1. Introduction
The resilience of power distribution networks plays a critical role in maintaining societal stability, economic productivity, and public safety [
1,
2,
3]. In modern society, where electricity supports nearly all aspects of urban life, rapid restoration of power after extreme events is vital [
4,
5]. Among the various types of natural disasters, earthquake events have been shown to pose some of the most severe threats to distribution networks due to their sudden onset, large spatial footprint, and simultaneous impact on multiple infrastructure components [
6,
7].
In recent years, several earthquake events have demonstrated the fragility of power distribution systems. The 2011 earthquake in eastern Japan [
8], the 2020 Zagreb earthquake in Croatia [
9], and the 2023 Turkey–Syria earthquake [
10] underscore the severe consequences of earthquakes and highlight the need for effective restoration methods after an earthquake disaster.
A major challenge posed by extreme earthquakes is the potential loss of connection to the upstream transmission network, leading to the formation of outage distribution islands. In such scenarios, the restoration process cannot rely on external power sources and must use local resources with black-start capability. These resources must be coordinated to sequentially restart generators and loads under significant operational and topological constraints. It becomes essential to optimize the recovery strategy after an earthquake in a way that leverages internal generators, respects operational constraints, and prioritizes critical loads.
Recently, several studies have contributed to the understanding of post-disaster distribution system restoration [
11,
12,
13]. In terms of earthquake failure modeling, some researchers proposed fragility-based probabilistic approaches to estimate component failure under peak ground acceleration (PGA), enabling realistic scenario generation [
14,
15]. Others developed earthquake integration models to simulate geographically correlated damage patterns across urban grids [
16]. Monte Carlo simulation has also been employed to construct degraded topologies for resilience evaluation and planning, improving the resilience and supplying the essential loads during and after the earthquake [
17].
In the studies of generator start-up, early studies formulated black-start scheduling problems for microgrids with simplified connectivity assumptions [
18,
19,
20]. An optimization-based framework for black-start resource allocation aimed at improving the efficiency of system restoration following a blackout [
21]. Their model considered the interdependence between black-start and non-black-start generators, and formulated a MILP to determine the optimal allocation of black-start capabilities under various system constraints. However, the study primarily focused on high-voltage transmission networks and did not account for the topological degradation or resource limitations commonly observed in distribution networks following natural disasters such as earthquakes. Recent efforts have begun to address generator start-up in distribution systems. For example, a parallel black-start strategy for microgrids, considering the characteristics of distributed generators and proposing a sequencing method for restoration, is developed in [
22]. Nevertheless, their method assumes a structurally intact system and does not consider the probabilistic damage patterns caused by natural disasters such as earthquakes. As a result, their model cannot be directly applied to post-earthquake scenarios where critical paths may be unavailable or uncertain. In addition, a coordinated recovery framework involving black-start and non-black-start generators is proposed in [
23], utilizing a deterministic optimization approach. While this work introduces cranking power constraints and generator dependencies, it lacks stochastic modeling of disaster impact and does not incorporate realistic restoration delays caused by infrastructure fragmentation.
Load restoration has also been extensively studied under normal outage scenarios [
24,
25,
26,
27]. A multi-step reconfiguration model is proposed for active distribution networks that integrates the start-up sequence of distributed generators while maximizing restored loads under power flow constraints [
28]. However, its formulation does not consider the probabilistic failures induced by disasters, limiting its applicability in post-earthquake scenarios where system topology and supply capacity may be severely compromised. A microgrid-based framework for critical load service restoration is developed in [
27], where optimization aims to re-energize high-priority loads while respecting network operational constraints. While effective under controlled microgrid settings, their work does not model the stochastic degradation of network elements, nor does it support system-wide recovery strategies in damaged distribution systems. Moreover, a two-stage restoration method for distribution networks is introduced in [
26], combining component repair decisions with load restoration scheduling. Though the model accounts for time-based restoration dynamics, it is not specifically designed for earthquake-induced damage. More advanced approaches incorporated second-order cone relaxations to improve solution feasibility for power flow, though they often did not consider earthquake scenarios with probabilistic degradation and local generator start-up constraints [
29].
