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We present numerical results that provide an explanation of the occurrence of burst pulses and secondary streamers at intervals of 10–20 μs after a positive onset corona streamer pulse in air at atmospheric pressure. The calculations show that the positive charge left in the streamer channel, after a primary streamer has stopped, before reaching the cathode, will move away from the point causing a rising electric field at the anode. After 10 μs, this electric field is high enough, over a sufficient distance, that the conditions become suitable for a self-sustained discharge, and seed electrons near the anode cause a rapid increase in charge density. A secondary streamer then forms at the anode and propagates along the length of the original streamer channel in ∼300 ns, stopping at the same point as the primary streamer. The amplitude of the secondary current pulse is ∼10% of that of the primary current pulse. After each pulse, the remnant positive charge moves away from the point, creating the necessary conditions for further pulses; thus a series of pulses can be formed. The time between pulses is governed by the movement of the remnant positive charge away from the point. The remnant positive space-charge limits the size of the burst pulses which are considerably smaller than the primary pulse.
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Morrow et al. (2002) studied this question.
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