A measurement of the location of the X-ray source SCO X-1.
Location of X-ray source Sco X-1 determined by instrumented payload flown on stabilized Aerobee rocket
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Location of X-ray source Sco X-1 determined by instrumented payload flown on stabilized Aerobee rocket
Explosive limb flare of November 20, 1960 shown to coincide with beginning of radio and X-ray emission
X-ray and gamma ray astronomy, discussing observational methods, physical processes of generation, radiation intensity, etc
Neutron stars considered as origin of X-ray emission from Scorpius and Crab Nebula
Interstellar X-ray absorption edges due to K- shell photoionization of oxygen and neon, using element abundances and atomic photoelectric cross section data
Suprathermal X ray bremsstrahlung from proton-electron collisions in galactic and solar cosmic radiation
Solar X ray flare of July 7, 1966 with Explorer 33 satellite atributed to McMath plage region 8362, discussing solar and cosmic radio noise
X ray polarization from Sco X-1, noting spurious instrumental polarization due to cosmic ray anisotropy using X ray polarimeter
Scorpius XR-1 X ray emission spectra, discussing Fe emission line near 7 kev plasma models, supernova mass and cosmic abundance
X ray line emission from Sco X-1 using Monte Carlo estimates of spectral distribution of scattered photons in terms of Fe line and cosmic abundance
X rays from Sco XR-1 compared with galactic cosmic rays and solar Lyman alpha radiation to determine ionospheric ionization causing radio wave attenuation
X ray and H alpha emissions associated with solar proton flares, correlating rise time with solar cosmic rays
Solar wind X ray emission, investigating diffused cosmic ray origin and flow pattern models
Scorpius X-1 X ray line emission, discussing continuum and background counts and cosmic abundance of iron
Characteristics of energetic interplanetary particles and X rays produced by solar activity
Satellite-borne anisotropy and energy spectra measurement instruments for cosmic ray electrons and protons and solar and galactic X-rays
Gamma-ray and X-ray spectrometers carried in the service modules of the Apollo 15 and Apollo 16 spacecraft were employed for compositional mapping of the lunar surface. The measurements involved the observation of the intensity and characteristic energy distribution of gamma rays and X-rays emitted from the lunar surface. A large-scale compositional map of over 10 percent of the lunar surface was obtained from an analysis of the observed spectra. The objective of the X-ray experiment was to measure the K spectral lines from Mg, Al, and Si. Spectra were obtained and the data were reduced to Al/Si and Mg/Si intensity ratios and ultimately to chemical ratios. Analyses of the results have indicated (1) that the Al/Si ratios are highest in the lunar highlands and considerably lower in the maria, and (2) that the Mg/Si concentrations generally show the opposite relationship. The objective of the gamma-ray experiment was to measure the natural and cosmic-ray-induced activity emission spectrum. At this time, the elemental abundances for Th, U, K, Fe, Ti, Si, and O have been determined over a number of major lunar regions. Regions of relatively high natural radioactivity were found in the Mare Imbrium and Oceanus Procellarum regions.