COMPOSITE MATERIALS IN ERECTABLE SPACE STRUCTURES - ECHO SATELLITES
Discussion of composite materials in erectable space structures, and experimental results on the echo satellites
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Discussion of composite materials in erectable space structures, and experimental results on the echo satellites
Echo II satellite communication capability
Echo II satellite observational data showing no change in apparent cross section one year after launch
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Experiments with Echo II satellite to determine its capability as passive communications device and study shape and surface as function of time
This paper describes an empirical study of the basic mechanisms by which electrons precipitate from the geomagnetic field to produce 'auroral X rays' during periods of geomagnetic activity. The study was based on data obtained by the Echo satellites. Echo I, launched in 1970, injected 40 keV, 0.1 amp electron pulses at low latitude (L ? 2.6) and successfully measured the returning pulses from the conjugate region. Electric fields and multiple Coulomb scattering were studied. Echo II, launched in 1972 from high latitude (L ? 8) studied the interaction of the beams with background radiation and the detailed motion of the beams near the rocket. Evidence for a beam plasma instability was obtained. Echo III launched in April 1974, (L ? 5.5) detected a series of conjugate echoes during the presence of a strong convective field in the magnetosphere. It was shown that the electric field measurement in the ionosphere using the incoherent backscatter radar and detectors on the rocket was transferred to the equatorial plane as though field lines were equipotentials.
Simultaneous tracking of echo i satellite for geodetic purposes - celestial triangulation
Photometric measurements of Echo I satellite on specular degradation of aluminized Mylar surface during orbit
Echo ii communications satellite launching
Comparison of theory and observation of the echo I satellite
Charge-up to maintain shape of echo type satellites
Observations of the Echo I balloon satellite have been compared with a theory including the following perturbing effects: (1) solar radiation pressure; (2) lunar and solar gravitation; (3) second, third, and fourth harmonics of the earth's gravitational potential; and (4) atmospheric drag. With a set of orbital elements at the 26th day of the lifetime of the satellite, it was possible to match the observational data to 180 days with root mean square residuals as follows: Delta-a = 17.9 km, Delta-e = 0.0021, Delta-i = 0.0177 deg., Delta-omega = 1.1231 deg., Delta-Omega = 0.4821 deg., Delta-perigee height = 7.50 km. No differential correction has been applied as yet. Values of atmospheric density between 1500 and 930 km, assuming neutral drag effects only, have been inferred from the orbital data. The connection between solar activity and drag is also examined. As the Echo I perigee height continues to oscillate between 900 and 1500 km, more valuable orbital data will be obtained and atmospheric properties will be deduced. Further refinements in the mathematical model, especially in a time-dependent model atmosphere, should bring a substantial reduction in the residuals of the observations.
Design, fabrication, packaging, and test methods used in Echo II satellite
Photometric measurements of Echo I satellite surface characteristics
Radio beacon telemetry system for measuring orbital performance of Echo II satellite, including internal pressure and skin temperature
Geodetic junction of France and North Africa determined by synchronized photographs taken from Echo I satellite
Orbital behavior of echo i satellite and its rocket casing during its first 500 days
Signal transmission from U.S.S.R. to United Kingdom via Echo II communications satellite