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Development of a wavelet-based algorithm to detect and determine ...

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7.3. MATLAB IMPLEMENTATION 61<br />

7.3.2 Summary<br />

Figure 7.7: Structure chart <strong>of</strong> the program module<br />

which identifies the disturbance<br />

It is possible <strong>to</strong> add new pattern for other disturbances. The calculation is the same as<br />

with already integrated disturbances. It is not necessary <strong>to</strong> find new criteria <strong>to</strong> <strong>detect</strong><br />

these new disturbances, as it is necessary if the identifying is estimated with changing<br />

<strong>of</strong> the RMS values (for example for a short circuit the criterias are: decreasing voltage<br />

<strong>and</strong> increasing current, but this can be a load switching also, thus additional criterias<br />

are need for this identifying).<br />

The characteristic pattern described are calculated for a voltage frequency <strong>of</strong> 60Hz at<br />

an unknown sampling rate. So these pattern have <strong>to</strong> be adopted for 50Hz <strong>and</strong> a known<br />

sampling frequncy. Through simulations with Matlab it is known that for getting the<br />

same pattern as described, a sampling rate <strong>of</strong> 8333,33Hz is necessary. Because this is<br />

not possible, the new pattern have <strong>to</strong> be calculated. To calculate them, it is necessary<br />

<strong>to</strong> have very clear disturbance recordings. Of course this is possible with a simula-<br />

<strong>to</strong>r (power network model or computer <strong>based</strong> simula<strong>to</strong>r). It is very interesting <strong>to</strong> do<br />

this simulation with a sampling rate <strong>of</strong> 12,8kHz, because the Simeas R disturbance<br />

recorder can be used <strong>to</strong> get the disturbance recordings or 6,4kHz because the distur-<br />

bance recording can be downsampled from the recordings from the Simeas R. The<br />

pattern for several equal disturbances are not the same exactly but in a small range. So<br />

several disturbances for each fault have <strong>to</strong> be calculated <strong>to</strong> get the range <strong>of</strong> the pattern.<br />

In the time for this diploma thesis, it was not possible <strong>to</strong> make these simulations.<br />

It is obvious <strong>to</strong> use this small peaks, which are described above for localizing the dis-

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