Despite these advancements having contributed significantly to either generator start-up scheduling or load restoration modeling, they often treat these processes independently, assuming one stage is complete before the other begins. However, the operational states of generators and the topology of the distribution system evolve dynamically and interdependently under earthquake damage. In reality, generator start-up directly influences the available supply capacity and network energization status, which in turn determines the feasibility and sequence of load restoration. Separating the two stages may lead to suboptimal recovery paths. For instance, neglecting the spatial and temporal coupling between generator energization and load pickup can result in infeasible load schedules or delayed service to critical infrastructure. Moreover, some loads may be essential not only from a consumer standpoint but also for supporting black-start operations and local grid stability.
Therefore, this paper proposes a two-stage restoration method for distribution networks after an earthquake. The approach explicitly accounts for stochastic damage modeling, generator start-up, and critical load restoration.
To summarize, our contributions are listed as follows:
A fragility curve failure modeling approach is integrated with earthquake ground motion prediction to generate degraded distribution topologies through Monte Carlo simulation.
A time-domain generator start-up model is developed based on MILP, incorporating segmented start-up curves, cranking power dependencies, and radial connectivity constraint.
A load recovery model is formulated as a MISOCP, maximizing weighted load restoration, and taking power flow constraints, voltage and current limits, and radial constraints into account.
The rest of the paper is organized as follows:
Section 2 describes the modeling of earthquake-induced damage, including PGA estimation, fragility analysis, and degraded topology generation using Monte Carlo simulation.
Section 3 presents the two-stage restoration method, covering the MILP-based generator start-up model and the MISOCP-based load recovery model.
Section 4 introduces the overall solution process.
Section 5 provides case studies to verify the effectiveness of the proposed method.
Section 6 concludes the paper.
2. Distribution Network Degradation After Earthquake Disaster
2.1. Earthquake Model Based on GMPE
To accurately assess the impact of earthquakes on distribution networks, it is essential to quantify the seismic intensity at different geographical locations within the network. This is typically achieved by estimating the PGA, which reflects the maximum ground acceleration experienced during the shaking phase of an earthquake. The spatial distribution of PGA serves as a fundamental input to the fragility analysis of distribution components and provides the basis for post-earthquake restoration planning.
The estimation of PGA values is conducted using GMPEs, which are widely recognized empirical models that relate earthquake characteristics and site-specific conditions to expected ground motion intensity. GMPEs enable the conversion of seismic source parameters—such as earthquake magnitude and epicentral distance—into quantitative estimates of PGA. These equations also incorporate the effects of local geological features that can amplify or attenuate seismic waves, thus allowing for site-specific disaster evaluation.
A commonly used functional form of the GMPE is expressed as follows:
In this equation, PGA denotes the peak ground acceleration at a specific site, measured in either or . The variable represents the earthquake magnitude, while denotes the rupture distance from the fault to the site. c1 is a constant term; it is used to set the benchmark level of the model and plays an overall offset adjustment role in the intensity of ground motion. c2 reflects the influence of the earthquake magnitude on ground motion, c3 controls the attenuation rate with distance, c4 adjusts the near-field distance effect, and c5 captures the interaction between magnitude and distance attenuation. The term is a site amplification factor that accounts for local soil conditions, including shear-wave velocity and soil layering effects.
This GMPE formulation captures the combined influence of the seismic source characteristics, wave propagation path, and local site effects on the resulting ground motion. Specifically, the logarithmic attenuation term accounts for energy loss over distance, while the exponential magnitude term reflects nonlinear source scaling. The site amplification term ensures that nodes located on soft soils or near-surface sediments receive appropriately adjusted PGA values, which can significantly differ from those on bedrock.
In this study, the GMPE is applied to each node in the distribution network to compute its expected PGA. For each node, its spatial coordinates are used to determine the rupture distance from the earthquake epicenter. Given the assumed magnitude and known site classification, the PGA value at each node is calculated accordingly. The result is a spatially continuous PGA field over the entire network, which captures the variation in seismic intensity due to geography.
This PGA serves as the primary input to the fragility damage model described in the following section. It allows for quantification of failure probabilities and facilitates the construction of realistic degraded topologies that are essential for post-earthquake restoration optimization. By integrating GMPE into the resilience framework, the proposed method ensures that the earthquake impact is consistently and accurately propagated through all stages of the restoration decision process.
2.2. Fragility Curve Probability Model
Following the establishment of the spatial PGA distribution across the distribution network, it becomes necessary to translate ground motion intensity into the likelihood of component failure. This is achieved through the use of fragility functions, which express the probability that a structural or electrical component will exceed a specific damage threshold when subjected to a given level of seismic demand. Fragility modeling plays a central role in probabilistic disaster impact analysis and provides the mathematical linkage between earthquake intensity and physical system vulnerability.
