence decomposes and transforms the stability problem of high-order complex systems into a series of easily analyzable problems.
2. When the generator system becomes unstable, we can directly identify the out-of-step generator G k through the α matrix.
3. This equivalence provides the basis for utilizing the meta-generator system to verify the validity of the synchronous stability boundary. Moreover, the results demonstrate that the synchronous stability boundary of high-order complex systems is also independent of the network.
4. This reduction algorithm is solely defined by the frequency value and is agnostic to any specific discipline. Consequently, it can be directly applied to a broader range of fields.

2. Materials and Methods

Simulation experiment and software
The swing equation can be used to analyze the synchronization of the generators and is presented as follows:
d θ i d t = ω i ω 0 d ω i d t = ω 0 2 H i ( P m i P e i D i ( ω i ω 0 ) )
where ω 0 represents the synchronous speed of the system, H i denotes the inertia constant, D i indicates a damping coefficient, and the strength of the interactions and θ i represents the power angle. P m i represents the mechanical power, and P e i represents the electrical power of the ith generator. The swing equation is the power system equivalent of the Kuramoto model [1,2]:
d θ i d t = ω i I i d ω i d t = P i γ i ω i + j = 1 N K i j sin ( θ j θ i )
( γ i : The damping of an oscillator; I i : The inertia constant and K i j : A coupling matrix).
This paper employs the time-domain simulation results of the swing equation to verify the validity of Eq. (1). Therefore, to conveniently obtain more accurate calculation results, each of the two test systems was simulated separately in this paper via the Power System Analysis Software Package[42] (PSASP 7.0), a simulation software. Standard power flow calculations and transient stability calculations were performed in the above network models via this software. Time series data of the response of the generator to network faults in the free state are collected. These data are mapped from generators u i ( t ) , δ i ( t ) to meta-generators u i ( t ) , δ i ( t ) , and the results are visualized.
Experimental steps
To validate the boundary equation, we conducted simulation experiments following this general procedure: induce a line fault in a power grid model, compute the system’s dynamic response, and assess whether the boundary equation accurately discriminates between stable and unstable outcomes.
The detailed experimental steps are as follows. First, the network models for the test systems were constructed within the simulation software. The component and generator dynamic parameters were sourced from refs. 29 and 30. A standard power flow calculation was initially conducted to obtain the steady-state operating condition, which served as the foundational input for all subsequent dynamic simulations. The system frequency was set to a base value of 50 Hz. To observe the inherent system response without external control interventions, all the automated controls were disabled.
Prior to dynamic simulation, the fault scenario was defined. This included the fault location (e.g., Node 18 in the New England test system, as shown in Figure 1 and Figure 3), the fault type, and the fault clearing time Δ t . To investigate the synchronization stability under severe disturbances, all the faults in this study were set as three-phase short-circuits to ground. Such disturbances pronouncedly excite and unveil the inherent nonlinearities and uncertainties in the power system, shifting it from a normal, quasi-linear, and stable operating state into a highly nonlinear and even unstable dynamic regime. The dynamic simulation was then executed, and the rotation rate ω i * and terminal voltage u i ( t ) of each generator were recorded over a time window T of 20 seconds, starting from the fault inception. This extended time window was chosen specifically to capture multiswing stability phenomena.
To observe the disturbed trajectory, we turned off the controls. Prior to performing dynamic calculations, we established the fault location (e.g., node 18 in the New England test system, as shown in Figure 1 and Figure 3) and specified the fault type and the fault clearing time Δ t . To simulate the synchronization stability under large disturbances, all fault types discussed in this paper were set as a three-phase short circuit to ground. We calculated the rotation rate ω i * and port bus voltage u i ( t ) of the ith generator for various fault clearing times Δ t . To test the effectiveness of the approach for the stability of multiple swings, the time window T was set to 20 seconds. That is, using the start of the disturbance as a starting point, we calculated and recorded the generator data for the next 20 seconds. The fault location and type were held constant. The fault clearing time was then systematically increasing step length d ( Δ t ) , and the simulation process was repeated until the system transitioned from a stable state to a loss of synchronization state, as confirmed by the simulation results (e.g., Figures 1(e) and 2(d)).
High-order interactions transform into pairwise interactions
The angle of rotation rate of the ith generator was subsequently calculated as δ i ( t ) = 2 arctan [ ω i * ( t ) ] . The extensive interconnections between generators make stability analysis very challenging (see Figure S2). This challenge is also attributed to the complexity of the network. In essence the connection between generators involves higher-order interactions, as each generator is influenced by more than one other generator within the system. To address these challenges, the concept of a meta-generator is introduced. At moment t, the instantaneous values of the n generator system u i ( t ) , δ i ( t ) , i = 1 , 2 , , n are arranged in descending order by δ ω , relabeled, and then reconstituted as the n meta-generator system u i ( t ) , δ i ( t ) , i = 1 , 2 , , n . In other words, when the condition δ i + 1 ( t ) > δ i ( t ) is true, we relabel the serial number of the generator at that moment:
( u i + 1 ( t ) , δ i + 1 ( t ) ) = ( u i ( t ) , δ i ( t ) ) , u i ( t ) , δ i ( t ) = u i + 1 ( t ) , δ i + 1 ( t ) .
A meta-generator is created by reordering and labeling generators. Note that for the meta-generator, in the subsequent equations of this paper [such as Eq. (1)], L = K + 1. This transformation has been shown not to change the stability of the system [see appendix F] and the dynamic trends of the generators [compare the results in Figures 3(b) and S3(a)].
On the other hand, the meta-generator, defined by Eq. (S2), is the product of a stability-preserving reduction that transforms the system’s high-order dynamics into a sequence of pairwise interactions (L = K + 1). This formulation allows the synchronization stability of the entire system to be analyzed through the collective state of its constituent meta-generator pairs via the unified boundary of Eq. (1).
In this manner, we obtain the meta-generator data u i ( t ) , δ i ( t ) , i = 1 , 2 , , n . Before and after the transformation, the numbers of generators and meta-generators are equal. Except Figures S2 and S3, all results and discussions in this paper are based on the meta-generator.
