Guiding effect of runaway electrons in atmospheric pressure nanosecond pulsed discharge: mode transition from diffuse discharge to streamer

In this study, the role of runaway electrons (RAEs) during the pulsed breakdown in the atmosphere is investigated. Nanosecond pulsed discharge (NPD) is driven by high-voltage pulses between blade-to-plate electrodes (with the blade as the cathode). RAEs with an energy higher than 10 keV are selected by a titanium foil with a thickness of 1 mu m and detected by a beam collector with a front of about 50 ps. The temporal-spatial evolution of the electric field over the NPD period is measured using electric field induced second harmonic method adopting a picosecond pulsed laser. It is verified that the current amplitude of RAEs decreases drastically with the voltage amplitude V (p) and the peak electric field at the front of the ionization wave formed during the breakdown of NPD plays a key role in maintaining the runaway state of electrons. With single-shot discharge imaging, it is observed that the discharge is initially in a diffuse mode near the cathode, while it branches and transits into streamers, which can be either synchronously propagating multi streamers (with a high V (p)) or certain dominant streamers (with a low V (p)). Using particle-in-cell Monte-Carlo collision simulation, a similar mode transition of diffuse to streamer is observed with RAEs emitted from the cathode and it is illustrated that the flux of RAEs controls the pre-ionization degree and further dictates branching and non-uniformity of discharge, which qualitatively explains the experimental observation. It is proposed that an enhanced RAEs emission would produce a large volume diffuse discharge at atmospheric pressure.