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NASA Scientific and Technical Aerospace Reports

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which are particularly well suited to study electron emission as related to spacecraft charging. These measurements include<br />

electron-induced secondary <strong>and</strong> backscattered yields, spectra, <strong>and</strong> angular resolved measurements as a function of incident<br />

energy, species <strong>and</strong> angle, plus investigations of ion-induced electron yields, photoelectron yields, sample charging <strong>and</strong><br />

dielectric breakdown. Extensive surface science characterization capabilities are also available to fully characterize the<br />

samples in situ. Our measurements for a wide array of conducting <strong>and</strong> insulating spacecraft materials have been incorporated<br />

into the SEE Charge Collector Knowledge-base as a Database of Electronic Properties of Materials Applicable to Spacecraft<br />

Charging. This Database provides an extensive compilation of electronic properties, together with parameterization of these<br />

properties in a format that can be easily used with existing spacecraft charging engineering tools <strong>and</strong> with next generation<br />

plasma, charging, <strong>and</strong> radiation models. Tabulated properties in the Database include: electron-induced secondary electron<br />

yield, backscattered yield <strong>and</strong> emitted electron spectra; He, Ar <strong>and</strong> Xe ion-induced electron yields <strong>and</strong> emitted electron spectra;<br />

photoyield <strong>and</strong> solar emittance spectra; <strong>and</strong> materials characterization including reflectivity, dielectric constant, resistivity,<br />

arcing, optical microscopy images, scanning electron micrographs, scanning tunneling microscopy images, <strong>and</strong> Auger electron<br />

spectra. Further details of the instrumentation used for insulator measurements <strong>and</strong> representative measurements of insulating<br />

spacecraft materials are provided in other Spacecraft Charging Conference presentations. The <strong>NASA</strong> Space Environments <strong>and</strong><br />

Effects Program, the Air Force Office of <strong>Scientific</strong> Research, the Boeing Corporation, <strong>NASA</strong> Graduate Research Fellowships,<br />

<strong>and</strong> the <strong>NASA</strong> Rocky Mountain Space Grant Consortium have provided support.<br />

Author<br />

Spacecraft Charging; Electrical Properties; Spacecraft Construction Materials; Insulators; Universities; Utah; Knowledge<br />

Bases (Artificial Intelligence)<br />

20040111059 <strong>Aerospace</strong> Corp., Los Angeles, CA, USA<br />

An Empirical Low-Energy Ion Model of the Inner Magnetosphere<br />

Roeder, J. L.; Chen, M. W.; Fennell, J. F.; Friedel, R.; 8th Spacecraft Charging Technology Conference; March 2004; 15 pp.;<br />

In English; See also 20040111031<br />

Contract(s)/Grant(s): GC131165NGD; No Copyright; Avail: CASI; A03, Hardcopy<br />

Ion flux measurements by the CAMMICE/MICS <strong>and</strong> Hydra instruments on the <strong>NASA</strong> Polar satellite have been used to<br />

build empirical models of the ion environment at low energies in the Earth s inner magnetosphere. These models may be used<br />

to develop design <strong>and</strong> test specifications for spacecraft surface materials, which are susceptible to damage by the ions. The<br />

combination of the CAMMICE/MICS <strong>and</strong> Hydra models provide the ion flux at energies in the range 20 eV 200 keV as a<br />

function of position in the magnetosphere. For the 1 200 keV energy range, the H+ <strong>and</strong> O+ ion flux is estimated separately<br />

using the CAMMICE/MICS data. Average environments have been calculated for several sample orbital trajectories: a<br />

geosynchronous orbit <strong>and</strong> the orbits of several satellites in the Global Positioning System (GPS) constellation. At high energies<br />

(~100 keV) the flux estimates agree with corresponding estimates from the <strong>NASA</strong> AP-8 model, but the fluxes at low energies<br />

are larger than those extrapolated simply from AP-8. The CAMMICE/MICS model shows that H+ dominates the \g2 keV ion<br />

populations, but that the O+ flux becomes comparable to the H+ flux at ~1 keV. The st<strong>and</strong>ard deviation of both the ion <strong>and</strong><br />

electron flux was found to be 100 200% of the average value over the entire considered energy range. The average 1 200 keV<br />

O+ flux estimates for GEO appear very similar to the averages for GPS orbit, so that any material damage due to O+ ions in<br />

this energy range should be the same for the two orbits.<br />

Author<br />

Ions; Flux (Rate); Earth Magnetosphere; Design Analysis; Surface Properties; Geosynchronous Orbits<br />

20040111061 Kyoto Univ., Japan<br />

Feasibility Study of an Experimental Platform With Active Plasma Emission for Japan Experimental Module Onboard<br />

ISS<br />

Usui, Hideyuki; Funaki, I.; Nakayama, Y.; Tashima, H.; Kuninaka, H.; Okada, M.; 8th Spacecraft Charging Technology<br />

Conference; March 2004; 11 pp.; In English; See also 20040111031; No Copyright; Avail: CASI; A03, Hardcopy<br />

A Japanese experimental module (JEM) onboard the international space station (ISS) is directly exposed to space, hence<br />

if a plasma device is equipped to the exposed facility of JEM, many kinds of new plasma experiment become possible.<br />

However, there is a concern that by emitting plasmas, spacecraft charging <strong>and</strong> corresponding discharge will severely damage<br />

JEM <strong>and</strong> even ISS. We are proposing an experimental module for JEM in order to clarify such spacecraft-plasma interaction<br />

by operating a sub-scaled plasma-emitting floating body that can be deployed from JEM with some diagnostic equipment.<br />

Prior to the design of such a plasma experimental facility, strict assessment on the plasma environment around the plasma<br />

emitting device should be finished. We particularly focus on the transient response to the plasma emission. In this paper, the<br />

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