Data Calculation
The polar coordinates of the ith meta-generator are denoted by ( u i , δ i ) [see Fig. B1]. The 3D coordinate point formed by the Kth and Lth meta-generators is denoted by ( u K , u L , δ K , L ) [see Figure 1]. These points are calculated as follows:
The means of u i ( t ) , δ i ( t ) , i = 1 , 2 , , n over 0 , T were
u i = 1 T 0 T u i ( τ ) d τ , δ i = 1 T 0 T δ i ( τ ) d τ
and
δ K , L = 1 T 0 T δ K , L ( τ ) d τ = 1 T 0 T δ K ( τ ) δ L ( τ ) d τ = 1 T 0 T δ K ( τ ) δ L ( τ ) d τ = δ K δ L .
The results are shown in Figures 1(b), 3(b), S1(a), etc.
The means of u i ( t ) , δ i ( t ) , i = 1 , 2 , , n over [ T , T + d T ] were
u i ( d T ) = 1 d T T T + d T u i ( τ ) d τ , δ K , L ( d T ) = δ K ( d T ) δ L ( d T ) = 1 d T T T + d T δ K ( τ ) δ L ( τ ) d τ ,
where d T represents the time interval. The results are shown in Figures 1(c) and 2(b).
The standard deviation of δ i is calculated as follows:
σ δ i = i = 1 n ( δ i E δ i ) 2 n , E δ i = i = 1 n δ i n .
where E δ i represents the expectation of δ i . The results are shown in Figs. 3(a), S1(a) and S4.
Figure S1. Spontaneous synchronization independent of the network (meta-generator in the 3-gen). The horizontal axis represents the fault clearing time. The fault clearing time Δ t increases from 0.227 s to 0.245 s. A three-phase short circuit to a ground fault occurs at the 4-node. d ( Δ t ) = 0.001   s . (a). Spontaneous synchronization of meta-generators in the 3-gen. The horizontal axis represents the fault clearing time. The vertical axis represents the standard deviation of δ . Here, σ δ i denotes the standard deviation of δ , which begins to decrease at Δ t = 0.227   s (magenta dots) and increases by 2200% at Δ t = 0.245   s (cyan star) when the system becomes unstable (cyan pentagram dots). σ δ i can be calculated via Eq. (S6). (b). Another manifestation of spontaneous synchronization. The slope a δ changes from greater than 1 (cyan stars) to less than 1 (magenta diamonds), and a δ 1 changes from positive to negative. a δ is calculated with the following equation: a δ = d δ K d δ L = δ K ( Δ t + d ( Δ t ) ) δ K ( Δ t ) δ L ( Δ t + d ( Δ t ) ) δ L ( Δ t ) . The moment of a δ = 1 is close to 0.227 s.
Figure S1. Spontaneous synchronization independent of the network (meta-generator in the 3-gen). The horizontal axis represents the fault clearing time. The fault clearing time Δ t increases from 0.227 s to 0.245 s. A three-phase short circuit to a ground fault occurs at the 4-node. d ( Δ t ) = 0.001   s . (a). Spontaneous synchronization of meta-generators in the 3-gen. The horizontal axis represents the fault clearing time. The vertical axis represents the standard deviation of δ . Here, σ δ i denotes the standard deviation of δ , which begins to decrease at Δ t = 0.227   s (magenta dots) and increases by 2200% at Δ t = 0.245   s (cyan star) when the system becomes unstable (cyan pentagram dots). σ δ i can be calculated via Eq. (S6). (b). Another manifestation of spontaneous synchronization. The slope a δ changes from greater than 1 (cyan stars) to less than 1 (magenta diamonds), and a δ 1 changes from positive to negative. a δ is calculated with the following equation: a δ = d δ K d δ L = δ K ( Δ t + d ( Δ t ) ) δ K ( Δ t ) δ L ( Δ t + d ( Δ t ) ) δ L ( Δ t ) . The moment of a δ = 1 is close to 0.227 s.
Preprints 186712 g005
(c). δ K , L decreases as Δ t increases. The magenta line indicates δ 1 , 2 , and the cyan line indicates δ 2 , 3 . In both cases, a significant decrease in the tail is observed; that is, both d δ 1 , 2 d ( Δ t ) and d δ 2 , 3 d ( Δ t ) are less than 0 after Δ t = 0.239   s Preprints 186712 i001
As shown in Figure 3(a), the spontaneous synchronization near the boundary is shown in Figure S1(a). Owing to the monotonicity of δ i with respect to Δ t , i.e., d δ L d ( Δ t ) > 0 . d δ K L d ( Δ t ) = d ( a δ 1 ) δ L + b δ d ( Δ t ) = ( a δ 1 ) * d δ L d ( Δ t ) . As shown in Figure S1(b), a δ 1 < 0 , then d δ K , L d ( Δ t ) < 0 (the results in Figure S1(c) also provide direct evidence). These findings suggest that the Kth and Lth meta-generators are evolving toward synchronization. Unlike Figure 3(b), this result is another manifestation of spontaneous synchronization. These results reveal the complexity of spontaneous synchronization.
Figure S2. “Synchronization stability” loses transferability between generators (in the 10-gen) and the necessity of Eq. (S2). The fault is a three-phase short-circuit ground fault. The disturbed trajectory starts from planes u K u L 0 . δ K , L increases as the fault clearing time increases. Note that the time series data of the generator u i ( t ) , δ i ( t ) , i = 1 , 2 , , n are used here. (a). When failure occurs at node 12, the trajectories of ( u 30 , u 39 , δ 30 , 39 ) , ( u 30 , u 38 , δ 30 , 38 ) and ( u 39 , u 38 , δ 39 , 38 ) . d ( Δ t ) = 0.04   s . The system is stable at 0.285 s (cyan dots) but unstable at 0.286 s (magenta dots). The trajectory of ( u 30 , u 39 , δ 30 , 39 ) (orange solid line) moves closer to and eventually crosses the boundary, but the trajectories of ( u 30 , u 38 , δ 30 , 38 ) (black dashed line) and ( u 39 , u 38 , δ 39 , 38 ) (black solid line) are in the stable domain and move away from the boundary. (b). When the failure occurs at node 18, the trajectories of ( u 30 , u 39 , δ 30 , 39 ) , ( u 30 , u 38 , δ 30 , 38 ) and ( u 39 , u 38 , δ 39 , 38 ) . d ( Δ t ) = 0.02   s . The system is stable at 0.154 s (cyan dots) but unstable at 0.155 s (magenta dots). The trajectory of ( u 30 , u 39 , δ 30 , 39 ) (orange solid line) moves closer to and eventually crosses the boundary, but the trajectories of ( u 30 , u 38 , δ 30 , 38 ) (black dashed line) and ( u 39 , u 38 , δ 39 , 38 ) (black dashed line) are in the stable domain and move away from the boundary.
