43 results about "Angular frequency" patented technology

A method for coating a substrate, in which emissivity values (UE,n) and reflectance values (UR,n) are determined using pyrometers in order to control the temperature of the substrate. Since the wavelengths of the two pyrometers differ slightly, the raw temperature determined from the emissivity value (UE,n) cannot be optimally compensated for using the reflectance value (UR,n). The angular frequencies (ωE, ωR) of the curves of the two values (UE,n) and (UR,n) oscillating over time t differ slightly from one another, leading to an oscillation of the actual temperature value. To counteract this phenomenon, values modified by a numerical time transformation are used rather than the measured values.

The invention provides a VSG inertia and damping adaptive coordination control method, and belongs to the technical field of virtual synchronous generator control. Research finds that the oscillation process can be segmented, and in each segment, the inertia and damping coefficient requirements are different. Based on the relevance between the rotational inertia / damping coefficient and the system angular frequency offset / angular frequency change rate, the arctan function is used in the control strategy provided by the invention to participate in adjusting the system inertia and damping change, and the advantage that the rotational inertia and damping coefficient parameters of the virtual synchronous machine are flexible and adjustable is fully utilized; the relevance between the angular frequency change rate / angular frequency offset and the rotational inertia / damping coefficient is studied. Through cooperative control of the rotational inertia and the damping coefficient, when the system is disturbed, sufficient inertia support can be provided, the frequency change of the system is stabilized, and the transient process of the frequency and the active power during system load disturbance is effectively improved.

The embodiment of the invention discloses a harmonic compensation method for an angle error of a magnetic encoder, and the method comprises the steps: enabling the magnetic encoder to rotate at a constant speed in a setting mode, collecting sine and cosine signals outputted by the magnetic encoder, and carrying out the calculation through CORDIC, thereby obtaining an initial angle sequence containing a fundamental wave error and a harmonic wave error; extracting each harmonic component through an adaptive wave trap, constructing a harmonic compensation polynomial, and storing each coefficient; in an application mode, a magnetic encoder signal is collected in real time, a current initial angle value is solved, a harmonic compensation amount is calculated according to a current fundamental wave angular frequency and a stored coefficient, and an accurate angle value is obtained by subtracting the compensation amount from the initial angle value. According to the method, external reference signals and a large amount of storage space are not needed, each harmonic error is directly eliminated through a harmonic compensation polynomial, and approximate errors caused by traditional linear interpolation are avoided; and the compensation precision can be improved only by increasing polynomial terms, and the storage requirement is not obviously increased.

The invention discloses a network construction type energy storage parameter adaptive control method for improving transient stability. The method comprises the following steps: determining a rated angular frequency of a network construction type energy storage system, measuring a current operation angular frequency, and calculating an angular frequency deviation and an angular frequency change rate; the VSG output active power is measured, and the active power deviation is calculated in combination with the mechanical power instruction value; dividing a system oscillation period into four oscillation intervals; calculating a damping coefficient reference value and a rotational inertia reference value by using the maximum mechanical torque of the VSG system, the maximum angular frequency offset allowed by the system and the maximum active power output by the system; calculating real-time rotational inertia and a damping coefficient according to the oscillation interval in combination with the adjustment coefficient; and the rotational inertia and the damping coefficient controlled by the VSG are adjusted. According to the method, the defect that transient stability and dynamic response are difficult to consider by fixed parameters in traditional virtual synchronous generator control is overcome, the frequency overshoot is remarkably reduced, and the recovery time is shortened.

The invention discloses an electric energy metering method and device based on harmonic self-adaptive observation and zero point tracking type SOGI-FLL. The electric energy metering method comprises the following steps: step 1, carrying out ADC sampling on voltage and current signals of a power grid; 2, performing frequency rapid estimation on the voltage signal based on a zero point tracking frequency-locked loop, and obtaining a fundamental wave angular frequency of a power grid in real time; step 3, constructing adaptive observers of voltage and current by using the fundamental wave angular frequency, and estimating parameters of fundamental waves, harmonic waves and direct current components in voltage and current signals in real time through an adaptive law based on Lyapunov stability; 4, according to the parameter estimation value, the amplitude and phase of the voltage and current are calculated; and step 5, calculating active power and reactive power of each harmonic based on the voltage and current amplitudes and phases obtained in the step 4, and summing to obtain total active power and total reactive power so as to realize metering of active electric energy and reactive electric energy. According to the invention, rapid and accurate metering of fundamental wave and harmonic wave electric energy under complex working conditions is realized.

