There are different causes for power system transients. For example, lightning strokes to the wires in the power system or to ground and component switching either of network components or end user equipment can produce transients. Nature of power system transients are very much event dependent.
Short duration events can be classified into three classes:
1. Events that can be identified by their fundamental frequency magnitude. Voltage magnitude in such events goes through significant changes for long periods. The changes are well apart and observable with respect to time. This enables magnitude estimators to identify and resolving events having significant changes. These are observed mainly in fault induced events, transformer saturation, induction motor starting, etc. Voltage dips with duration typically between 50ms and several seconds and interruptions with duration from several seconds up to many hours are associated with such transient events.
2. Events having significant changes in the fundamental frequency magnitude but of short duration. In such events, it is very difficult to extract voltage magnitude of transients. These are normally observed in fuse-cleared faults and self-extinguishing faults.
3. Events of very short duration (transients) for which the fundamental frequency magnitude does not offer important information. For this class, the higher frequency components of the signal must be considered for a thorough characterization and classification.
Based on waveform shape, power system transients, can be classified into
1. Oscillatory transients
2. Impulsive transients
3. Multiple transients
Impulsive transients are common during lightning. Lightning stroke may appear directly or by indirect induction. When a lightning stroke hits a transmission line (direct stroke) an impulsive over voltage is induced. They have high magnitude. Lightning over voltage can also be induced by nearby strokes to the ground or between clouds. These over-voltages are of lower magnitude than those produced by direct strokes. Normally impulsive transient shows a sudden rise followed by an exponential decay. But in some cases, lightning transient shows a sudden rise followed by a sudden drop and an oscillation with relatively small amplitude.
Short duration events can be classified into three classes:
1. Events that can be identified by their fundamental frequency magnitude. Voltage magnitude in such events goes through significant changes for long periods. The changes are well apart and observable with respect to time. This enables magnitude estimators to identify and resolving events having significant changes. These are observed mainly in fault induced events, transformer saturation, induction motor starting, etc. Voltage dips with duration typically between 50ms and several seconds and interruptions with duration from several seconds up to many hours are associated with such transient events.
2. Events having significant changes in the fundamental frequency magnitude but of short duration. In such events, it is very difficult to extract voltage magnitude of transients. These are normally observed in fuse-cleared faults and self-extinguishing faults.
3. Events of very short duration (transients) for which the fundamental frequency magnitude does not offer important information. For this class, the higher frequency components of the signal must be considered for a thorough characterization and classification.
Based on waveform shape, power system transients, can be classified into
1. Oscillatory transients
2. Impulsive transients
3. Multiple transients
1) IMPULSIVE TRANSIENTS
An impulsive transient is defined as a sudden change in the steady state condition of voltage, current or both, that is unidirectional in polarity either positive or negative. Analysis of impulsive transients is done by their rise and decay times. Impulsive transients are damped quickly by the resistive circuit elements and do not propagate far from their source. Thus their effects are localized.Impulsive transients are common during lightning. Lightning stroke may appear directly or by indirect induction. When a lightning stroke hits a transmission line (direct stroke) an impulsive over voltage is induced. They have high magnitude. Lightning over voltage can also be induced by nearby strokes to the ground or between clouds. These over-voltages are of lower magnitude than those produced by direct strokes. Normally impulsive transient shows a sudden rise followed by an exponential decay. But in some cases, lightning transient shows a sudden rise followed by a sudden drop and an oscillation with relatively small amplitude.