Figure S2. “Synchronization stability” loses transferability between generators (in the 10-gen) and the necessity of Eq. (S2). The fault is a three-phase short-circuit ground fault. The disturbed trajectory starts from planes u K u L 0 . δ K , L increases as the fault clearing time increases. Note that the time series data of the generator u i ( t ) , δ i ( t ) , i = 1 , 2 , , n are used here. (a). When failure occurs at node 12, the trajectories of ( u 30 , u 39 , δ 30 , 39 ) , ( u 30 , u 38 , δ 30 , 38 ) and ( u 39 , u 38 , δ 39 , 38 ) . d ( Δ t ) = 0.04   s . The system is stable at 0.285 s (cyan dots) but unstable at 0.286 s (magenta dots). The trajectory of ( u 30 , u 39 , δ 30 , 39 ) (orange solid line) moves closer to and eventually crosses the boundary, but the trajectories of ( u 30 , u 38 , δ 30 , 38 ) (black dashed line) and ( u 39 , u 38 , δ 39 , 38 ) (black solid line) are in the stable domain and move away from the boundary. (b). When the failure occurs at node 18, the trajectories of ( u 30 , u 39 , δ 30 , 39 ) , ( u 30 , u 38 , δ 30 , 38 ) and ( u 39 , u 38 , δ 39 , 38 ) . d ( Δ t ) = 0.02   s . The system is stable at 0.154 s (cyan dots) but unstable at 0.155 s (magenta dots). The trajectory of ( u 30 , u 39 , δ 30 , 39 ) (orange solid line) moves closer to and eventually crosses the boundary, but the trajectories of ( u 30 , u 38 , δ 30 , 38 ) (black dashed line) and ( u 39 , u 38 , δ 39 , 38 ) (black dashed line) are in the stable domain and move away from the boundary.
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The numbers 30 and 39 indicate that the two generators are connected to nodes 30 and 39, respectively, in the 10-gen test system. “38” also applies this convention. A comparison of the results in Figure S2 and Table S1 reveals that the boundary can also determine the synchronous stability of the system. These results reveal the validity of the synchronous stability boundary. However, compared with meta-generator models, generator models have the following drawbacks:
1. δ K and δ L are difficult to define. For a system with n generators, N ( N 1 ) perturbed trajectories must be examined. This increases computational costs.
2. When Δ t = 0.3   s , generators 30 and 38 are synchronized, and generators 38 and 39 are synchronized, but generators 30 and 39 are not synchronized as shown in Figure S2(a). Similar conclusions are shown in Figure S2(b). These results are clearly illogical.
The examples in Figure S2 reveal that for a generator system, “stabilization” occurs for the entire system, and determining which generator is out of step is challenging. “Synchronization stability” results in a loss of transferability between generators. This is the primary challenge facing generator systems in large-scale networks. This difficulty stems from the fact that the couplings between generators involve higher-order interactions rather than simple pairwise interactions, as each generator is affected by multiple other generators within the same system. Therefore, the generator system cannot directly provide information about subsystem levels such as coherent groups. Therefore, the introduction of the meta-generator concept is crucial for analysis.
Figure S3. Self-organization behavior of generators near the boundary (generators in the 10-gen).
Figure S3. Self-organization behavior of generators near the boundary (generators in the 10-gen).
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Three-phase short-circuit ground fault at the 18-node. Δ t increases from 0.140 s to 0.154 s. d ( Δ t ) = 0.001   s . The black arrow indicates the direction in which Δ t increased. Note that the time series data of the generator u i ( t ) , δ i ( t ) , i = 1 , 2 , , n are used here.
(a). Phenomenon of the potential barrier on plane δ 30 δ 39 ( the generator). As shown in Figure 3(b), from 0.147 s (the magenta dots) onward, the distance between neighboring points decreased in the direction of the black arrow (shaded area). The points are calculated via Eq. (S3).
(b). Position of the thin layer where spontaneous synchronization occurs in the 3D coordinate system u K u L δ K , L . The bottom of the gray shaded area indicates the boundary. At Δ t = 0.146   s , ( u 30 , u 39 , δ 30 , 39 ) reaches the boundary. Within the range from 0.147 s to 0.154 s, ( u 30 , u 39 , δ 30 , 39 ) remains within the thin layer (gray shaded area), which coincides precisely with the period during which spontaneous synchronization emerges.
The potential barrier of the generator is similar to that of the meta-generator, as shown in Figure 3(b); that is, the barrier of the generator is the same as that of the meta-generator. The existence of a metastable region formed by spontaneous synchronization close to the boundary is shown in Figure S3(b). When the system operates in this region, spontaneous synchronization occurs, delaying system destabilization. This provides an additional layer of protection for the stability of the power system.
Figure S4. Spontaneous synchronization always occurs when the system becomes unstable. (Meta-generator in the 10-gen test system). A three-phase short-circuit ground fault is set at the corresponding node. The black arrow indicates the direction in which Δ t increased.
Figure S4. Spontaneous synchronization always occurs when the system becomes unstable. (Meta-generator in the 10-gen test system). A three-phase short-circuit ground fault is set at the corresponding node. The black arrow indicates the direction in which Δ t increased.
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(a)–(e). Spontaneous synchronization phenomena under different fault conditions. As in Figure 3(a), the horizontal axis represents the fault clearing time. The vertical axis represents the standard deviation of δ i . The phenomenon of σ δ i decreasing occurs only near the point of instability. The faults are at nodes 6, 12, 24, 30 and 36. No regular pattern is observed for the distribution of the positions of these nodes in the network. σ δ i was calculated via Eq. (S6). These repeated results indicate that this novel phenomenon of spontaneous synchronization is not accidental.
(f) and (g). Phenomenon of the potential barrier on plane δ 1 δ 2 (the faults at the 6-node (0.114 s~0.124 s) in (f) and 24-node (0.126 s~0.135 s) in (g)).The points crossed the potential barrier (shaded area). The points are calculated via Eq. (S3).
