2.1. Offshore Wind Grid Connection System Modeling
The topology of the offshore wind AC submarine cable transmission system is illustrated in
Figure 2. Specifically, the main structure of the offshore wind AC transmission system is depicted in
Figure 2a. The control schematic of the rotor-side converter (RSC) is shown in
Figure 2b, while that of the grid-side converter (GSC) is presented in
Figure 2c. The structure of the phase-locked loop is illustrated in
Figure 2d.
In
Figure 2a, the main components of the offshore wind AC transmission system are illustrated, including the wind turbine, permanent magnet synchronous generator (PMSG), machine-side converter, grid-side converter, filter resistor
R1, filter inductor
L1, submarine AC cable, grid inductor
Lg, and the grid.
In
Figure 2b, the rotor-side converter (RSC) employs rotor flux-oriented vector control to achieve a precise regulation of electromagnetic power and rotational speed. The control logic of the machine-side converter is structured as a dual-loop system, comprising an outer speed loop and an inner current loop. The outer speed loop uses the error between the reference speed
n*, typically determined by a maximum power point tracking strategy, and the actual speed
n as input. This error is processed by a PI controller to generate reference currents
and
, with
typically set to zero. The inner current loop takes the error between reference current
,
and actual currents
isd,
isq as input, producing d-axis and q-axis voltages
Usd,
Usq via a PI controller. These voltages account for stator resistance
Rs, stator inductances
Lsd and
Lsq, electrical angular velocity
ωe, and permanent magnet flux linkage ψ
f. The resulting signals undergo dq/abc transformation and sinusoidal pulse width modulation (SPWM) to generate switching signals, synchronized with the rotor angle
θRSC.
In
Figure 2c, the grid-side converter adopts grid voltage-oriented vector control to regulate DC-link voltage and reactive power output while ensuring low-voltage ride-through (LVRT) capability. The control scheme of the grid-side converter features a dual-loop structure. The outer voltage loop operates in two modes based on system conditions: under normal operation (Mode 0), the error between the reference DC bus voltage
Udcref and the actual voltage
Udc is processed by a PI controller to produce the reference d-axis current
Idref, with
Iqref = 0, ensuring stable DC voltage; during LVRT (Mode 1),
Idref is calculated as
, where
Iqref is determined by (0.9 − U
pcc)
K1IN, providing additional reactive support to meet grid LVRT requirements. The inner current loop uses the error between reference currents
Idref,
Iqref and actual currents
Id,
Iq as input, generating d-axis and q-axis voltages
Ud,
Uq via a PI controller. These voltages incorporate feedforward terms
ed,
eq, angular frequency ω, and inductance
L1, followed by dq/abc transformation to produce switching signals. The control phase signal
θPLL, used for system synchronization, is generated by the DSOGI-PLL.
In
Figure 2d, the DSOGI-PLL structure processes the three-phase grid voltages
Ea,
Eb,
Ec, which are transformed into stationary frame components
uα and
uβ via an abc/αβ transformation module. These components are then processed by a dual second-order generalized integrator to extract positive-sequence components
and
. The positive-sequence components undergo αβ/dq transformation to yield d-axis and q-axis voltage components
ed and
eq, ultimately producing
θPLL for phase synchronization with the grid.
2.2. Mechanism of Phase Jump Generation in Offshore Wind Systems
When an asymmetrical fault occurs in the offshore wind grid-connected system, a phase jump occurs at the grid-connected point. The phase-locked loop undergoes a short dynamic process when tracking the phase of the grid connection point, resulting in a phase-locking error. The phase-locking error affects the output characteristics of the inverter by influencing the Park transform and inverse transform processes, resulting in a large harmonic component in the inverter output current.
When an asymmetric fault occurs, the three-phase asymmetric voltage can be expressed as follows:
where
Ea,
Eb, and
Ec are phase A, B and C voltages, respectively;
ω0 is the voltage fundamental frequency;
Esa,
Esb, and
Esc are the voltage amplitudes of each phase after the fault.
