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Fig. 6 Current phase changes of fault power path (F1 and ABC).
Fig. 7 Current phase changes of fault power path (F2 and ABC) Fig. 8 Current sum (F2 and ABC).
Judged by the criterion in Test and results section, the fault is identified to be on the line 6 13 which is fault 3. Fig. 9 Current phase changes of fault power path (F3 and ABC).
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Recently, on the basis of seismicity analysis (of tremors) about tidal responses, Ide and Tanaka (2014) and Tanaka et al. (2015a) suggested exponential dependence of stress changes on fault slip rates.
Furthermore, the fault diagnosis strategy is be able to distinguish when the operator is carrying out load power changes free of fault as normal operating conditions.
Then, the changes of the fault signal approximately equal to the changes of the residual signal.
Figure 7 shows the current phase changes of the fault power path.
The phase angle changes of the fault power path are calculated and the two terminal phase angle changes of one line are compared to judge the fault.
Table 3 Voltage amplitude and objection function values of key nodes (Fault 2) Node 1 (DG) 4 5 6 (DG) 8 (DG) ABC Voltage Amplitude (kV) 98.44 3.79 68.09 63.74 127.02 Z ∗ (MW) 2.52 7.40 −1.63 −9.92 0. The phase angle changes of the fault power path are calculated and the two terminal phase angle changes of one line are compared to judge the fault.
Table 1 Voltage amplitude and objection function values of key nodes (Fault 1) Node 1 (DG) 4 5 6 (DG) 8 (DG) ABC Voltage Amplitude (kV) 98.92 5.62 68.98 64.69 127.02 Z ∗ (MW) 3.25 11.86 1.14 −9.85 0. Figure 6 shows the current phase changes of the fault power path.
The analysis shows that with the change of the fault location, the action time of the current protection zone I can be adjusted adaptively.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com