Contribution to the study of traveling-wave-type plasma accelerators contribution a l'etude des accelerateurs de plasma a ondes progressives
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Search indexed NASA NTRS and DOE OSTI research on propulsion, heat transfer, battery materials and energy systems. Follow report and document links to the original sources.
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Vibration frequency and damping behavior of Stored Tubular Expendable Member /STEM/ booms
Conduction band structure in n-type strontium titanate investigated by measuring oscillatory magnetoresistance in high magnetic fields
Excited carbon dioxide diffusion coefficient and wall deexcitation probability, attributing difference from viscosity measurement to energy transfer in collisions
Double precision ephemeris package for IBM 360/95 in FORTRAN with stored planetary positions and velocities
Chondrite meteorite fall /1969/ in Mexico, noting opaque and microcrystalline matrices and gamma rays from short lived isotopes
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Determining exit conditions that result when heat is withdrawn from rocket thrust chamber and added to gas flow in nozzle
Stretch Yo-Yo mechanism for reducing initial spin rate of space vehicle
Transition probabilities computed for spectral lines due to magnetic quadrupole radiation, discussing deexcitation of excited atoms in solar corona
Flare rising from behind solar limb deoccultated by simultaneous recording by OSO III X ray detector and photoheliograph
Linear dynamic system recursive state estimation for set-membership description of uncertainty under unknown input disturbances and observation errors
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Remote sensor data from a NASA Convair 990 radar flight and Mission 101 and 105 have been interpreted and evaluated. Based on interpretation of the remote sensor data, a geologic map has been prepared and compared with a second geologic map, prepared from interpretation of both remote sensor data and field data. Comparison of the two maps gives one indication of the usefulness and reliability of the remote sensor data. Color and color infrared photography provided the largest amount of valuable information. Multiband photography was of lesser value and side-looking radar imagery provided no new information that was not available on small scale photography. Thermal scanner imagery proved to be a very specialized remote sensing tool that should be applied to areas of low relief and sparse vegetation where geologic features produce known or suspected thermal contrast. Low sun angle photography may be a good alternative to side-looking radar imagery but must be flown with critical timing.
There are no author-identified significant results in this report.
In photoelectric observations of a series of occultations of the Jovian satellite Europa by the Jovian satellite Io it was observed that increasingly larger fractions of the north polar region of the former were covered at mid-event with each successive occultation. One of the possible explanations of the observed phenomena involves the existence of a bright north polar cap for Europa. The reported investigation shows that a second explanation may be more plausible. This explanation is related to the possibility that at mid-event the projected minimum distance between the centers of the satellites was smaller than predicted by Sampson's theory.
The paper describes a Cerenkov detector system designed to obtain abundances and energy spectra of cosmic ray nuclei above charge 12 and above 350 MeV/nucleon. The detector system consists of three pulse ionization chambers, a Lucite Cerenkov counter and a plastic scintillation-counter hodoscope. The data analysis follows from the standard dE/dx-C technique. It is shown that by using the relativistic ionization rise, the resolution and pulse height corresponding to charged particles of Beta ? 1 in Cerenkov detectors can be determined. Least-squares-fit procedures are used to obtain area and time variations of detector response from flight data and to extract elemental abundances from data with charge resolution of roughly 0.3 charge units.
Frequently a photograph received from a spacecraft will be smeared by some process, e.g., by camera motion. Algebraically such smearing can be represented as p = sigma f, where sigma is the true picture, p is the received picture, and f is the smearing function. (p, sigma, and f are polynomials in two variables x and y.) Thus, in principle, sigma can be recovered by multiplying p by 1/f. However, there are problems involved in computing 1/f. Some of these problems are investigated.