Similar to Figure 3, the results reveal that σ δ i significantly decreases where the system is about to become unstable, and a “potential barrier” appears in some cases. These results indicate a strong correlation between the synchronization stability boundary and spontaneous synchronization.
Figure S5. Further evidence regarding the validity of Eq. (1). (meta-generators in the 10-gen).
Figure S5. Further evidence regarding the validity of Eq. (1). (meta-generators in the 10-gen).
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A New England test system was used. A three-phase short-circuit ground fault is set at the corresponding node. The faults are located at nodes 6 (a–c), 24 (d–f), and 36 (g–i). d ( Δ t ) = 0.001   s . The blue surface in panels (a), (d), and (g) is the synchronization stability boundary described by Eq. (1). Panel (a) shows the positions of ( u K , u L , δ K , L ) when Δ t = 0.124 s (cyan) and Δ t = 0.125   s (magenta). Panels (b) and (c) are the simulation results of δ max (magenta line) and δ min (cyan line) for cases Δ t = 0.124 s and Δ t = 0.125   s , respectively. The panels in the other rows use a similar correspondence.
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)
BUS No. ∆t (s) stability δ1 (°) U1 (p.u.) δ2 (°) U2 (p.u.) δ3 (°) U3 (p.u.) δ4 (°) U4 (p.u.) δ5 (°) U5 (p.u.)
1BUS 0.410 1 95.11555411 0.972148631 94.92885679 0.973716987 94.81681981 0.97448043 94.727995 0.971945477 94.65814985 0.974931179
0.411 0 116.2838975 0.787539945 95.17936924 0.945323128 95.02558851 0.952272919 94.93012487 0.951782769 94.85370453 0.960884043
2BUS 0.169 1 96.04069551 0.960258826 95.8785429 0.965856947 95.77207434 0.958046877 95.69266479 0.957502269 95.62255917 0.964113913
0.170 0 107.8380972 0.736833073 106.4727572 0.782240045 105.9099072 0.761523438 105.5710704 0.77734927 103.4279355 0.879271019
3BUS 0.155 1 95.93970595 0.962107621 95.77882717 0.962144193 95.68308109 0.95929918 95.61034772 0.963636157 95.54300897 0.964995462
0.156 0 115.1120065 0.708101864 106.0805204 0.8763196 105.915216 0.895178931 105.798553 0.903385962 105.7174657 0.917328581
4BUS 0.144 1 95.49943802 0.963207476 95.33631336 0.96354949 95.22257344 0.973346457 95.13473041 0.974280975 95.05640969 0.97051974
0.145 0 113.7028178 0.717026117 106.2733036 0.872775282 106.0989124 0.879218006 105.9890866 0.90616004 105.9052054 0.918249115
5BUS 0.128 1 94.52320443 0.969090585 94.36701698 0.976674953 94.24864075 0.987336377 94.15638351 0.987375677 94.07229309 0.994060865
0.129 0 115.9831999 0.773989975 94.52959525 0.964788781 94.40928277 0.97531902 94.32941425 0.972376952 94.26325248 0.973208376
6BUS 0.124 1 94.46098178 0.973053278 94.28678393 0.977291604 94.16608912 0.992088171 94.08132732 0.988349925 94.00230227 0.988741399
0.125 0 116.3065577 0.758977216 96.10567456 0.933971214 95.95487764 0.947303483 95.84717312 0.951647661 95.74990573 0.955337441
7BUS 0.148 1 94.42207976 0.972385172 94.25139816 0.978490575 94.12735511 0.991819425 94.04416404 0.990110255 93.96456484 0.991832264
0.149 0 116.0029089 0.775363888 94.47784506 0.963737171 94.35502368 0.973952579 94.27228721 0.972884263 94.20339521 0.978896372
8BUS 0.146 1 94.45665354 0.973155312 94.28350283 0.976244833 94.16013147 0.992475927 94.07595345 0.989382604 94.00092242 0.989227246
0.147 0 116.2077842 0.758953048 95.2643495 0.931248586 95.0706542 0.952026682 94.96194403 0.950911379 94.87450075 0.958051534
9BUS 0.305 1 95.03771918 0.964372529 94.84728485 0.966554948 94.72809603 0.981846217 94.63468125 0.979325052 94.55206921 0.985364243
0.306 0 115.6459655 0.767382344 95.27456994 0.94403028 95.11519555 0.955202859 95.02661015 0.962191709 94.95649674 0.968149985
10BUS 0.136 1 94.5195023 0.970495937 94.37067529 0.977765182 94.25033802 0.985164963 94.15875226 0.989552314 94.07188875 0.990737136
0.137 0 116.2008942 0.768276577 95.21773162 0.938303193 94.96491263 0.957196997 94.86989747 0.957897196 94.79466108 0.961815182
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ6 (°) U6 (p.u.) δ7 (°) U7 (p.u.) δ8 (°) U8 (p.u.) δ9 (°) U9 (p.u.) δ10 (°) U10 (p.u.)