A fragility function is commonly represented by a cumulative lognormal distribution, formulated as follows:
In this equation, denotes the probability of failure for a given component under seismic excitation. The term is the cumulative distribution function of the standard normal distribution, which transforms the logarithmic ground motion ratio into a probability value ranging from 0 to 1. The variable θ is the median PGA value at which the component reaches the specified damage state, often derived from historical testing or empirical assessments. The parameter β is the standard deviation in natural log space, capturing the uncertainty in seismic response due to material variability, installation quality, and modeling assumptions.
This mathematical formulation implies that as PGA increases, the failure probability rises in a nonlinear, probabilistic manner. Different types of components—such as overhead lines, underground cables, transformers, and switches—have distinct fragility parameters based on their structural robustness and installation environment. For instance, overhead lines typically exhibit higher fragility at lower PGA thresholds due to their exposure and mechanical flexibility, while underground cables and transformers often have higher median capacities before failure is probable.
To apply the fragility function across the network, the node-specific PGA values calculated in
Section 2.1 are used as inputs. For each component
i, its geographic location determines the PGA value
, which is then substituted into the fragility function to compute its individual failure probability
. This approach allows for spatially differentiated risk modeling, wherein components located nearer to the earthquake epicenter or situated on soft soil are more likely to fail, while those farther away or on firmer ground have lower risk levels.
The resulting set of failure probabilities forms a probabilistic damage profile for the entire distribution system. The model recognizes disaster uncertainty and enables scenario generation through stochastic sampling. This probabilistic profile will be used in the following section to produce post-disaster degraded network topologies using Monte Carlo simulation techniques. By incorporating the fragility model, the proposed framework ensures that earthquake infrastructure vulnerability is quantitatively and realistically embedded into the restoration planning process.
2.3. Monte Carlo Simulation of Post-Disaster Network Degradation
Given the probabilistic nature of infrastructure failure under an earthquake, a deterministic damage assessment cannot sufficiently capture the diversity of potential outcomes. Instead, a scenario-based approach is required to account for the inherent uncertainty in the spatial and structural response of distribution networks. To this end, Monte Carlo simulation is employed to generate multiple realizations of network degradation caused by earthquake-induced component failures.
The Monte Carlo method is a statistical technique that approximates the behavior of a complex stochastic system through repeated random sampling. In this context, the distribution system is considered as a set of components
, where each component
is assigned a failure probability
, computed based on the PGA field and the fragility model described in
Section 2.2. For each simulation trial
, a uniformly distributed random variable
is drawn for every component. If
, the component is deemed to have failed in that trial.
The operational status
of component
in trial
is defined as follows:
This stochastic sampling procedure is repeated for trials, producing distinct post-earthquake failure scenarios. Each scenario captures a unique and feasible manifestation of the impact of an earthquake on the distribution infrastructure.
From each sampled set of component states, a degraded network topology is constructed, denoted by . Here, represents the subset of network nodes that remain accessible or energizable, while denotes the set of branches or lines that remain physically and electrically intact. Nodes that lose all adjacent connectivity due to failed branches are excluded from , while failed branches are similarly excluded from . Each degraded topology reflects the real-world possibility of network fragmentation and isolation caused by earthquake-induced component damage.
The collection of degraded topologies
forms a representative scenario set that serves as the basis for subsequent restoration modeling. In particular, each degraded network is used as the input to the two-stage restoration strategy, where the feasible structure of the post-earthquake system constrains both the black-start optimization and load recovery scheduling processes. This approach enables robust evaluation and design of restoration strategies under uncertainty, ensuring critical loads can be recovered even in adverse and low-probability damage scenarios. The diagram of fault scenario generation is shown in
Figure 1.
By combining fragility-informed failure probabilities with Monte Carlo scenario generation, this modeling framework captures the full spectrum of structural outcomes resulting from an earthquake. It provides a physically realistic and statistically grounded foundation for resilience-aware restoration planning in distribution networks.
5. Case Study
To validate the effectiveness of the proposed two-stage restoration method, a modified IEEE 33-bus distribution network is adopted as the test system. The topology of the network under normal operation is shown in
Figure 4.