θa,
θb, and
θc are the phase jump angles of each phase after the fault. The unbalanced voltage components in the two-phase stationary coordinate system are as follows:
The voltage positive-sequence component can be calculated by dividing
uα,
uβ by SOGI quadrature. The voltage positive-sequence component is transformed by αβ-dq to obtain
and
. The expressions for
ed and
eq obtained from the αβ/dq transformation of the positive-sequence components
and
are given by the following:
Among them,
where
θ is the angle between the d-axis and the a-axis, and the phase jump angle of the positive-sequence voltage after the fault is noted as
δθ. When
= 0, the phase jump angle of the positive-sequence voltage under three-phase imbalance
δθ is as follows:
Per Equation (5), under an asymmetric fault, the positive-sequence voltage phase jump angle δθ can be expressed as a function of the unbalanced three-phase voltage amplitudes Esa, Esb, Esc and their respective phase jump angles θa, θb, θc. Consequently, a phase jump δθ manifests in the system during an asymmetric fault.
2.3. Influence of Phase Locking Error on Harmonic Characteristics
When an asymmetrical short circuit fault occurs in the offshore wind power grid-connected system, a phase jump occurs at the grid-connected point. During the phase jump, there is a short-time dynamic process of phase tracking by the phase-locked loop, and the phase can be accurately tracked in the theoretical case. However, due to the existence of the integral link when the fault occurs, the phase tracking of the phase-locked loop is delayed, and before the accurate tracking, the output phase of the phase-locked loop deviates from the actual phase. The schematic diagram of the voltage phase change before and after the fault is shown in
Figure 3.
In
Figure 3,
θ0 is defined as the angle between the d-axis and α-axis.
θ1 represents the phase of positive-sequence voltage at the point of common coupling after fault occurrence. The positive-sequence voltage phase jump angle
δθ corresponds to the d-axis phase difference between pre-fault and post-fault conditions, expressed as
δθ =
θ1 −
θ0.
θPLL denotes the angle between the d-axis and
dPLL-axis, representing the tracked phase angle during the dynamic tracking process of the phase-locked loop. ∆
θe is defined as the untracked phase angle during DSOGI-PLL dynamic tracking, termed the phase-locking error, which satisfies ∆
θe =
δθ −
θPLL.
The phase-locking deviation ∆
θe, which remains untracked during the DSOGI-PLL dynamic tracking process, is influenced by the parameters of the PLL’s PI controller. When ∆
θe is considered, the PLL dynamic response alters the output current characteristics at the offshore wind farm’s point of common coupling. This occurs through modifications in the Park inverse transformation process. The analytical expression of the fault current is derived as follows [
9]:
The phase-locked loop PI parameters in the analytical expression are found to increase harmonic content in the inverter output current.
Under ideal conditions, the fault current comprises solely the fundamental frequency component ω0. However, when the dynamic response of the DSOGI-PLL is considered, the inverter output current includes non-fundamental frequency components in addition to the fundamental component, resulting in elevated harmonic content.
According to Equation (6), to reduce the harmonic content in the inverter output current, the tuning of the PI parameters can be analyzed. The dynamic response of the DSOGI-PLL is influenced by these PI parameters, and the response time of the dynamic process can be expressed as follows:
where
tr is defined as the rise time,
ωc is the natural oscillation frequency and
ξ is the damping ratio.
The relationships between the natural oscillation frequency
ωc, damping ratio
ξ, and the DSOGI-PLL PI parameters are established as follows:
where
kp is defined as the proportional gain coefficient of the phase-locked loop, and
ki is specified as the integral gain coefficient.
The following relationship is derived by combining Equations (8) and (9):
The variation pattern between the DSOGI-PLL PI parameters and the rise time can be obtained from the above equations. This correlation is graphically demonstrated in
Figure 4.
As shown in
Figure 4, by adjusting the PI parameters of the DSOGI-PLL, the dynamic rise time can be improved, thereby accelerating the dynamic response. Traditional DSOGI-PLLs typically use preset PI coefficients. However, these preset PI parameters fail to quickly track sudden voltage phase changes during grid faults. Considering the dynamic characteristics of the DSOGI-PLL during unbalanced faults, real-time dynamic adjustment of the DSOGI-PLL’s PI parameters can be used to track the actual phase. A grid-connected harmonic suppression strategy based on Vague set theory [
36,
37,
38] is designed in this study. This approach models and processes phase-locked errors in offshore wind power systems through three dimensions: true membership degree, false membership degree, and hesitation degree. The strategy updates the DSOGI-PLL’s PI parameters in real time, allowing the DSOGI-PLL to match the actual phase angle variations in the grid and effectively suppress harmonic content in the grid connection.