The invention discloses an underwater pore medium stratum bubble size calculation method, and relates to the technical field of underwater pore medium stratum geophysical exploration, and the method comprises the following steps: S1, obtaining rock physical parameters of an underwater stratum to be detected; s2, a sound wave transmitting transducer and a receiver are deployed at a point to be measured, the sound wave transmitting transducer transmits a set signal to determine a measurement frequency range, and the receiver records a sound wave speed and an attenuation coefficient of each frequency point; s3, judging whether adjacent frequency points meeting the requirements of sound wave speed reduction and attenuation coefficient increase exist or not, and if yes, re-measuring and extracting the sound wave speed and attenuation coefficient corresponding to the bubble resonance characteristics; otherwise, recording the bubble-free characteristic times, and if the times do not reach the threshold value, continuing to adjust the number of the frequency points and returning to the step 2; s4, constructing a target function; and S5, under the condition that the angular frequency and the sound wave speed are known, solving the independent variable, the bubble radius and the bubble saturation which enable the objective function to be minimum, and determining the final bubble size and saturation.

The invention provides an ocean current dynamic response analysis method and system based on a wind wave current coupling relationship, and the method comprises the steps: building a first fluctuating wind speed model based on sea wind characteristic parameters, sea wave characteristic parameters and motion state parameters of a ship under different sea conditions, and calculating the power spectrum density of the fluctuating wind speed through employing a specific calculation method; constructing a relational expression between the power spectrum density and the amplitude of the fluctuating wind speed in the angular frequency interval range; a second fluctuating wind speed model is obtained through the relational expression and the first fluctuating wind speed model, and then the absolute wind speed of the sea wind is calculated; the method comprises the following steps: calculating the sexual wave height of sea waves according to the absolute wind speed, respectively calculating the flow velocity of wind-induced flow and wave-induced flow by adopting a specific calculation method, further constructing an ocean current flow velocity model, and calculating the disturbing force of ocean current on a ship by adopting the specific calculation method based on the ocean current flow velocity model. By fully considering the mutual influence among the sea wind, the sea wave and the ocean current, the dynamic response of the ship in the wind wave current can be predicted more accurately.

The invention provides a frequency-locked phase-locked loop method, which is based on a synchronous rotating coordinate system, and adopts an angular frequency error and a phase angle error to carry out frequency locking and phase locking. According to the technology, a low-pass filter is adopted to observe a power grid voltage synchronous rotating coordinate system component udq to obtain an observation error edq and an observation value # imgabs0 #, the conjugate # imgabs1 # of the observation value is calculated, and the observation error edq is multiplied by the conjugate # imgabs2 # of the observation value to obtain an expression containing angular frequency error information; multiplying an imaginary part xaI containing an angular frequency error information expression by a normalization coefficient gamma and a transfer function f (s) for pole-zero cancellation to obtain an angular frequency error omega e, multiplying an actually measured value of a direct-axis component or a quadrature-axis component of the power grid voltage by a proportionality coefficient K, or multiplying an observed value by the proportionality coefficients K and f (s) to serve as a phase angle control signal epsilon, and calculating the phase angle of the power grid voltage according to the phase angle control signal epsilon. And after the added value is input into the integrator with the transfer function of # imgabs3 #, an angular frequency observation value # imgabs4 # is output, after the angular frequency observation value # imgabs5 # is input into the integrator with the transfer function of # imgabs6 #, a phase angle observation value # imgabs7 # is output, and finally frequency locking and phase locking are achieved.

The present invention discloses a method for measuring the acoustic nonlinear coefficient of a material by using the phase relationship. It uses finite-amplitude ultrasound to perform non-destructive testing on a material with mechanical nonlinearity, performs Hilbert transform processing on the detected and / or calculated displacement signal or particle vibration velocity signal to obtain the phase of the nonlinear signal, and then obtains the normalized angular frequency through numerical calculation, so as to measure the acoustic nonlinear coefficient according to the maximum value of the normalized angular frequency. The method of the present invention is simpler, and can expand the experimental conditions. The nonlinear coefficient can still be measured under conditions of longer distance, stronger excitation, and larger nonlinear coefficient, and the test results are more accurate; the applicable conditions of the present invention can approach the generation position of the shock wave.