All numerical experiments in this paper are conducted using the YALMIP toolbox in MATLAB for model formulation. YALMIP provides a high-level modeling interface for mixed-integer and convex optimization problems, which is well-suited for implementing the MILP and MISOCP models proposed in this study. The optimization problems are solved using the Gurobi solver, which offers efficient algorithms for large-scale linear and second-order cone programming tasks.
The simulation environment is set up on a PC with the following configuration: an Intel Core i7-12700, 32 GB of RAM, and the Windows 11 operating system. All models are implemented and executed in MATLAB R2022b. The Gurobi Optimizer version 11.0.0 is integrated with YALMIP as the solver.
In this test case, a total of seven distributed generators (DGs) are integrated into the network. Among them, the generator located at node 1 is designated as the black-start generator, possessing black-start capability without external power support. The remaining six generators are modeled as non-black-start generators, which require cranking power support from the black-start generator during the restoration process. The dashed lines represent sectionalizing switches. These switches are used by distribution system operators to flexibly reconfigure the network in the event of faults or during system restoration. During the restoration, operators are allowed to selectively close or open these switches to implement optimal restoration strategies or fault isolation. After the earthquake, the distribution network dispatchers adjusted the weights of the loads related to post-earthquake reconstruction. The purple squares and orange triangles represent first-level and second-level loads; in this paper, the weights of first-level loads and second-level loads are set to 100 and 1, respectively. The parameters of generators, loads, and branches are shown in
Table A1,
Table A2 and
Table A3.
and
are set as 0.85 and 1.05,
is set as 1.05,
β and ln(
θ) are set as 0.44 and 0.45 g, and
c1 to
c5 are set as −1.474, 0.718, −1.054, 0.00115, and 0.00035, according to [
30].
The restoration process is divided into 30 time intervals. All numerical simulations are implemented in MATLAB. The optimization models are constructed using the CVX, and Gurobi is adopted as the solver to compute the optimal solutions of the MILP and MISOCP, as presented in
Section 3.1 and
Section 3.2.
In this paper, an earthquake with an average PGA of 0.5 g was modeled across the region where the distribution network is located. The ranges of
and
are 4.2~8.0 and 2~80 km, and the PGA values and failure probabilities of buses and branches are shown in
Table 1 and
Table 2.
The fragility curve of distribution devices under the earthquake is shown in
Figure 5 [
31]. The horizontal axis represents the PGA, while the vertical axis indicates the corresponding failure probability of components such as poles, overhead lines, and transformers. The curve follows a typical lognormal cumulative distribution form, reflecting the probabilistic nature of infrastructure failure under an earthquake.
As shown, the failure probability remains below 0.1 when PGA is less than 0.2 g, indicating high survivability of most equipment under weak shaking conditions. However, as the PGA increases beyond 0.4 g, the failure probability grows significantly. At PGA ≈ 0.6 g, the failure probability reaches approximately 0.5, suggesting that half of the components subjected to such ground motion are likely to fail. For PGA values exceeding 1.0 g, the failure probability asymptotically approaches 1.0, indicating that component failure becomes certain in severe earthquakes.
This curve provides a quantitative basis for mapping ground motion intensity to physical failure likelihood across the distribution network. When combined with nodal PGA values obtained from GMPE models, this fragility function enables the Monte Carlo simulation process to accurately generate degraded network topologies. These topologies serve as essential inputs to the proposed two-stage restoration models developed in
Section 3.1 and
Section 3.2.
Subsequently, 1000 Monte Carlo trials were generated. In each trial, device states were sampled based on
, producing a degraded topology of the distribution grid. On average, approximately 40–45% of the branches and 15–20% of the switches were found to be non-operational after a major earthquake. A representative degraded topology after an earthquake is shown in
Figure 6; the lines and generators in red, such as line 23–24, line 6–7, and G25, represent devices destroyed by the earthquake which will not recover during restoration.
Solving the generator start-up MILP model, the start-up time of each generator is shown in
Table 3. During the restoration process, the black-start generator G1 is activated at
t = 1, and ramps up quickly due to its characteristics. Then, G1 begins to energize adjacent transmission paths to support the restart of non-black-start generators. In order to deliver the required cranking power to downstream generators, sectionalizing switches between nodes 8 and 21, 9 and 15, and 18 and 33 are closed, thereby enabling flexible power routing through alternative paths.
