Proposal for galactic and solar cosmic ray studies on OGO E and G
Integrated set of three detectors for galactic and solar ray studies of OGO-E and OGO-G
SEARCH · Engineering Papers
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.
Quote a phrase for an exact phrase match. Source license links do not imply unrestricted reuse.
Integrated set of three detectors for galactic and solar ray studies of OGO-E and OGO-G
Electron density profiles of Nike-Apache rocket observations of nitric oxide ionization by Lyman alpha radiation in E region at sunrise
Diurnal variation of sporadic E at high latitude as function of geomagnetic activity
Geomagnetic field variations in temperate zone sporadic E layer according to wind-shear theory
Positive ion layers in E region explained by wind shear theory, obtaining steady state solutions for simple model
Electron and ion temperature changes in sporadic E layer based on wind shear theory, using energy equation
Lower E-region positive ion concentrations measured at time of declining solar activity by rocket installed mass spectrometer
Ionospheric E region dynamical processes, discussing energy phenomena of planetary waves, tidal oscillations and gravity waves
Electron temperature observation in E region with Langmuir probes on Nike Apache rockets, discussing solar radiation effect
Computer program for OGO-E vehicle response analysis to transient loading during Atlas booster burnout
OGO-E plasma spectrometers for measuring total flux below 12 kev and energy /spectral density/ of plasma
Analysis of wind and electron density profiles of E-region obtained from Nike-Apache rockets launched 22 Feb. 1968
Channel multiplier spectrometer for low energy electrons and protons at synchronous altitude on ATS-E satellite
Plasma tocopherol concentrations and vitamin E deficiency in dogs, noting pathologic changes in smooth muscle, central nervous system, skeletal muscle and retina
Particle flux densities of radiation belts for atmospheric explorer missions C, D, and E
Neutral wind effects on redistribution of E region ionization and recombination, comparing electron density profiles to vertical ion drift velocities
We have calculated the polarization fraction of the Lyman-alpha radiation emitted in e/-/-H/1s/ collisions using the Glauber, Born, and various Vainshtein approximations, and have compared these predictions with observation. We find that the Born, Glauber and all forms of the Vainshtein yield results which are very close to each other and to the data in the energy range from 30 to 700 eV. The comparatively small differences between the various approximations are detailed in the text; also, the reason for the close agreement of the predicted polarization fractions - although the computed 1s-2p total and differential cross sections are not so close - is explained. With respect to the Glauber approximation, the importance of computing the phase integral along a direction perpendicular to the momentum transfer q at each value of q, is stressed.
The pattern of abundances within the iron-abundance peak of the solar system is analyzed for various Cr, Fe, and Ni abundances, and a method is developed for finding the best fit to a given set of abundances with a chosen number of zones, i.e., mass contributions characterized by differing values of eta. This material can be synthesized by a superposition of e-process compositions in a low-eta region (eta = 0.003) and a high-eta region (eta = 0.065 -0.080) with at least 85% coming from the low-eta region. Addition of a third eta zone is unproductive. The applicability of the particle-poor freeze out is discussed in the light of these abundances, and the results of employing different numbers and types of zones are interpreted as an indication of the relative abundances themselves. Ejection of the low-eta zones is of great interest in gamma-ray astronomy and for empirical testing of theories of nucleosynthesis. The distribution of high zones should give important information about the formation of collapsed remnants.