The present application relates to the technical field of marine winch metering and control in marine operation equipment, and discloses a compensation method for dynamic error of marine winch metering. By synchronously sampling the angular displacement and the acceleration along the rope direction, the rope length sequence is converted to obtain the rope length vector and the acceleration vector in the window; the discrete angular frequency is set according to the sampling point and the period, the sine cosine base function is generated to form the harmonic orthogonal base, and the rope length sequence is projected and reconstructed to obtain the harmonic component of each frequency; the power spectrum analysis is performed on the acceleration sequence, the dominant frequency of vibration is identified according to the power spectrum, and the upper limit of high-frequency disturbance is determined, and the harmonic component is accumulated in the frequency not higher than the upper limit to obtain the low-frequency trend rope length sequence; the rope length is first reduced by the low-frequency trend value and then reduced by the high-frequency error component to form the error vector and the compensated rope length sequence, the double compensation of the winch metering error is realized, the rope length change and the vibration disturbance are separated under the time-frequency structure, and the metering precision and the real-time performance are improved.

The invention provides an ocean current flow velocity modeling method and system based on a wind wave flow coupling relation, and the method comprises the steps: building a first fluctuating wind speed model based on sea wind characteristic parameters and sea wave characteristic parameters under different sea conditions, calculating the power spectrum density of fluctuating wind speed through employing a specific calculation method, and carrying out the calculation of the power spectrum density of the fluctuating wind speed in an angular frequency interval range; constructing a relational expression between the power spectrum density and the amplitude of the fluctuating wind speed; a second fluctuating wind speed model is obtained through the relational expression and the first fluctuating wind speed model, and then the absolute wind speed of the sea wind is calculated; according to the method, the sexual wave height of sea waves is calculated according to the absolute wind speed, the flow velocity of wind-induced flow and the flow velocity of wave-induced flow are respectively calculated by adopting a specific calculation method, then an ocean current flow velocity model is constructed, and the more accurate and comprehensive ocean current flow velocity model can be provided by fully considering the mutual influence among sea wind, sea waves and ocean currents. The method is of great significance in understanding and coping with a complex marine environment.

The application discloses a laser radar correction method and device based on an angular frequency field, a storage medium and electronic equipment, and the method comprises the following steps: controlling a laser radar to emit sinusoidal modulation light to irradiate a whiteboard, acquiring four-phase original intensity data and displacement increment values; reconstructing a phase sequence for each pixel and estimating an angular frequency, and forming an angular frequency distribution of a full field of view; establishing an analytical coupling model of the angular frequency and a rotation matrix according to the distribution, an internal parameter matrix and a whiteboard normal vector, solving a rotation matrix estimation value by using a least square method, and combining an initial normal distance to calculate a translation vector estimation value; calculating real distances of each pixel to a whiteboard point according to the rotation and translation estimation values, recalibrating phase zero point offset and fixed mode phase noise, and generating a correction lookup table; and outputting the rotation, translation parameters and the lookup table. According to the application, a pattern target is not needed, and only a whiteboard and a guide rail are used to restore external parameters, system errors introduced by tilting are reduced, and the ranging and point cloud reconstruction precision are improved.

The invention relates to the technical field of wave making, in particular to a wave making method based on an underwater flat plate longitudinal pushing type wave maker. Wave surface equations of different wave surface positions are constructed according to the obtained geometric parameters of the wave maker and the motion parameters of the underwater flat plate; according to the input target wave parameter, determining the wave number of the target wave and the underwater flat plate amplitude required for generating the target wave; if the target wave is a regular wave, controlling an underwater flat plate to longitudinally move according to a simple harmonic motion rule according to the flat plate amplitude; and if the target wave is an irregular wave containing N angular frequency components, introducing a random phase, and driving the underwater flat plate to perform multi-frequency synthetic vibration according to the flat plate amplitude corresponding to each angular frequency component. According to the method, the wave surface equation of vertical movement of the two-dimensional underwater flat plate structure is derived based on the potential flow theory, and the transfer function is obtained by using the equation, so that accurate generation of regular waves and irregular waves can be realized through the underwater flat plate.

