Abstract
Using the Magneto-Plasma-Dynamic Arc Jet (MPD Arc Jet) device, the plasma-material interaction during simulated plasma disruption was experimentally investigated. To clarify the effects of the evaporation, the isotropic graphite was used as a target. The thermal conductivity of the isotropic graphite was much higher than that of the pyrolytic graphite, resulting in smaller evaporation. The light intensity distribution during the simulated disruption for the isotropic graphite was quite different from that for the pyrolytic graphite. (author)
Sukegawa, Toshio;
Madarame, Haruki;
Okamoto, Koji
[1]
- Tokyo Univ., Tokai, Ibaraki (Japan). Nuclear Engineering Research Lab.
Citation Formats
Sukegawa, Toshio, Madarame, Haruki, and Okamoto, Koji.
Evaporative behavior of carbon with MPD Arc Jet.
Japan: N. p.,
1996.
Web.
Sukegawa, Toshio, Madarame, Haruki, & Okamoto, Koji.
Evaporative behavior of carbon with MPD Arc Jet.
Japan.
Sukegawa, Toshio, Madarame, Haruki, and Okamoto, Koji.
1996.
"Evaporative behavior of carbon with MPD Arc Jet."
Japan.
@misc{etde_489223,
title = {Evaporative behavior of carbon with MPD Arc Jet}
author = {Sukegawa, Toshio, Madarame, Haruki, and Okamoto, Koji}
abstractNote = {Using the Magneto-Plasma-Dynamic Arc Jet (MPD Arc Jet) device, the plasma-material interaction during simulated plasma disruption was experimentally investigated. To clarify the effects of the evaporation, the isotropic graphite was used as a target. The thermal conductivity of the isotropic graphite was much higher than that of the pyrolytic graphite, resulting in smaller evaporation. The light intensity distribution during the simulated disruption for the isotropic graphite was quite different from that for the pyrolytic graphite. (author)}
place = {Japan}
year = {1996}
month = {Oct}
}
title = {Evaporative behavior of carbon with MPD Arc Jet}
author = {Sukegawa, Toshio, Madarame, Haruki, and Okamoto, Koji}
abstractNote = {Using the Magneto-Plasma-Dynamic Arc Jet (MPD Arc Jet) device, the plasma-material interaction during simulated plasma disruption was experimentally investigated. To clarify the effects of the evaporation, the isotropic graphite was used as a target. The thermal conductivity of the isotropic graphite was much higher than that of the pyrolytic graphite, resulting in smaller evaporation. The light intensity distribution during the simulated disruption for the isotropic graphite was quite different from that for the pyrolytic graphite. (author)}
place = {Japan}
year = {1996}
month = {Oct}
}