11.12.2012 Views

NASA Scientific and Technical Aerospace Reports

NASA Scientific and Technical Aerospace Reports

NASA Scientific and Technical Aerospace Reports

SHOW MORE
SHOW LESS

Create successful ePaper yourself

Turn your PDF publications into a flip-book with our unique Google optimized e-Paper software.

20040120944 <strong>NASA</strong> Langley Research Center, Hampton, VA, USA<br />

Preliminary Convective-Radiative Heating Environments for a Neptune Aerocapture Mission<br />

Hollis, Brian R.; Wright, Michael J.; Olejniczak, Joseph; Takashima, Naruhisa; Sutton, Kenneth; Prabhu, Dinesh; [2004];<br />

12 pp.; In English; AIAA Atmospheric Flight Mechanics Conference <strong>and</strong> Exhibit, 16-19 Aug. 2004, Providence, RI, USA<br />

Contract(s)/Grant(s): NAS2-99092; NAS1-00135; NCC1-02043; 320-10-00<br />

Report No.(s): AIAA Paper 2004-5177; No Copyright; Avail: CASI; A03, Hardcopy<br />

Convective <strong>and</strong> radiative heating environments have been computed for a three-dimensional ellipsled configuration which<br />

would perform an aerocapture maneuver at Neptune. This work was performed as part of a one-year Neptune aerocapture<br />

spacecraft systems study that also included analyses of trajectories, atmospheric modeling, aerodynamics, structural design,<br />

<strong>and</strong> other disciplines. Complementary heating analyses were conducted by separate teams using independent sets of<br />

aerothermodynamic modeling tools (i.e. Navier-Stokes <strong>and</strong> radiation transport codes). Environments were generated for a<br />

large 5.50 m length ellipsled <strong>and</strong> a small 2.88 m length ellipsled. Radiative heating was found to contribute up to 80% of the<br />

total heating rate at the ellipsled nose depending on the trajectory point. Good agreement between convective heating<br />

predictions from the two Navier-Stokes solvers was obtained. However, the radiation analysis revealed several uncertainties<br />

in the computational models employed in both sets of codes, as well as large differences between the predicted radiative<br />

heating rates.<br />

Author<br />

Aerocapture; Convective Heat Transfer; Radiative Heat Transfer; Neptune Atmosphere; Aerothermodynamics<br />

14<br />

GROUND SUPPORT SYSTEMS AND FACILITIES (SPACE)<br />

Includes launch complexes, research <strong>and</strong> production facilities; ground support equipment, e.g., mobile transporters; <strong>and</strong> test chambers<br />

<strong>and</strong> simulators. Also includes extraterrestrial bases <strong>and</strong> supporting equipment. For related information see also 09 Research <strong>and</strong><br />

Support Facilities (Air).<br />

20040111057 Jet Propulsion Lab., California Inst. of Tech., Pasadena, CA, USA<br />

Comparison of Classical <strong>and</strong> Charge Storage Methods for Determining Conductivity of Thin Film Insulators<br />

Swaminathan, Prasanna; Dennison, J. R.; Sim, Alec; Brunson, Jerilyn; Crapo, Eric; Frederickson, A. R.; 8th Spacecraft<br />

Charging Technology Conference; March 2004; 20 pp.; In English; See also 20040111031; No Copyright; Avail: CASI; A03,<br />

Hardcopy<br />

Conductivity of insulating materials is a key parameter to determine how accumulated charge will distribute across the<br />

spacecraft <strong>and</strong> how rapidly charge imbalance will dissipate. Classical ASTM <strong>and</strong> IEC methods to measure thin film insulator<br />

conductivity apply a constant voltage to two electrodes around the sample <strong>and</strong> measure the resulting current for tens of<br />

minutes. However, conductivity is more appropriately measured for spacecraft charging applications as the ‘decay’ of charge<br />

deposited on the surface of an insulator. Charge decay methods expose one side of the insulator in vacuum to sequences of<br />

charged particles, light, <strong>and</strong> plasma, with a metal electrode attached to the other side of the insulator. Data are obtained by<br />

capacitive coupling to measure both the resulting voltage on the open surface <strong>and</strong> emission of electrons from the exposed<br />

surface, as well monitoring currents to the electrode. Instrumentation for both classical <strong>and</strong> charge storage decay methods has<br />

been developed <strong>and</strong> tested at Jet Propulsion Laboratory (JPL) <strong>and</strong> at Utah State University (USU). Details of the apparatus,<br />

test methods <strong>and</strong> data analysis are given here. The JPL charge storage decay chamber is a first-generation instrument, designed<br />

to make detailed measurements on only three to five samples at a time. Because samples must typically be tested for over a<br />

month, a second-generation high sample throughput charge storage decay chamber was developed at USU with the capability<br />

of testing up to 32 samples simultaneously. Details are provided about the instrumentation to measure surface charge <strong>and</strong><br />

current; for charge deposition apparatus <strong>and</strong> control; the sample holders to properly isolate the mounted samples; the sample<br />

carousel to rotate samples into place; the control of the sample environment including sample vacuum, ambient gas, <strong>and</strong><br />

sample temperature; <strong>and</strong> the computer control <strong>and</strong> data acquisition systems. Measurements are compared here for a number<br />

of thin film insulators using both methods at both facilities. We have found that conductivity determined from charge storage<br />

decay methods is 102 to 104 larger than values obtained from classical methods. Another Spacecraft Charging Conference<br />

presentation describes more extensive measurements made with these apparatus. This work is supported through funding from<br />

the <strong>NASA</strong> Space Environments <strong>and</strong> Effects Program <strong>and</strong> the USU Space Dynamics Laboratory Enabling Technologies<br />

Program.<br />

Author<br />

Spacecraft Charging; Electric Charge; Capacitance<br />

25

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!