The application provides a flow field reconstruction and deduction method based on K-A theorem, and belongs to the technical field of ship hydrodynamics. First, multi-dimensional data such as the direction, amplitude, period, frequency and flow velocity of irregular waves are collected and integrated into high-dimensional wave vectors. Then, the KAN network with B-spline curve as a learnable function is used to map the high-dimensional input into a low-dimensional parameter list, obtain the amplitude, angular frequency and initial phase of the dominant equivalent regular wave, calculate the decoupling target function by constructing an equivalent wave superposition model, compare the decoupling target function with the true value to obtain a loss function, and then optimize the network parameters by backward propagation until convergence. Finally, based on the network output parameters, a wave superposition model is constructed to represent the real wave in the form of a series of interpretable regular waves superimposed in time sequence, so that efficient and accurate flow field reconstruction and deduction are realized.

The present invention discloses a method and system for identifying power system oscillation parameters based on synchronized phasor data, which relates to the technical field of power system oscillation analysis. It solves the problem that the traditional MPM directly obtains the eigenvalues of the matrix pencil, resulting in large errors. The key points of its technical solution are as follows: By constructing a real Hankel matrix and solving the eigenvalues of this matrix, the fundamental wave component angular frequency that satisfies the angular frequency conjugate constraint of two modes of the fundamental frequency component and the oscillation component angular frequency that satisfies the angular frequency conjugate constraint of two modes of the oscillation component can be directly obtained. The solution is simple and the computational amount is small. Moreover, by combining the real part and the imaginary part of the synchronized phasor to construct a real Hankel matrix, the information of the synchronized phasor can be completely retained, and thus the subsynchronous oscillation parameters can be accurately identified under an ultra-short data window.

The invention provides a method and a system for transferring motion energy of a large ship in a wind wave flow environment, and the method comprises the steps: building a first fluctuating wind speed model based on the feature parameters of sea wind, sea waves and ships under different sea conditions, and calculating the power spectrum density of the fluctuating wind speed through employing a specific calculation method; constructing a relational expression between the power spectrum density and the amplitude of the fluctuating wind speed in the angular frequency interval range; a second fluctuating wind speed model is obtained through the relational expression and the first fluctuating wind speed model, and then the absolute wind speed of the sea wind is calculated; and finally, based on the time domain motion signal and the absolute wind speed in any marine environment, respectively calculating the average power of the sea waves, the sea wind and the ship by adopting a specific calculation method, and further calculating the energy transfer efficiency of the disturbed motion of the ship under different sea conditions. The motion characteristics and the energy transfer relation of the large ship in different working conditions can be comprehensively described by fully considering the working condition environment jointly influenced by complex wind wave and flow environments under different sea conditions.

The invention discloses a joint inversion three-dimensional quality factor method, which comprises the following steps of: acquiring average attenuation travel time through an initial three-dimensional quality factor (Q value) and an average attenuation travel time formula, and acquiring a theoretical frequency spectrum amplitude at the frequency by combining a plurality of initial values including corner frequency, field effect, low-frequency amplitude and frequency and an amplitude formula; converting the displacement frequency spectrum amplitude in the frequency domain into an observation frequency spectrum amplitude in a natural logarithm domain, and obtaining a residual vector formula in combination with a theoretical frequency spectrum amplitude; a formula obtained after meshing of the seismic wave three-dimensional propagation speed and the initial Q value in the average attenuation travel time formula is substituted into a residual vector formula, smooth constraint and damping parameters are added to obtain a new residual vector formula, and the new residual vector formula is solved to obtain a value of a parameter disturbance quantity; superposing the values to the plurality of initial values to obtain a plurality of new initial values of the next round of iteration; and substituting the initial three-dimensional Q value back to a residual vector formula to obtain a residual vector, and taking the new initial three-dimensional Q value as a target three-dimensional Q value when a difference value between the residual vector and the amplitude meets a condition.