1BUS 0.410 1 94.58897196 0.972295872 94.51125334 0.971868301 94.42488824 0.974795712 94.31465581 0.977211419 94.12484002 0.978123283
0.411 0 94.77924106 0.954117956 94.70375693 0.954536142 94.61362516 0.957671354 94.51410122 0.952261589 94.33451457 0.947971714
2BUS 0.169 1 95.55292096 0.962245282 95.47497555 0.959441144 95.39775964 0.958754533 95.2967245 0.960566357 95.12690353 0.970588966
0.170 0 103.3095171 0.88109082 103.2085339 0.879340215 103.0839553 0.879275567 97.89209347 0.795840125 95.25021024 0.928024693
3BUS 0.155 1 95.47018166 0.965264823 95.3988683 0.963680475 95.31708048 0.960043928 95.22812941 0.961394008 95.06693926 0.969893173
0.156 0 105.634039 0.913361174 105.5516243 0.9025301 105.4342427 0.889150385 105.264469 0.881717211 93.31246926 0.927812484
4BUS 0.144 1 94.98392762 0.973201764 94.9080898 0.970926942 94.82563258 0.970691159 94.71308068 0.965893783 94.53777855 0.968922304
0.145 0 105.8268355 0.92232027 105.7340101 0.907327001 105.6071671 0.886331099 105.4256159 0.874409845 93.17204604 0.922775862
5BUS 0.128 1 94.00232942 0.992500805 93.92470002 0.989645432 93.84058111 0.986944218 93.72654228 0.976143033 93.54628773 0.97086086
0.129 0 94.20036381 0.973173543 94.13193367 0.972998291 94.05701325 0.970208036 93.9734825 0.966111754 93.82283555 0.965166797
6BUS 0.124 1 93.92826781 0.992369735 93.85186196 0.991731929 93.76457256 0.987084713 93.64887027 0.982844813 93.45341582 0.972683283
0.125 0 95.65910634 0.957254643 95.56042037 0.955578781 95.46098343 0.951118361 95.34350183 0.945809655 95.15941882 0.935662344
7BUS 0.148 1 93.89373903 0.992862219 93.81787571 0.99147987 93.73204894 0.988722604 93.61496323 0.981773913 93.42125823 0.972857001
0.149 0 94.13820919 0.972108976 94.06790908 0.971848091 93.99017277 0.97262992 93.89859153 0.96725942 93.75018536 0.963524413
8BUS 0.146 1 93.92897149 0.993836647 93.85403504 0.99179094 93.76831654 0.986358206 93.65108192 0.983137821 93.4546903 0.972279145
0.147 0 94.79168369 0.95650035 94.70229692 0.956857611 94.60167517 0.950034498 94.46002579 0.949436587 94.29790546 0.948553518
9BUS 0.305 1 94.48438445 0.984754288 94.40056555 0.983783148 94.31180458 0.978517426 94.19481873 0.971449055 93.99298818 0.966232659
0.306 0 94.89276862 0.967781289 94.82059898 0.966952399 94.74695815 0.957083563 94.64727107 0.950980845 94.48254016 0.949593013
10BUS 0.136 1 93.99883525 0.988542709 93.92137581 0.990257546 93.83261457 0.98661036 93.71775434 0.978940815 93.54182877 0.972722829
0.137 0 94.71954893 0.9620201 94.6398427 0.964243018 94.55625657 0.959562469 94.44905057 0.955244708 94.29771996 0.9514295
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ1 (°) U1 (p.u.) δ2 (°) U2 (p.u.) δ3 (°) U3 (p.u.) δ4 (°) U4 (p.u.) δ5 (°) U5 (p.u.)
11BUS 0.137 1 94.39297825 0.976521574 94.24069015 0.976160485 94.1223366 0.992075892 94.03506233 0.987872719 93.95208443 0.990959525
0.138 0 116.2038337 0.775181689 94.75534661 0.954534603 94.62576975 0.966341554 94.53741295 0.969586307 94.4590329 0.974124493
12BUS 0.285 1 94.79704603 0.964415502 94.61552161 0.967584288 94.48506001 0.981840755 94.39871137 0.984355797 94.33038106 0.985486347
0.286 0 115.7537307 0.767055457 94.84804905 0.953396832 94.7024218 0.963960955 94.61761982 0.962234643 94.54997951 0.968173813
13BUS 0.147 1 95.14161021 0.962428056 94.97442425 0.966675047 94.85000053 0.972206482 94.75097414 0.975664063 94.6636762 0.97965037
0.148 0 115.8902599 0.752636832 95.59280453 0.941720435 95.44509413 0.953524448 95.35569179 0.957955082 95.27737599 0.964978996
14BUS
0.151 1 95.84027909 0.956784648 95.68377866 0.95459977 95.58121414 0.965912019 95.49071168 0.969755782 95.41157176 0.970283753
0.152 0 112.1283651 0.737896982 106.5057776 0.858001069 106.3469307 0.895004398 106.2517709 0.905817031 106.1707492 0.913470185
15BUS
0.15 1 95.80391394 0.976902524 95.60953968 0.970209335 95.50060742 0.965883753 95.41186483 0.964411309 95.33853591 0.961790545
0.151 0 116.0065047 0.751527466 111.1451259 0.861091474 110.9963451 0.870727091 110.8879872 0.884035847 110.7964457 0.873218761
16BUS
0.114 1 95.77556855 0.971176967 95.57273209 0.963935062 95.45212322 0.960723103 95.34726145 0.967982909 95.2674853 0.965222154
0.115 0 119.7205834 0.646441209 115.3611523 0.660710515 112.5744789 0.728580545 111.6551848 0.715872344 108.7017029 0.741367276
17BUS
0.13 1 95.77340536 0.973510845 95.58948735 0.966640235 95.47987381 0.965451939 95.39039774 0.967316372 95.3090596 0.966665792
0.131 0 123.5493475 0.674131769 115.2198059 0.790938411 112.152811 0.845266187 112.0231818 0.849906532 111.9040671 0.850024188
18BUS 0.154 1 95.8254409 0.97185966 95.65126882 0.96483996 95.55993959 0.965383203 95.47461509 0.96673025 95.39994378 0.96656084
0.155 0 120.3106286 0.665679725 107.3294936 0.893064573 107.202687 0.901250035 107.108259 0.899117211 107.025826 0.899906662
19BUS 0.129 1 95.22613477 0.961028851 95.01843163 0.964292744 94.87579602 0.973182194 94.77289721 0.979713093 94.69476717 0.980383243
0.13 0 108.5072056 0.809818406 95.17021439 0.950055172 95.01400819 0.962665232 94.90962203 0.962988556 94.81742606 0.977463358
20BUS
0.151 1 95.26215533 0.9625008 95.05199184 0.967287446 94.9367082 0.971256797 94.84735126 0.976987431 94.76783563 0.979706692
0.152 0 132.8093106 0.567889105 111.8978958 0.681239325 109.9364109 0.735196867 109.2970568 0.735997691 109.1125995 0.737416897
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ6 (°) U6 (p.u.) δ7 (°) U7 (p.u.) δ8 (°) U8 (p.u.) δ9 (°) U9 (p.u.) δ10 (°) U10 (p.u.)
