Jul 2 – 6, 2018
Žofín Palace
Europe/Prague timezone

P2.4012 Flow control and its impact on avalanche dynamics in a basic transport experiment

Jul 3, 2018, 2:00 PM
2h
Mánes

Mánes

Speaker

Suying Jin

Description

See the full Abstract at http://ocs.ciemat.es/EPS2018ABS/pdf/P2.4012.pdf Flow control and its impact on avalanche dynamics in a basic transport experiment S. Jin1, B. Van Compernolle1, M. J. Poulos1, G. J. Morales1 1 Department of Physics and Astronomy, University of California, Los Angeles, United States Results of a basic heat transport experiment1,2 involving an offaxis heat source are presented. Experiments are performed in the Large Plasma Device (LAPD) at UCLA. A ringfshaped electron beam source injects low energy electrons (below ionization energy) along a strong magnetic feld into a prefexisting, large and cold plasma. The injected electrons provide an offaxis heat source that results in a long, hollow, cylindrical region of elevated plasma pressure embedded in a colder plasma, and far from the machine walls. The offaxis source is active for a period long compared to the density decay time, i.e. as time progresses the power per particle increases. Two distinct regimes are observed to take place, an initial regime dominated by avalanches, identifed as sudden intermittent rearrangements of the pressure profle, and a second regime dominated by sustained driftfAlfven wave activity following a global collapse of the density profle. The avalanches are triggered by the rapid growth of driftfAlfven waves. The data suggest that fows play a critical role in the dynamics, in particular in the onset of the avalanches through the interplay of the stabilizing fow shear and the destabilizing pressure gradient. The fows are imposed by the boundary condition at the ringfsource. This source has now been modifed from previous experiments to gain active control of the fows by controlling the bias between the emitting ring and surrounding carbon masks. A regime was found in which avalanches are absent. The new source also provides some control over the size and frequency of avalanches when present. Supported by the NSF grant PHY1619505, and performed at the Basic Plasma Science Facility, sponsored jointly by DOE and NSF. 1 B. Van Compernolle et al. Phys Rev. E 91, 031102 (2015) 2 B. Van Compernolle et al, Phys. Plasmas 24, 112302 (2017)

Primary author

Presentation materials

There are no materials yet.