The present invention discloses a method for calculating the bubble size of an underwater pore medium formation, which relates to the technical field of geophysical exploration of underwater pore medium formations, and includes: S1, obtaining the petrophysical parameters of the underwater formation to be measured; S2, deploying a sound wave transmitting transducer and a receiver at the measurement point, the sound wave transmitting transducer emits a set signal to determine the measurement frequency range, and the receiver records the sound wave velocity and attenuation coefficient at each frequency point; S3, determining whether there are adjacent frequency points that satisfy the condition that the sound wave velocity decreases and the attenuation coefficient increases. If so, re-measure and extract the sound wave velocity and attenuation coefficient corresponding to the bubble resonance characteristics; otherwise, record the number of times without bubble characteristics. If the number of times does not reach the threshold, continue to adjust the number of frequency points and then return to step 2; S4, constructing an objective function; S5, under the condition that the angular frequency and the sound wave velocity are known, solving the independent variable, bubble radius and bubble saturation that minimize the objective function, and determining the final bubble size and saturation.

The invention relates to an angular sensor comprising: a resonator (2) capable of supporting a radial mode of vibration with respect to an axis of symmetry of the resonator (2); transducers (5.1, 5.2, 6.1, 6.2) for delivering a first measurement signal and a second measurement signal concerning a deformation of the resonator (2) in a first direction and a second direction, respectively, said directions being orthogonal to one another in a reference frame of the mode of vibration, and for applying a force to the resonator (2) in these two orthogonal directions; and an electronic processing circuit (7) electrically connected to the transducers (5, 6) and designed to determine, on the basis of the measurement signals, an estimate (Formula) of an angular speed applied to the angular sensor and to output control signals for the transducers (6.1, 6.2) in order to generate and keep a vibration of the resonator (2) at a frequency corresponding substantially to a theoretical natural angular frequency ω0 and with a substantially constant amplitude a and a substantially zero quadrature component q, by processing an amplitude servo-control error X p — a 0 where X p is an amplitude servo-controlled to an amplitude setpoint a 0 , a quadrature servo-control error Y q , an angle estimation error Y p and a phase estimation error X q , characterized in that the electronic processing circuit (7) is designed to carry out compensation that makes the errors insensitive to a variable angular speed of the sensor taking into account the theoretical natural angular frequency ω0 and the estimate of the angle of the angular sensor.

The present invention discloses a method and system for analyzing the seismic active earth pressure of a bridge abutment. The method comprises the following steps: first, a calculation model for the horizontal acceleration distribution of the abutment can be established based on the three-segment design acceleration response spectrum specified in the current specification. Then, the characteristic angular frequency of the abutment to be analyzed can be obtained, and the characteristic angular frequency can be substituted into the calculation model for the horizontal acceleration distribution of the abutment, thereby calculating the various sinusoidal acceleration time-history component coefficients of the abutment at the characteristic angular frequency. Finally, all the sinusoidal acceleration time-history component coefficients and the various structural parameters of the abutment to be analyzed can be combined to calculate the seismic active earth pressure parameters of the abutment through the constructed analytical model for the seismic active earth pressure of the abutment. Since the frequency domain characteristics of the seismic acceleration time history covered by the design response spectrum specified in the bridge seismic design specification are fully considered, the accuracy of the analytical results of the seismic active earth pressure of the abutment is improved.

The invention discloses a method, device and equipment for determining an earthquake reflection coefficient, a medium and a product. The method comprises the following steps: acquiring an actually measured seismic record, and determining an original amplitude spectrum corresponding to a target frequency band from the actually measured seismic record; the target frequency band comprises a plurality of angular frequencies; determining at least two main frequencies based on the target frequency band; determining a frequency division recording amplitude spectrum corresponding to the main frequency based on the plurality of angular frequencies, the main frequency and a preset frequency band width, and determining a wavelet amplitude spectrum corresponding to the main frequency based on the plurality of angular frequencies and the main frequency; and based on the original amplitude spectrum, the frequency division record amplitude spectrum corresponding to each main frequency and the wavelet amplitude spectrum, determining a seismic reflection coefficient corresponding to the actually measured seismic record. The problem that in the prior art, seismic wavelets are extracted from seismic records, and the seismic reflection coefficient is reversely deduced through an inversion method, so that the accuracy of determining the seismic reflection coefficient is poor is solved, and the effect of improving the accuracy of determining the seismic reflection coefficient is achieved.

This invention discloses a wave generation control method and apparatus for wave generators deployed at both ends in a wave testing tank. First, the target positions and target angular frequencies of two wave trains are determined based on the target function, which can be wave attenuation, bidirectional wave generation, or focused wave generation. Then, the propagation times of the two wave trains are calculated respectively. Based on the propagation times, the target activation time of the corresponding wave generator is determined. Finally, the corresponding wave generator is activated at the target activation time, generating the corresponding waves based on the target wave height and target angular frequency. In this invention, each end of the wave generators deployed at both ends can independently control wave generation at each end. Based on the synergistic effect of the wave generators deployed at both ends, wave propagation and superposition are controlled, accurately generating focused waves and simulating the effect of concentrated waves on marine structures.