11BUS 0.137 1 93.8787395 0.990168641 93.80049044 0.992279335 93.71374446 0.985886062 93.59723121 0.983066502 93.42238086 0.977152139
0.138 0 94.38692128 0.974832024 94.30865135 0.970655982 94.22355351 0.967205057 94.12982433 0.964944553 93.98956338 0.95541089
12BUS 0.285 1 94.26544891 0.985303313 94.19216456 0.985162594 94.10972554 0.978638581 93.9861976 0.976276737 93.78756131 0.965482834
0.286 0 94.48794463 0.970924388 94.4230196 0.967004453 94.34625082 0.962531694 94.25192127 0.959071699 94.09294401 0.956754433
13BUS 0.147 1 94.58305747 0.979242454 94.49926693 0.976933368 94.40217157 0.973155827 94.28564351 0.971089635 94.10477482 0.969173138
0.148 0 95.20530796 0.960095317 95.13468721 0.962301634 95.04738198 0.955750775 94.95330968 0.945173588 94.78857197 0.946637461
14BUS 0.151 1 95.33804343 0.970074863 95.26559295 0.969533783 95.16942407 0.964822079 95.07633987 0.958568451 94.90739313 0.961662564
0.152 0 106.0912031 0.915871739 105.9989988 0.906138881 105.8977411 0.892013703 105.7257801 0.871913938 93.32689163 0.92308922
15BUS 0.15 1 95.27187963 0.961101179 95.20210686 0.965217886 95.12117672 0.966637241 95.00454523 0.971750685 94.80301651 0.984451659
0.151 0 110.7086025 0.867204778 110.6062907 0.876881364 110.4894933 0.873925112 110.318508 0.872769955 92.81647305 0.92150951
16BUS 0.114 1 95.18903562 0.962312244 95.1134542 0.964592944 95.01343122 0.962635202 94.88461145 0.969606862 94.67842721 0.982270965
0.115 0 108.0071161 0.821266077 107.8928651 0.81685912 107.7612071 0.813505687 106.5827932 0.782672584 94.78379451 0.919132629
17BUS 0.13 1 95.24201104 0.965654218 95.16714294 0.965292884 95.07679965 0.964502204 94.96508215 0.969626367 94.77086494 0.983478726
0.131 0 111.804953 0.850457711 111.7007481 0.853125092 111.5829741 0.853590995 111.4447301 0.853934638 92.03966964 0.922414548
18BUS 0.154 1 95.3309761 0.966505917 95.2544011 0.964055527 95.17570345 0.964709475 95.07576665 0.964711939 94.89580971 0.978851279
0.155 0 106.9540967 0.90576905 106.8749795 0.903488291 106.7840003 0.905033853 106.6578714 0.894109445 92.98320026 0.924357656
19BUS 0.129 1 94.62325432 0.983365017 94.54341707 0.977106632 94.43733677 0.971706532 94.29655792 0.970893898 94.07986622 0.972007076
0.13 0 94.74106263 0.974065037 94.66122043 0.971051229 94.55993025 0.965085347 94.4239523 0.962860325 94.22231491 0.959947741
20BUS 0.151 1 94.69985366 0.978241399 94.61921006 0.973334478 94.52754084 0.970361584 94.40749349 0.975976547 94.18920033 0.972822379
0.152 0 107.4999575 0.83100965 107.3405165 0.821181149 107.178335 0.82972905 99.50670949 0.760628566 95.19966297 0.912921279
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ1 (°) U1 (p.u.) δ2 (°) U2 (p.u.) δ3 (°) U3 (p.u.) δ4 (°) U4 (p.u.) δ5 (°) U5 (p.u.)
21BUS 0.138 1 95.86925125 0.954335852 95.63852619 0.951556197 95.48940498 0.954757491 95.37744846 0.962131899 95.28555129 0.962494388
0.139 0 99.52239075 0.859408001 99.23606534 0.852861649 98.38964572 0.893207226 97.51808977 0.909902999 97.40840624 0.916455312
22BUS 0.129 1 95.31264584 0.970634608 95.05602724 0.96350946 94.91261868 0.968278761 94.81792111 0.969660645 94.73217752 0.974536597
0.130 0 119.5374327 0.716091229 108.265515 0.883086707 108.0997164 0.8922798 107.9828514 0.87914 107.8929075 0.876665867
23BUS 0.144 1 96.26891636 0.946089065 96.06009329 0.945849025 95.89098892 0.946768421 95.77479287 0.954263703 95.68794011 0.959713083
0.145 0 111.957676 0.783399045 96.56158609 0.936368271 96.40203425 0.939091479 96.278055 0.937704288 96.18659336 0.946762379
24BUS 0.135 1 95.91217872 0.971651424 95.70751385 0.96443052 95.59172207 0.957493363 95.48583266 0.961542454 95.40372946 0.962134808
0.136 0 119.8954622 0.701722629 105.9143963 0.800277631 104.6725155 0.865817086 104.5262518 0.874019575 104.4286197 0.876853848
25BUS 0.159 1 96.02587579 0.962654493 95.70324743 0.967612919 95.53968201 0.965132954 95.44932754 0.961267271 95.37760176 0.955787256
0.16 0 133.3412024 0.693013903 113.7846351 0.839787271 113.6981061 0.868059675 113.6495475 0.882103523 113.593138 0.912946692
26BUS 0.119 1 94.64078926 0.979718821 94.46951484 0.976854143 94.37479489 0.976644748 94.28812295 0.97385059 94.20371586 0.974373923
0.12 0 133.9743585 0.702262579 93.83045786 0.967168856 93.71703003 0.964651349 93.634102 0.954474103 93.58027514 0.952556402
27BUS 0.15 1 94.64078926 0.979718821 94.46951484 0.976854143 94.37479489 0.976644748 94.28812295 0.97385059 94.20371586 0.974373923
0.151 0 120.6452889 0.711985682 119.6205942 0.697735852 108.314783 0.835208306 108.1842291 0.856605282 108.074389 0.875480965
28BUS 0.12 1 93.70982682 1.013354868 93.70790084 1.015115552 93.70810549 0.944737386 93.70762744 0.948885287 93.70417222 0.968854208
0.121 0 135.3150783 0.701496427 93.64768174 0.962285457 93.49341869 0.958625572 93.4140093 0.950331284 93.34209711 0.947862824
29BUS 0.103 1 94.21689878 0.977826032 94.00598487 0.984383213 93.92974447 0.981454033 93.85065056 0.985910435 93.78009398 0.984891019
0.104 0 135.0731176 0.706603598 93.53803956 0.964498131 93.41400656 0.961247461 93.34709548 0.952619885 93.27525088 0.949690405
30BUS 0.286 1 95.32889648 0.966875467 95.14444735 0.975102274 95.03974705 0.966391289 94.94019077 0.965485962 94.8612708 0.969697576
0.287 0 129.2217328 0.582331669 125.6196868 0.594226492 113.3676557 0.868058741 113.2476765 0.874023458 113.1605724 0.87239901
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ6 (°) U6 (p.u.) δ7 (°) U7 (p.u.) δ8 (°) U8 (p.u.) δ9 (°) U9 (p.u.) δ10 (°) U10 (p.u.)
