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NASA Scientific and Technical Aerospace Reports

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stabilized GEO spacecraft via an improved radiative force model. The macro-model approach for the Tracking <strong>and</strong> Data Relay<br />

Satellites (TDRSS), models the spacecraft area <strong>and</strong> reflectivity properties using an assembly of flat plates to represent the<br />

spacecraft components. This ‘box-wing’ approach has been adapted for the UNIX version of the Goddard Trajectory<br />

Determination System (GTDS) at the MIT/Lincoln Laboratory. This thesis presents background <strong>and</strong> mathematical<br />

development of the macro-model approach. This thesis also describes software development <strong>and</strong> testing, including<br />

incorporation of a one-panel spacecraft model along with the full macro-model. A model for Earth albedo <strong>and</strong> Earth infrared<br />

radiation <strong>and</strong> related software development is also described. Additionally, this thesis gives details about the TDRSS macromodel,<br />

<strong>and</strong> explains the development of a macromodel for the <strong>NASA</strong> Geosynchronous Operational Environmental Satellites<br />

(GOES) I-M spacecraft. Results of simulated data testing using the improved radiative force models are presented. The real<br />

data testing detailed in this thesis is an investigation into improving GEO orbit determination using the new force models along<br />

with observation data from the Space Surveillance Network (SSN). For the TDRSS spacecraft, HANDS optical observations<br />

are used in conjunction with the SSN data. NOAA ranging observations are included in some of the tests for the GOES-10<br />

spacecraft. The spacebased visible (SBV) observation model has also been incorporated into GTDS, <strong>and</strong> SBV observations<br />

are included in the orbit determination testing. The results of this thesis give a better underst<strong>and</strong>ing of the process of<br />

determining precise orbits for GEO spacecraft with the box-wing model <strong>and</strong> SSN observation7<br />

DTIC<br />

Artificial Satellites; Earth Orbits; Geosynchronous Orbits; Orbit Determination; Solar Radiation<br />

20040111738 Pittsburgh Univ., Pittsburgh, PA<br />

Acquisition of Hyperthermal Atomic Oxygen Source<br />

Yang, Judith C.; Aug. 11, 2004; 7 pp.; In English<br />

Contract(s)/Grant(s): F49620-02-1-0198<br />

Report No.(s): AD-A425922; AFRL-SR-AR-TR-04-0446; No Copyright; Avail: CASI; A02, Hardcopy<br />

The objective of this grant was the acquisition of a hyperthermal atomic oxygen (AO) source that is of critical importance<br />

to a Multi-University Research Initiative (MURI) on the fundamental mechanisms of materials degradation in the low earth<br />

orbit (LEO). (&quot;Simulations of Fundamental Degradation Process in Space Environments&quot;, PI: J. C. Yang, MURI<br />

Contract #: F49620-O1-1-0336). A Physical Sciences, Inc. (PSI) FASTTM (Fast Atom Sample Tester) source was specially<br />

designed for portability with an ultra-high vacuum exposure chamber <strong>and</strong> delivered to University of Pittsburgh in October<br />

2003. The portability of this FASTTM AO source allows the utilization of unique experimental tools located at different sites.<br />

This system has now been improved so that the best base vacuum is 4x1O(-9) torr. A room temperature sample stage has been<br />

built, a dual head quartz crystal monitor (QCM) system has been installed for in situ weight loss. A sensitive Mettler balance<br />

was purchased in order to measure total weight changes. All of these items have been installed <strong>and</strong> working since May 2004.<br />

Present experiments are being performed on Si, Al, Ag <strong>and</strong> Au single crystals <strong>and</strong> thin films.<br />

DTIC<br />

Earth Orbits; Oxygen; Oxygen Atoms<br />

20040120869 Morgan Research Corp., Huntsville, AL, USA, <strong>NASA</strong> Marshall Space Flight Center, Huntsville, AL, USA<br />

Atmospheric Models for Aeroentry <strong>and</strong> Aeroassist<br />

Justus, C. G.; Duvall, Aleta; Keller, Vernon W.; June 15, 2004; 8 pp.; In English; 2nd Planetary Probe Workshop, 23-26 Aug.<br />

2004, Moffett Field, CA, USA; Original contains color illustrations<br />

Contract(s)/Grant(s): NNM04AA02C; No Copyright; Avail: CASI; A02, Hardcopy<br />

Eight destinations in the Solar System have sufficient atmosphere for aeroentry, aeroassist, or aerobraking/aerocapture:<br />

Venus, Earth, Mars, Jupiter, Saturn, Uranus, <strong>and</strong> Neptune, plus Saturn’s moon Titan. Engineering-level atmospheric models<br />

for Earth, Mars, Titan, <strong>and</strong> Neptune have been developed for use in <strong>NASA</strong> s systems analysis studies of aerocapture<br />

applications. Development has begun on a similar atmospheric model for Venus. An important capability of these models is<br />

simulation of quasi-r<strong>and</strong>om perturbations for Monte Carlo analyses in developing guidance, navigation <strong>and</strong> control algorithms,<br />

<strong>and</strong> for thermal systems design. Characteristics of these atmospheric models are compared, <strong>and</strong> example applications for<br />

aerocapture are presented. Recent Titan atmospheric model updates are discussed, in anticipation of applications for trajectory<br />

<strong>and</strong> atmospheric reconstruct of Huygens Probe entry at Titan. Recent <strong>and</strong> planned updates to the Mars atmospheric model, in<br />

support of future Mars aerocapture systems analysis studies, are also presented.<br />

Author<br />

Atmospheric Models; Solar System; Aeroassist; Aerobraking; Aerocapture; Guidance (Motion)<br />

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