The geosynchronous orbit debris inclination vector evolution calculation method disclosed by the application comprises the following steps: firstly, calculating the influence of the J2 term of the earth's non-spherical perturbation on the change rate of the inclination debris, calculating the angular frequency of the geosynchronous orbit debris inclination vector, the period of the precession and the angular rate of the precession under the influence of the J2 term; then, calculating the frequency of the geosynchronous orbit debris inclination vector precession, the period of the precession and the angular rate of the precession caused by the sun's gravity and the moon's gravity respectively; finally, synthesizing and calculating the different angular frequencies, the periods of the inverse precession and the angular rates of the precession. The geosynchronous orbit debris inclination vector evolution calculation method disclosed by the application separately calculates the effects of the J2 term of the earth and the sun and the moon, and compared with the traditional geosynchronous orbit debris inclination vector evolution calculation method which adopts complete numerical calculation, the method has the advantages of fast calculation speed and can be used for the analysis and calculation of the long-term evolution of the geosynchronous orbit debris orbit.

The application discloses a method for exciting polarization medium transient electromagnetic forward fast selection of central frequency, and belongs to the technical field of geophysical prospecting, and comprises the following steps: firstly, determining three-dimensional forward time step iteration parameters and a central frequency range, and constructing a Cole-Cole model; then, sequentially performing Padé series approximation on the discrete central frequency vector and the angular frequency vector at each frequency point to obtain an expansion format of each frequency point; respectively calculating time domain pulse responses of the expansion format and the Cole-Cole model and relative errors thereof, obtaining a two-dimensional distribution of the relative errors, expanding the Cole-Cole model by using the Padé series approximation method, and starting three-dimensional forward calculation of the Cole-Cole model with the exciting polarization effect. The application can provide a fast central frequency selection method for developing three-dimensional forward calculation of transient electromagnetic waves in the underground polarized medium, and is the basis of geophysical transient electromagnetic prospecting.

A method for measuring low-frequency angle dynamic characteristics of an inertial measurement combination based on a three-axis turntable comprises the following steps: mounting the inertial measurement combination on the three-axis turntable, rotating the inertial measurement combination, and sampling angular position information of the three-axis turntable and pulse output of the inertial measurement combination at a certain frequency; performing difference calculation on the pulse output of the inertial measurement combination obtained by sampling in each direction to obtain a pulse difference after the common-mode error is eliminated; calculating the triaxial angular position of the inertial measurement combination based on the pulse difference after the common-mode error is eliminated; fourier transform is carried out on the angular position information of the three-axis turntable and the three-axis angular position of the inertial measurement combination to obtain an amplitude spectrum and a phase spectrum of the three-axis turntable and the inertial measurement combination, and an angular frequency is calculated based on the maximum value in the amplitude spectrum of the angular position of the three-axis turntable and the serial number of the maximum value in the amplitude spectrum; meanwhile, the gain and the phase difference of the inertial measurement combination relative to the maximum value in the amplitude spectrum of the angular position of the three-axis turntable are calculated.

The present invention discloses a method for suppressing VSG power oscillation based on active power feedback. The method includes the following steps: 1) Collect the output voltage u of the VSG abc and the grid-connected current i abc , and calculate the active power P of the VSG e ; 2) Feed P e into the active droop control to obtain the virtual mechanical power P m , add P m to the active reference value P ref of the VSG to obtain the active command P set of the rotor motion equation; 3) Subtract P set from P e , and the obtained difference is subjected to proportional and integral operations to obtain the initial angular frequency deviation Δω1 of the VSG; 4) Multiply P e by the feedback coefficient K to obtain the angular frequency deviation correction amount Δω2 of the VSG; 5) Subtract Δω2 from Δω1 to obtain the final angular frequency deviation Δω3 of the VSG; 6) Add Δω3 to the rated angular frequency ω n to obtain the angular frequency ω of the VSG, and integrate to obtain the output phase θ of the active loop; 7) Feed the amplitude E and the phase θ of the VSG reference voltage into the voltage-current double closed loop, and drive the inverter to operate through the PWM link. This solution can achieve the suppression of the output active power transient oscillation of the VSG under external disturbances.

