Differential electron spectra in the radiation belts in 10 energy intervals from 0.17 to 4.5 Mev have been obtained from a directional electron spectrometer on satellite 1964-45A. The satellite was launched on August 14, 1964, into a near polar orbit with a 3765-km apogee and a 270-km perigee. Typical quiet-time data of August 15, 1964, are presented. A soft and a hard component both are clearly present in the electron spectra for 1.7 400 km, are fit by exponential energy distributions with characteristic energies of 0.9±0.5 Mev for the hard component and 0.2 to 0.07 Mev for the soft component. The hard component is the remnant of fission electrons injected by the July 9, 1962, high-altitude nuclear test. The soft component becomes softer as L increases, and may largely be due to cosmic-ray albedo neutron decay. For 3.5 < L < 8 the portions of the differential spectra above 0.5 Mev are fit by single exponential distributions with characteristic energies of 0.6 to 0.2 Mev, becoming generally softer as L increases. The quiet-time outer zone electrons peak at lower L for higher energies. The magnetic moments of the electrons at the peaks change along computed inward drift trajectories, which conserve the first two adiabatic invariants. Consequently, this diffusion is a dominant source of these electrons only if a comparable loss process is present. Generally, there are no pronounced changes in quiet-time electron spectra with altitude along a field line in either the outer or inner zones. However, in the outer zone the flux of 0.2-Mev electrons increases by up to a factor of 2 as B changes from 0.24 to 0.1 gauss.
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