Study of drift-field solar cells damaged by low-energy protons Progress report, Jun. 15 - Aug. 10, 1965
Irradiation damage of drift-field solar cells by low energy protons - calibration of irradiation apparatus and monitoring equipment
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Irradiation damage of drift-field solar cells by low energy protons - calibration of irradiation apparatus and monitoring equipment
Low energy proton damage to drift field solar cells
Determination of maximum force on static sheet of aluminum subjected to magnetic field of hammer coil
Flow field produced by three hypersonic jets impinging on surface in vacuum environment
Silicon solar cell with drift fields of various widths and magnitudes, considering performance changes before and after radiation
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The qualitative properties of an open magnetosphere and its electric field are examined and compared to a simple model of a dipole in a constant field and to actual observations. Many of these properties are found to depend on the separatrix, a curve connecting neutral points and separating different field-line regimes. In the simple model, the electric field in the central polar cap tends to point from dawn to dusk for a wide choice of external fields. Near the boundary of the polar cap electric equipotentials curve and become crescent-shaped, which may explain the correlation of polar magnetic variations with the azimuthal component of the interplanetary magnetic field, reported by Svalgaard. Modifications expected to occur in the actual magnetosphere are also investigated: in particular, it appears that bending of equipotentials may be reduced by cross-field flow during the merging of field lines and that open field lines connected to the polar caps emerge from a long and narrow slot extending along the tail.
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Using the Caltech videomagnetograph, we obtained a 6.5-hr movie of the magnetic fields in a young active region. The major contribution to the short term magnetic evolution of the region was provided by many discrete magnetic points which move in apparently random directions with typical velocities of 0.4 - 1.0 km/sec. The majority of these features appear to be footpoints of new EFR's, which emerge at an observed rate of one to two per hour. The pattern of the motions suggests that the magnetic evolution of a growing region cannot be principally due to photospheric convective cells.
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