Figure 7 shows the progress of generator start-up; at
t = 4, node 4 becomes energized via the transmission path 1–2–3–4, allowing the non-black-start generator G4 to initiate its start-up process. G4 receives cranking power from G1 and transitions into a self-sustained operating state. However, due to the permanent failure of line 28–29 caused by the earthquake, generators G29 and G33 must delay their restart until alternative transmission paths are established. With the aid of the sectionalizing switch at node pair 18–33, G33 is able to begin its start-up sequence after 12 time intervals and becomes fully operational at
t = 18, while G29 requires a longer delay of 16 time intervals and completes its start-up at
t = 22. It is important to note that generator G25 suffers irreparable damage during the earthquake and remains out of service throughout the entire restoration period. The transmission path of each generator is shown in
Figure 8.
Figure 9 shows the total active power output of all generators in the system over the restoration timeline. This curve reflects the cumulative generation capability of the distribution network as black-start and non-black-start generators are sequentially re-energized. The horizontal axis represents the time interval since the onset of restoration, while the vertical axis indicates the total active power available in the system at each step.
At the initial stage (t = 1), only the black-start generator G1 is restarted, providing limited generation capacity to support cranking power requirements for downstream generators. During the early phase (t = 1 to t = 5), the curve rises gradually, corresponding to the start-up of a small number of nearby non-black-start generators with minimal cranking delays and simple transmission paths. This phase marks the progressive energization of nodes located within a short electrical distance from G1.
Between t = 6 and t = 16, the slope of the generation curve increases significantly. This inflection corresponds to the activation of several mid-distance generators such as G4, G15, and G21, whose start-up becomes feasible once critical transmission paths are restored. The closing of key sectionalizing switches facilitates these power routes and enables multiple units to restart in parallel.
After t = 16, the generation capacity continues to rise but at a slower rate, approaching its maximum value. This stage involves the recovery of distant generators (G29 and G33), which require longer delays due to either broken transmission lines or limited cranking power availability. The final plateau of the curve indicates that all available generators, excluding permanently damaged units (G25), have completed their start-up procedures.
Solving the load recovery MISOCP model,
Figure 10 shows the restoration result of the loads. According to the result of the generator capability curve, the total generation capacity of the system reaches 798 kW at time interval
t = 30. At this stage, all available generators supply power to critical loads to ensure power supply.
First-level loads are located at nodes 9, 20, 26, and 31, with load demands of 60 kW, 90 kW, 60 kW, and 150 kW, respectively. Second-level loads are assigned to nodes 5, 7, 13, 17, 23, and 28, with demands of 60 kW, 200 kW, 60 kW, 60 kW, 90 kW, and 60 kW, respectively. The restoration results in
Table 4 show that all first-level loads are restored, totaling 360 kW. After satisfying all first-level loads, 438 kW of generation capacity remains available for second-level loads. Among the second-level loads, power is allocated to nodes 5, 7, 17, and 23, which collectively consume 410 kW. However, due to the limited residual capacity and network constraints, nodes 13 and 28 are not restored within this time interval.
To validate the applicability and scalability of the proposed two-stage restoration method under a medium-scale test system, an additional case study is conducted based on a practical 61-bus distribution network. This system includes multiple generation resources and features a complex radial topology.
The network comprises a total of 61 nodes, with two black-start generators located at node 4 and node 43. The remaining six generators at nodes 8, 20, 24, 33, 36, and 45 are non-black-start generators that require cranking power from black-start generators to initiate their start-up processes.
Figure 11 illustrates the original topology of the distribution network and marks the sectionalizing switches as well as the post-earthquake component failures.
The simulation results of the 61-bus distribution network further demonstrate the effectiveness of the proposed two-stage restoration method under more realistic and larger-scale conditions. The results are shown in
Table 5 and
Table 6. Due to earthquake-induced damage, generator G20 is rendered inoperable and remains offline throughout the restoration process. In the initial time steps, both black-start generators located at nodes 4 and 43 are successfully energized and begin operation. The remaining non-black-start generators G8, G24, G33, G36, and G45 are sequentially restarted in
t = 5 or
t = 6 by receiving cranking power through feasible transmission paths.
