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Using detailed analyses of waveform components, voltage topographies and source localisation methods, we described the spatiotemporal propagation of SSEPs across the brain and demonstrated the stability of EEG recordings over time and across animals.
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This principle uses the measured fault component voltage and current on one side of the transmission line to estimate the fault component voltage on the other side.
Figure 2 is the distribution diagram of the measured value and estimated value of fault component voltage.
As for internal faults, there exists some difference between the measured value and the estimated value of fault component voltage.
The waveforms of fault component voltage and fault component current, and the waveforms of transient energies detected on the rectifier side and the inverter side are shown in Figs. 7a and b, respectively.
For positive pole line, it can be seen from Fig. 7 and Table 1 that the polarities of fault component voltage and current are opposite; the transient energies detected on both the rectifier side and the inverter side are negative, and they all exceed the threshold value, so two protection units on both sides of the positive pole line identify a positive direction fault.
The measured value and estimated value of fault component voltages on both sides of the line are consistent, when external faults occur.
Hence, both of the measured and the estimated fault component voltages on two sides of the transmission line can be acquired.
Figure 4 shows the fundamental components of voltage and current signals after pre-processing with DFT.
Here Va+ and Vb+ represent the positive sequence components of voltage phasors at buses a and b.
Later, one full cycle recursive DFT was used for calculating the fundamental components of voltage and current.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com