The invention discloses a navigation ship motion parameter extraction method based on wave height time sequence data. Two measuring points are arranged on the same side of a ship navigation main channel by adopting a wave height sensor; the method comprises the following steps: acquiring ship traveling wave time-wave height data in a channel by using double measuring points, and constructing a basic signal set; performing frequency spectrum domain conversion and purification processing on the basic signal set by combining short-time Fourier transform with noise threshold filtering to obtain an effective wave system frequency spectrum matrix; angular frequencies of two measuring points are extracted by adopting a dynamic window peak value detection method in combination with linear fitting aiming at transverse waves, and slopes of the two measuring points are extracted by frequency spectrum matrix binaryzation and improved Hough transform aiming at scattered waves; the ship navigational speed is inverted based on the angular frequency, the vertical distance between the ship and the measuring point is deduced in combination with the scattered wave slope, the navigational direction angle is deduced according to double-measuring-point geometric analysis, the navigational speed, the ship position and the course angle parameters are output, and navigational ship dynamic monitoring without active signal dependence is achieved. According to the invention, high-precision and high-reliability ship dynamic monitoring in a complex scene is realized.

The present invention provides a method and system for modeling ocean current velocity based on the wind-wave-current coupling relationship. A first fluctuating wind speed model is established based on characteristic parameters of the ocean breeze and the ocean wave under different ocean conditions, and a specific calculation method is used to calculate the power spectrum density of the fluctuating wind speed. In addition, a relationship between the power spectrum density and the amplitude of the fluctuating wind speed is constructed within the angular frequency range. A second fluctuating wind speed model is then obtained through the relationship and the first fluctuating wind speed model, and the absolute wind speed of the ocean breeze is calculated. The significant wave height of the ocean wave is calculated according to the absolute wind speed, and a specific calculation method is used to calculate the velocities of the wind-induced current and the wave-induced current, respectively, and thus an ocean current velocity model is constructed. By fully considering the mutual influence between the ocean breeze, ocean waves and ocean currents, a more accurate and comprehensive ocean current velocity model can be provided, which is of great significance for understanding and responding to complex ocean environments.

The invention belongs to the technical field of rotary transformer signal processing, and particularly relates to a rotary transformer envelope signal correction decoding method and system, and the method comprises the steps: demodulating an output signal of a rotary transformer through frequency shift, and obtaining a sine envelope signal and a cosine envelope signal; the method comprises the following steps: collecting a sine envelope signal and a cosine envelope signal based on a preset sampling frequency, carrying out offline parameter estimation, firstly estimating an envelope angular frequency estimation value of the envelope signal, and then estimating an amplitude estimation value, a phase offset estimation value and a direct current offset estimation value of the envelope signal by using the envelope angular frequency estimation value; a sine envelope signal and a cosine envelope signal are collected, and online non-ideal envelope signal correction and angular position decoding are carried out. According to the method and the system for correcting and decoding the envelope signal of the rotary transformer, the influence of a harmonic term in the envelope signal is fully considered by adopting an angular frequency off-line estimation method based on a self-adaptive notch filter and system identification.

The present invention provides a method and system for analyzing the dynamic response of ocean currents based on the coupling relationship between wind, wave and current. A first fluctuating wind speed model is established based on characteristic parameters of ocean breeze, characteristic parameters of ocean waves and motion state parameters of ships under different sea conditions, and a specific calculation method is used to calculate the power spectrum density of the fluctuating wind speed. In the angular frequency range, a relationship between the power spectrum density and amplitude of the fluctuating wind speed is constructed. A second fluctuating wind speed model is then obtained through the relationship and the first fluctuating wind speed model, and the absolute wind speed of the ocean breeze is calculated. The significant wave height of the ocean waves is calculated according to the absolute wind speed, and a specific calculation method is used to calculate the velocities of the wind-induced current and the wave-induced current respectively, and then an ocean current velocity model is constructed. Based on the ocean current velocity model and using a specific calculation method, the interference force of the ocean current on the ship is calculated. By fully considering the mutual influence between ocean breeze, ocean waves and ocean currents, the dynamic response of the ship in wind, wave and current can be more accurately predicted.