During the subsequent load restoration phase, all first-level loads are fully restored, totaling 540 kW, which accounts for 100% of the first-level load demand. Additionally, 410 kW of second-level loads are restored, corresponding to 78.85% of their total demand. These results indicate that, despite earthquake-induced component failures and partial generator loss, the proposed method effectively coordinates generator start-up and load restoration under operational and topological constraints.
This case study confirms that the proposed framework is well-suited for medium-scale distribution systems, offering adaptive and efficient recovery strategies. The method can provide valuable operational guidance for post-earthquake distribution system dispatching by optimizing restoration decisions in a data-driven and scenario-specific manner.
In current practice, most distribution network restoration strategies rely on pre-defined black-start plans that are established under normal operating conditions. These pre-arranged schemes assume a fixed system topology and generator availability, and are not adapted in real-time to specific failure scenarios. While such strategies may be effective for predictable faults or controlled islanding events, they are often inadequate in the aftermath of large-scale natural disasters such as earthquakes. In particular, fixed black-start plans may fail to address topological fragmentation, component unavailability, or disrupted transmission paths, resulting in non-optimal or even infeasible restoration decisions. This can significantly reduce restoration efficiency and delay the recovery of critical loads.
In contrast, the method proposed in this paper dynamically adapts to post-disaster conditions by explicitly incorporating earthquake-induced damage scenarios into the restoration planning process. Through probabilistic failure modeling and scenario-based optimization, our approach identifies the optimal start-up sequence of available generators and coordinates load restoration pathways according to real-time system capabilities. This enhances the resilience of the distribution system by ensuring that restoration decisions remain feasible and efficient even under adverse conditions.
To evaluate the advantages of the proposed method, a comparative case study is conducted against an existing distribution network restoration approach that does not consider the impacts of earthquake-induced damage. Unlike our method, which explicitly models component failures and network degradation caused by seismic events, the existing approach assumes an intact system and follows a pre-defined black-start sequence. As a result, it may produce infeasible or suboptimal restoration decisions under disaster scenarios.
The simulation results demonstrate that the traditional approach, which assumes full connectivity and available resources, fails to restore critical generators and loads in scenarios with significant damage. The results of this method, the comparison method, are shown in
Table 7 and
Table 8. In this comparative case, only generators G1, G4, and G22 are successfully restarted, while the remaining units fail to recover due to disrupted energization paths affected by earthquake-induced line outages. Consequently, the available generation capacity for load restoration is significantly reduced to 440 kW. In the subsequent load recovery stage, only 210 kW of first-level loads are restored, accounting for 58.33% of total first-level demand. For second-level loads, 210 kW are restored, corresponding to 39.62% of the total. In contrast, the proposed method successfully navigates the degraded topology, achieves a higher critical load restoration rate, and ensures more reliable system recovery.
To further demonstrate the generality and robustness of the proposed two-stage restoration method, an additional simulation is conducted under a higher-intensity earthquake scenario. In this case, a more severe seismic event is assumed, characterized by increased PGA across the network area. The objective of this scenario is to evaluate the performance of the proposed method under extreme stress conditions where infrastructure damage is more extensive and restoration decisions are more challenging.
Specifically, the PGA at each node is scaled up by approximately 30% compared to the baseline scenario. This leads to higher failure probabilities for distribution components based on the fragility model. In particular, the average failure probability of overhead lines increases to approximately 0.60–0.85, while transformers and switching devices exhibit failure probabilities in the range of 0.40–0.60. As a result, the network experiences more severe fragmentation, with a larger number of nodes and feeders becoming electrically isolated. The degraded topology of a severe earthquake is shown in
Figure 12.
Solving the MILP and MISOCP model, the test results are shown in
Table 9 and
Table 10. As a consequence, only three generators, G1, G4, and G16, are successfully restarted during the restoration process. G1 is energized at the beginning of the restoration because of its black-start capability. Subsequently, G4 and G16 are restarted after limited cranking support is routed through partially restored transmission paths. The remaining generators are unable to initiate start-up due to broken supply paths and insufficient cranking power, resulting in a severely constrained generation capacity throughout the recovery horizon.
The limited generation availability, combined with disrupted network connectivity, directly impacts the system’s ability to restore prioritized loads. By the end of the recovery process, only 58.33% of first-level loads and 37.73% of second-level loads are restored. The reduction in critical load recovery reflects not only the generation shortage but also the loss of network continuity to specific high-priority nodes. In particular, several first-level loads are located at nodes whose supply routes are permanently disconnected due to cascading line failures.