1998
DOI: 10.1103/physreve.57.7066
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Positive streamer in a weak field in air: A moving avalanche-to-streamer transition

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Cited by 153 publications
(187 citation statements)
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“…This condition describes the effect of the anode space-charge layer. The commonly used approach to represent initial conditions for the equation system (1) is the assumption that a quasi-neutral layer or 'plasma spot' exists in the gap, which initiates the discharge [1,3,4]. This appears to be artificial because the location of charges and their densities are set arbitrarily.…”
Section: Boundary and Initial Conditionsmentioning
confidence: 99%
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“…This condition describes the effect of the anode space-charge layer. The commonly used approach to represent initial conditions for the equation system (1) is the assumption that a quasi-neutral layer or 'plasma spot' exists in the gap, which initiates the discharge [1,3,4]. This appears to be artificial because the location of charges and their densities are set arbitrarily.…”
Section: Boundary and Initial Conditionsmentioning
confidence: 99%
“…Both results show significant deviation from experimental data as presented above. Simulations performed for a gap length of 10 mm have shown the ability of the streamer to propagate in a weaker field [3,13]. But it is difficult to relate the background field strength to the streamer properties in [3] because of the non-uniformity of the electric field.…”
Section: Introductionmentioning
confidence: 99%
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“…We consider the classical fluid model for air given by drift-diffusion equations self-consistently coupled with Poisson's equation [11,12]: ∂ t n e + ∇ · (n e v e ) − ∇ · (D e ∇n e ) = n e α|v e | − n e η|v e | − n e n p β ep + n n γ + S ph ,…”
mentioning
confidence: 99%