21BUS 0.138 1 95.19467421 0.960057081 95.10621633 0.959057511 95.01119537 0.958072144 94.85614387 0.957733478 94.57548054 0.965947546
0.139 0 97.31461471 0.920061004 97.21738441 0.918142789 97.09801703 0.915122849 96.92916067 0.91549989 95.03232631 0.952937741
22BUS 0.129 1 94.65235025 0.975154638 94.57057 0.969619585 94.47772576 0.968562189 94.33865891 0.968860195 94.05953856 0.974793213
0.130 0 107.7974987 0.877233818 107.7082762 0.88288952 107.5829084 0.889768656 107.4285448 0.893455062 92.88329878 0.927568436
23BUS 0.144 1 95.61073536 0.957764138 95.52253657 0.952081834 95.40443159 0.946991929 95.24500295 0.95168074 95.00533082 0.959777026
0.145 0 96.0934173 0.940408736 96.00838738 0.94281942 95.90426519 0.942688751 95.76802895 0.945136127 95.57429465 0.947873563
24BUS 0.135 1 95.32098884 0.960877336 95.24019294 0.961680485 95.14082104 0.960398861 95.00227761 0.965458131 94.79439156 0.978541034
0.136 0 104.3304082 0.867972264 104.2348118 0.875017611 104.1184124 0.87397991 103.9412118 0.868476652 94.84326042 0.92468064
25BUS 0.159 1 95.31563877 0.956525212 95.24168801 0.956074993 95.14139612 0.963841364 94.97932759 0.972905427 94.65146029 0.965928151
0.16 0 113.5527275 0.912662219 113.5009234 0.886053948 113.4525847 0.869711039 113.3636729 0.849122059 90.18551593 0.90635071
26BUS 0.119 1 94.12049594 0.972515877 94.04409414 0.974958696 93.95519675 0.979695682 93.86849268 0.983415177 93.68362091 0.986510065
0.12 0 93.53595878 0.952735107 93.49196777 0.95127026 93.4459171 0.952760285 93.37848586 0.964990895 93.22490332 0.971507106
27BUS 0.15 1 94.12049594 0.972515877 94.04409414 0.974958696 93.95519675 0.979695682 93.86849268 0.983415177 93.68362091 0.986510065
0.151 0 107.99803 0.879247481 107.9211172 0.880154848 107.8122234 0.859097786 107.6684962 0.840527801 93.17638293 0.921128286
28BUS 0.12 1 93.70637581 0.965314003 93.70727271 1.018336492 93.70700459 1.035278096 93.70518428 0.938892924 93.70737889 0.994130695
0.121 0 93.2937229 0.947159785 93.2499328 0.94575947 93.1878376 0.9507095 93.11040833 0.959872069 92.94701032 0.96483946
29BUS 0.103 1 93.72411291 0.984947341 93.65416714 0.98318043 93.58434117 0.980572759 93.50900284 0.986938491 93.28827153 0.985385632
0.104 0 93.22568816 0.951203443 93.17591941 0.948545722 93.10966834 0.953378356 93.0442657 0.959869975 92.91050319 0.968643993
30BUS 0.286 1 94.78749482 0.971889065 94.712031 0.966645687 94.61212148 0.973325842 94.50209129 0.975328456 94.31284691 0.975748446
0.287 0 113.0783706 0.872929675 112.9886077 0.868893958 112.883801 0.878444108 112.7668396 0.882022069 91.47404051 0.915203353
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ1 (°) U1 (p.u.) δ2 (°) U2 (p.u.) δ3 (°) U3 (p.u.) δ4 (°) U4 (p.u.) δ5 (°) U5 (p.u.)
31BUS 0.145 1 96.00646358 0.925662494 95.71446695 0.962222649 95.58292152 0.971792274 95.50834347 0.976985212 95.44524986 0.980330825
0.146 0 135.3337864 0.580943773 101.9518056 0.883271559 101.7757573 0.905465022 101.692181 0.905670925 101.6216516 0.915194068
32BUS 0.176 1 96.13122329 0.925948256 95.87235659 0.959079245 95.72946277 0.973537906 95.630327 0.974917441 95.5450373 0.981658171
0.177 0 105.5706819 0.791003618 96.46740327 0.938634198 96.33506578 0.965076827 96.2467396 0.962364038 96.16354044 0.964753733
33BUS 0.131 1 94.03647594 0.95428025 93.75268679 0.98568092 93.61904957 0.986931149 93.542537 0.984132154 93.47875945 0.981674278
0.132 0 96.3778254 0.899047921 94.36998905 0.966016737 94.21127419 0.979774323 94.13291233 0.97888059 94.06895094 0.976575827
34BUS 0.151 1 94.90617558 0.966874703 94.73046735 0.974074298 94.61662852 0.981411959 94.53076125 0.981708921 94.45707998 0.980959225
0.152 0 133.2007362 0.616571634 101.7717008 0.817471419 99.50193077 0.879410295 99.23682192 0.864908146 99.12078398 0.864997041
35BUS 0.145 1 96.55399649 0.938827486 96.19414687 0.944042454 96.01640433 0.952363418 95.90417777 0.959620685 95.8101293 0.960553003
0.146 0 119.0814082 0.664094473 109.4932682 0.865759665 109.2449151 0.855376302 109.1088331 0.838457706 108.9821996 0.841057356
36BUS 0.208 1 96.90247289 0.950480115 96.64618552 0.953233953 96.49896917 0.951387726 96.38257486 0.952074383 96.29514717 0.959536582
0.209 0 110.4420713 0.755853593 103.5047922 0.890433763 103.3071599 0.892079665 103.1825654 0.900228841 103.0813206 0.902691719
37BUS 0.168 1 94.94222696 0.957256982 94.51017388 0.969743103 94.367579 0.971234788 94.27570747 0.96906911 94.20711836 0.972812384
0.169 0 113.4007788 0.795416732 95.12970501 0.936361469 94.83890772 0.947233778 94.72514878 0.944992174 94.65372992 0.946502879
38BUS 0.099 1 94.0809412 0.975871809 93.86366815 0.987930455 93.7901087 0.985365507 93.71685134 0.987561439 93.64328531 0.986885182
0.1 0 134.2038708 0.704318366 93.47052963 0.968585117 93.36713812 0.960824913 93.3206924 0.966727246 93.25213146 0.960475752
39BUS 0.338 1 95.69609323 0.958127471 95.51500602 0.959037831 95.4053055 0.974222799 95.3218433 0.981492804 95.25325365 0.983042659
0.339 0 117.5649081 0.761814728 113.3547282 0.74132912 109.9341294 0.829295872 109.8147867 0.851616627 109.7236082 0.86253913
Table S1. Validity of the stability boundary. (meta-generators in the 10-gen)(Continued)
BUS No. ∆t (s) stability δ6 (°) U6 (p.u.) δ7 (°) U7 (p.u.) δ8 (°) U8 (p.u.) δ9 (°) U9 (p.u.) δ10 (°) U10 (p.u.)
