Probable observations of the geomagnetic tail at 10 super 3 earth radii by Pioneer 7.
Geomagnetic tail at 1000 earth radii, noting possibility of magnetic force lines connected to earth and tail geometry
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.
Geomagnetic tail at 1000 earth radii, noting possibility of magnetic force lines connected to earth and tail geometry
Pioneer VII plasma probe data indicating geomagnetic wake at 1000 earth radii downstream from earth
Explorer 26 observations of solar protons at altitudes of four earth radii inside magnetosphere near geomagnetic equator
Correlation of lunar radii estimates obtained from earth based photographic study and lunar orbiter gravitational field coefficient measures
Bonding radii of ribosomes crystal packing between forms found in chromatoid bodies of Entamoeba invadens and mitotic cells of chilled chick embryos
Geomagnetic tail observation at 500 earth radii by Pioneer 8
Solar wind plasma observations in geomagnetospheric wake compared at 1000 and 500 earth radii, considering ion energy spectra and geomagnetic tail
Three transient phenomena interpreted as coronal magnetic bottle at 10 solar radii having expansion at sub-Alevenic velocity
Magnetopause crossing of ATS geostationary satellite at 6.6 earth radii
Geomagnetic tail observations by Pioneer 8 at 500 earth radii, analyzing time-averaged magnetic field data
Neutron and proton distributions rms radii in nuclei by optical model analysis of low energy pion-nucleus interactions
Coronal magnetic bottle at ten solar radii from Faraday rotation measurements of occulted spacecraft radio source
Geomagnetic wake in solar wind at 500 earth radii, correlating Explorer 35 and Pioneer 8 data
Thermal contact conductance test data at high vacuum were obtained from two Armco iron specimens having smooth, large radii of curvature, convex, one-half wave length surfaces. The data are compared with calculations based on two macroscopic elastic deformation theories and an empirical expression. Major disagreement with the theories and fair agreement with the empirical expression resulted. Plastic deformation of all the contacting surfaces was verified from surface analyzer statistics. These results indicate that the theoretical assumption of macroscopic elastic deformation is inadequate for accurate prediction of heat transfer with light loads for Armco iron specimens similar to those used in this investigation.
Thermal contact conductance test data at high vacuum were obtained from two Armco iron specimens having smooth, large radii of curvature, convex, one-half wave length surfaces. The data are compared with calculations based on two macroscopic elastic deformation theories and an empirical expression. Major disagreement with the theories and fair agreement with the empirical expression resulted. Plastic deformation of all the contacting surfaces was verified from surface analyzer statistics. These results indicate that the theoretical assumption of macroscopic elastic deformation is inadequate for accurate prediction of heat transfer with light loads for Armco iron specimens similar to those used in this investigation.
Nearly three years of Ames magnetometer data from Explorer 35 are used to establish plasma-sheet configurations in the geomagnetic tail at the lunar orbit. The plasma sheet is defined either as a region with different field orientations from normal magnetic-field directions in the tail, or as a region where the magnetic field variance is greater than elsewhere in the tail. The plasma-sheet configuration at the lunar orbit derived in this manner is found to be similar to the distribution at 18 earth radii observed by Vela satellites. The seasonal dependence and variations with geomagnetic activity are also presented.
The two-dimensional (YZ plane) spatial distribution of magnetic field magnitudes in the geomagnetic tail at the lunar distance is given in both the solar magnetospheric and the neutral-sheet coordinate systems by using three years of data from the Ames magnetometer on Explorer 35. The effect of changes in geomagnetic activity is also presented. In the magnetotail near 60 earth radii, a broad region in which the magnetic field intensity is relatively weak in comparison with that in the other region of the tail is located adjacent to the solar magnetospheric equatorial plane and the calculated neutral sheet. This depression of the field due to the diamagnetic effect of the plasma sheet is more evident during times of minimum geomagnetic activity.-
Flux gate magnetometer data from OGO 5 are presented that establish the existence of large field depressions under conditions of varying degree of disturbance at distances ranging from 2.3 to 3.6 earth radii at all local times. For this study, flux gate data obtained near perigee during the period of approximately one year from Jan. 21, 1969, to Feb. 23, 1970, were used.