Aroh Barjatya Dr. Charles M. Swensoncse.usu.edu/foraffiliates/presentations_07/ArohBarjarta.pdf ·...
Transcript of Aroh Barjatya Dr. Charles M. Swensoncse.usu.edu/foraffiliates/presentations_07/ArohBarjarta.pdf ·...
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Spacecraft Charging
Aroh Barjatya Dr. Charles M. Swenson Utah State University
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Outline
Basics of spacecraft surface charging and langmuir probes Overview of various sounding rocket programs undertaken at Utah State Data from SAL rocket flight. Triboelectric charging. FPMU data results and charging on ISS.
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Spacecraft Charging: Basic
The spacecraft surface potential is a function of the net current flow to/from the spacecraft surface
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Current Collection IV Curve
Ion Saturation region:
Ions attracted, electrons repelled Electron Retardation region
Electron saturation region:
Electrons attracted, ions repelled
Floating Potential Plasma Potential
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Different Surface Geometries
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Spacecraft Charging Other Currents
T B BSE SE PH I E I V I (V) I (V) I V I (V) [I (V) I = + + + + − )] ( ) ( I E = Electron Current I I = Ion Current I PH =Photoelectron I SE =Secondary Electron I BSE =Back Scatter I B =Beam/Ion thruster
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Past Sounding Rocket Programs
Four Sequential Rockets: July1 2003, Wallops Island Study descending sporadicE layers
EWINDS
Two Rocket Flights: August 7 th and 15 th 2004, Kwajalein Atoll Study precursors to equatorial spreadF
EQUIS II SAL
Flight: 19th Feb 1998, Puerto Rico 2009 LT Study sporadic sodium layers
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Upcoming Sounding Rocket Programs
Flight in Fall 2007 Wallops Island
Tropical Storms Mission
Study mid latitude spreadF caused by tropical weather systems
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Sudden Atom Layer (SAL)
Flight: 19th Feb 1998, Puerto Rico 2009 LT Investigation of sporadic sodium layers Dust Detector
Langmuir Fast Temperature Probe (FTP) Floating Potential Probes
Swept Impedance Probe
DC Langmuir Probe (DCP)
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SAL Mission
Max. Altitude: 115 Km 5 Km thick sodium layer peaking at 94 Km Positively charged dust layer just below the sodium layer at 92 Km
Atoms
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SAL Electron Density Profiles
Charged Dust Layer
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The SporadicE Layer
(a) DCP Instrument Malfunction ? (b) Shock wave related effect ? (c) Vehicle Surface Charging ?
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Reasons for low DCP response (a) Instrument Malfunction ?
DCP worked above and below the layer
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Reasons for low DCP response (b) Effect of shock wave ?
Ambient Neutral Density: 0.6E+20 Density reduction factor around the DCP section of the boom: 3
Downleg 8º to Ram
Upleg 2º to Ram SIP
DCP
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Reasons for low DCP response (c) Vehicle Charging ?
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Reasons for low DCP response (c) Vehicle Charging ?
Triboelectric Charging: When two metal surfaces come in contact with each other and then separate, the metal surface with lower work function gets charged positive and the other surface gets charged negative
Work function: Aluminium: 4.2eV Sodium: 2.36eV è Dust source of electron current
Dust is modeled as RAM current
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Reasons for low DCP response (c) Vehicle Charging ?
Observed Dataset Triboelectric Charging Simulation Results
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Floating Potential Measurement Unit
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Floating Potential Measurement Unit
130 cm
150 cm
Wide Langmuir Probe (WLP)
Sweep 20 to +80 volts Plasma Impedance
Probe (PIP)
Narrow Langmuir Probe (NLP)
Sweep 5 to +5 volts around Vf
Floating Potential Probe (FPP)
Electronics
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Floating Potential Measurement Unit
Photovoltaic Cell Gap Geometry
After Miktarian et. al. IAC World Space Congress 2002 Houston, Texas
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Floating Potential Measurement Unit
Eclipse Sun Eclipse Sun
Data Dropout
Time
Fp (volts)