EE 350 Radioscience Seminar
Professor Umran S. Inan
Winter 2004-2005
Date: Wednesday, February 23, 2005
Time: 4:15 PM – Refreshments at 4:00
Location: Sloan Mathematics
Center (Building 380), Room 380Y
Generation of ULF Waves in Radiation Belts by Chemical Release
Dr. Gurudas Ganguli Plasma Physics Division, Naval Research Laboratory
Abstract
In 1970 Brice [1] noted that it is possible to artificially enhance the energetic particle precipitation rate in the radiation belts by
cold plasma injection. Since then creation of plasma clouds in the radiation belts via chemical release has been studied both theoretically and experimentally but these
studies were mainly restricted to high altitudes (L ~ 4 - 5). We have examined the possibility of generating electromagnetic ion-cyclotron (ULF) waves by chemical
release at inner radiation belt altitudes (L < 2). We show that ionization of the released chemicals can result in the formation of an ion ring distribution
perpendicular to the ambient magnetic field in a manner that is similar to the comet-solar wind interaction. Such an ion distribution is highly unstable to both
electrostatic and electromagnetic instabilities. We have compared the possible electrostatic and electromagnetic instabilities that may be generated by such ion
distributions, assessed their properties, and quantified the parametric domains and conditions where particular modes dominate. The electrostatic ion-cyclotron modes of
the ion ring distribution can be stabilized by Landau damping of the ambient plasma. This allows the electromagnetic ion-cyclotron modes to dominate since they are not
subjected to Landau damping. The quasi-stationary turbulent spectra can be sustained by fresh supply of ring ions through ionization. The threshold density and other
parameters that result in predominance of electromagnetic modes and their role in particle loss mechanisms in the radiation belts will be discussed.
* This work is supported by ONR
[1] Brice, N., Artificial enhancement of energetic particle precipitation through cold plasma injection, J. Geophys. Res., 75, 4890, 1970.
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