31BUS 0.145 1 95.3753097 0.980331999 95.31678107 0.980092309 95.23974678 0.968696982 95.11213571 0.96098943 94.80760875 0.932295747
0.146 0 101.56803 0.913795372 101.4902257 0.910249225 101.420495 0.907956912 101.2952403 0.897084388 95.53276768 0.911107971
32BUS 0.176 1 95.46300513 0.976945767 95.37216461 0.976084253 95.26865262 0.971636372 95.12044564 0.960917591 94.8589611 0.93710973
0.177 0 96.08614904 0.965812694 95.99917308 0.965296887 95.91409888 0.967375697 95.80326828 0.960803388 95.57587023 0.914188021
33BUS 0.131 1 93.41967686 0.982232939 93.35505186 0.982744208 93.2852666 0.989036477 93.14685969 0.989170865 92.85986639 0.9686506
0.132 0 94.00958109 0.978122294 93.94573978 0.976723358 93.87622621 0.977638666 93.74672096 0.982446887 93.41794104 0.957841954
34BUS 0.151 1 94.39143485 0.980285452 94.31289061 0.981443568 94.22624048 0.97789006 94.10969186 0.976598031 93.93050555 0.980136262
0.152 0 99.00036677 0.869167371 98.87520315 0.877421974 98.60491523 0.87211062 98.47785939 0.87496015 93.4289497 0.950283633
35BUS 0.145 1 95.72188876 0.958536902 95.63169523 0.961640525 95.52223313 0.956358826 95.35607991 0.947104293 94.9648387 0.9515796
0.146 0 108.8562397 0.841849815 108.741715 0.852498996 108.6070548 0.853536302 108.3562813 0.874876892 94.20755501 0.917552779
36BUS 0.208 1 96.21095426 0.95768021 96.11438719 0.954354233 95.99159726 0.955035992 95.83686503 0.956071659 95.58364697 0.960663163
0.209 0 102.9909169 0.898958651 102.8964269 0.897294653 102.7649712 0.896895692 102.5758144 0.897864088 95.3762545 0.921149995
37BUS 0.168 1 94.14643545 0.969596642 94.08414703 0.969790985 93.99671423 0.967111769 93.84367713 0.975457796 93.39777497 0.969109835
0.169 0 94.59783484 0.943873523 94.53490787 0.939311569 94.44639645 0.944852404 94.29953664 0.954335412 93.88563734 0.939982454
38BUS 0.099 1 93.58723994 0.989131664 93.51493365 0.988248001 93.44561152 0.982965027 93.3765968 0.988985527 93.14700785 0.983263153
0.1 0 93.21970513 0.957895262 93.18166187 0.96001971 93.13643951 0.957871124 93.07055057 0.964490795 92.93527414 0.972985892
39BUS 0.338 1 95.17705777 0.98204963 95.10556515 0.975484338 95.01362922 0.973099235 94.89905437 0.966554968 94.72607143 0.94710906
0.339 0 109.611875 0.849164168 109.5272771 0.86071952 109.4078691 0.840488246 109.2388728 0.831913218 93.38489471 0.903792194
The system has a total of 39 nodes (New England test system). Stability calculations have been performed at each node where a large disturbance fault occurred, one by one. The results of the calculations record the state points of each meta-generator when the system is stable or unstable. “BUS No.” indicates the number of the nodes where the failure occurred. Δ t represents the fault clearing time and d ( Δ t ) = 0.001   s . “1” indicates that the system is synchronously stable, and “0” indicates that the system is out of synchronization. When the system is stable, the results in Table S1 reveal that ω K ω L < < ω L ω K is true. Where u i and δ i are calculated via Eq. (S3). Substituting these data into Eq. (1) yields a visualization similar to that in Figure 2(b). These results indicate that Eq. (1) can well discriminate the synchronization stability of the power system well. The stability boundary discriminates the 39 pairs of cases with an accuracy of 100%. These results validate Eq. (1), and after transformation, also validate Eq. (C5). Considering space limitations, these results are presented in Table S1.

Data Availability Statement

All raw data for this article are publicly available at https://doi.org/10.57760/sciencedb.24825.

Conflicts of Interest

The author declare no conflicts of interest.

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Figure 1. Validity of the stability boundary (meta-generators in the 10-gen).
Figure 1. Validity of the stability boundary (meta-generators in the 10-gen).
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Figure 2. Validation of the network-independent synchronization stability boundary on a completely different system. (meta-generators in the 3-gen).
Figure 2. Validation of the network-independent synchronization stability boundary on a completely different system. (meta-generators in the 3-gen).
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Figure 3. Emergence of self-organization near the stability boundary. (meta-generators in the 10-gen).
Figure 3. Emergence of self-organization near the stability boundary. (meta-generators in the 10-gen).
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