70th Annual Gaseous Electronics Conference
Volume 62, Number 10
Monday–Friday, November 6–10, 2017;
Pittsburgh, Pennsylvania
Session QR2: Diagnostics III
8:00 AM–9:30 AM,
Thursday, November 9, 2017
Room: Duquesne
Chair: Vladimir Demidov, West Virginia University
Abstract ID: BAPS.2017.GEC.QR2.3
Abstract: QR2.00003 : Electric Field Measurements in Nanosecond Pulse Discharges in Air over Solid and Liquid Dielectric Surfaces
8:30 AM–9:00 AM
Preview Abstract
Abstract
Author:
Igor Adamovich
(Ohio State University)
Electric field in nanosecond pulse discharges in ambient air is measured by
picosecond four-wave mixing, with absolute calibration by a known
electrostatic field. The measurements are done in a discharge between two
parallel cylinder electrodes covered by quartz tubes, and in a discharge
between a razor edge high-voltage electrode and a plane grounded electrode
covered by a quartz plate or by a layer of distilled water. In the positive
polarity discharge between the parallel cylinders, peak electric field, 140
kV/cm, considerably exceeds DC breakdown threshold. In the negative polarity
discharge between the razor blade and quartz surface, the field follows the
applied voltage until ``forward'' breakdown occurs, after which the field in
the plasma decays due to charge separation. When the applied voltage is
reduced, the field reverses direction and increases again, until the
``reverse'' breakdown occurs, producing a secondary reduction in the field.
Spatially resolved measurements show that the discharge develops as a
surface ionization wave. Measurements of electric field vector components
demonstrate that the vertical field in the wave peaks ahead of the
horizontal field. Behind the wave, the vertical field remains low, while the
horizontal field is gradually reduced. In the discharge over water surface,
electric field is measured for both positive and negative pulse polarities,
with durations of about 10 ns and about 100 ns, respectively. In the
positive polarity pulse, breakdown threshold is 85 kV/cm, and no field
reversal is detected during the voltage reduction. In the negative polarity
pulse, breakdown occurs at 30 kV/cm, due to much longer pulse duration, and
the field reverses direction when the voltage is reduced. After the pulse,
the residual field over quartz and water surfaces decays on a microsecond
time scale, due to surface charge neutralization by charge transport from
the plasma. The results demonstrate considerable potential of the present
technique for electric field measurements in atmospheric pressure
discharges, providing quantitative insight into charge transport and plasma
kinetics near plasma-liquid interface.
To cite this abstract, use the following reference: http://meetings.aps.org/link/BAPS.2017.GEC.QR2.3