Observed laser lines in freon-helium mixtures.
Laser lines observation in Freon-He mixtures in CW gas discharge
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Laser lines observation in Freon-He mixtures in CW gas discharge
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Feasibibility study of Auger and photoelectron spectroscopy as analytical tool
Vibration-rotation bands of arsine in 2-mu regions
Changes in psychophysical judgments of roughness due to social influence with other subjects
Auger and photoelectron spectroscopy principles, instrumentation, and applications
Auger and photoelectron spectroscopy for chemical analysis, noting effects of sample thickness, sample potential, surface contamination and X ray incident angle
Heavy positive ions pulse counting by spiral-type continuous channel electron multipier, noting long pulse rise time composed of numerous after pulsing
Hypothermia and ionizing radiation effects on hamsters influenza immune response
Auger spectra characteristics obtained with X rays and electrons from radioactive alpha sources
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X ray excited LMM Auger spectra of copper, iron, and nickle
High rotor advance ratio from multiblade general coordinates method in linear analysis of lifting rotor dynamic stability and gust ratio
Core binding energy difference between bridging and nonbridging oxygen atoms in silicate chain of pyroxenes, using X ray photoelectron spectra
The X-ray fluorescence spectrometer, carried in the SIM bay of the command service module was employed principally for compositional mapping of the lunar surface while in lunar orbit, and secondarily, for X-ray astronomical observations during the trans-earth coast. The lunar surface measurements involved observations of the intensity and characteristics energy distribution of the secondary or fluorescent X-rays produced by the interaction of solar X-rays with the lunar surface. The astronomical observations consisted of relatively long periods of measurements of X-rays from pre-selected galactic sources such as Cyg-X-1 and Sco X-1 as well as from the galactic poles.
The effects of various gust alleviation methods on the random blade response in flapping were studied analytically, assuming a rigid rotor support. The analytical model assumes rigid flapping blades with elastic root restraints. Linearized equations which are approximately valid at low lift conditions were used. Because of the interblade coupling from the feedback devices, the method of multiblade generalized coordinates was most convenient and was extended to include coning, differential coning, and warping of the rotor. The numerical examples cover the dynamic stability characteristics as affected by feedback gains of three- to six-bladed rotors. The number of blades had large effects on stability limits and modal time functions at these limits. The random flapping response of the blades to atmospheric turbulence was determined at 1.6 rotor advance ratio using feedback gains below the stability limit. The most effective reduction of the flapping response per unit gain was achieved with a rotor coning angle feedback.
The CSM spectrometric data on the lunar surface with respect to its chemical composition are presented for Al, Mg, and Si as Al/Si and Mg/Si ratios for the various features overflow by the spacecraft. The lunar surface measurements involved observations of the intensity and characteristic energy distribution of the secondary or fluorescent X-rays produced by the interaction of solar X-rays with the lunar surface. The results showed that the highlands and maria are chemically different, with the highlands having considerably more Al and less Mg than the maria. The mare-highland contact is quite sharp and puts a limit on the amount of horizontal transport of material. The X-ray data suggest that the dominant rock type of the lunar highlands is a plagioclase-rich pyroxene bearing rock, probably anorthositic gabbro or feldspathic basalt. Thus the moon appears to have a widespread differentiated crust (the highlands) systematically richer in Al and lower in Mg than the maria. This crust is pre-mare and may represent the first major internal differentiation of the moon.
The preliminary results from the Sco X-1 and Cyg X-1 obtained from the Apollo 15 X-ray detector data are presented along with preliminary results of the X-ray fluorescence spectrometric data of the lunar surface composition. The production of the characteristic X-rays following the interaction of solar X-rays with the lunar surface is described along with the X-ray spectrometer. Preliminary analyses of the astronomical X-ray observation and the X-ray fluorescence data are presented.