词条 | ultraviolet astronomy |
释义 | ultraviolet astronomy ![]() Ultraviolet astronomy became feasible with the advent of rockets (rocket) capable of carrying instruments above Earth's (Earth) atmosphere, which absorbs most electromagnetic radiation of ultraviolet wavelengths (i.e., roughly 100 to 4,000 angstroms) from celestial sources. Much radiation is lost even at the highest altitudes that balloons can reach. During the 1920s, unsuccessful attempts were made to photograph the Sun's ultraviolet spectrum from balloons; not until 1946 did a rocket-borne camera succeed in doing so. Since the early 1960s the United States and several other countries have placed in Earth orbit unmanned satellite observatories (satellite observatory) carrying telescopes (telescope) with optical surfaces specially coated for high ultraviolet reflectivity. These include eight Orbiting Solar Observatories, launched from 1962 to 1975 by the U.S. National Aeronautics and Space Administration (NASA), which enabled astronomers to obtain thousands of ultraviolet spectra of the Sun's corona. Another series of U.S. satellites, known as Orbiting Astronomical Observatories (Orbiting Astronomical Observatory), in service from 1968 to 1981, permitted the study of the interstellar medium and remote stars (star) in the spectral range of 1,200 to 4,000 angstroms. ![]() |
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