Electrical and Computer Engineering ETDs
Publication Date
Winter 1-20-2023
Abstract
A coronal mass ejection or a high-altitude nuclear explosion can produce an artificial radiation belt containing high-energy electrons (~1MeV) in the Earth's magnetosphere. Some electrons become trapped in the Earth's magnetic field and have enough energy to severely damage or destroy nearly all lower-earth orbit (LEO) satellites. Over the years, there has been much interest in using a space-borne dipole antenna to inject very low frequency (VLF) whistler waves (3-30kHz) along the Earth's magnetic field lines. The whistler waves precipitate the electrons from the magnetosphere through a wave-particle interaction called pitch-angle scattering. However, because the magnetosphere is composed of plasma, a charged antenna will form a nonlinear plasma sheath around its surface. The plasma sheath changes the input impedance of the antenna, reducing efficiency. This research uses a fully kinetic electrostatic curvilinear particle-in-cell (CPIC) code to characterize the sheath and understand its effects on the input impedance of the antenna.
Keywords
dipole, magnetosphere, sheath, plasma, particle-in-cell, whistler wave
Document Type
Dissertation
Language
English
Degree Name
Electrical Engineering
Level of Degree
Doctoral
Department Name
Electrical and Computer Engineering
First Committee Member (Chair)
Dr. Mark Gilmore
Second Committee Member
Dr. Edl Schamiloglu
Third Committee Member
Dr. Quinn Marksteiner
Fourth Committee Member
Dr. Paul Song
Recommended Citation
Shipman, Kevin A.. "Particle-in-Cell Simulations of Plasma Sheath Effects on a Whistler Wave Electric Dipole Antenna Operating in the Magnetosphere." (2023). https://digitalrepository.unm.edu/ece_etds/587