Diffusive mixing as a tool for confirming the origin of tektites Semiannual report, Apr. 1, 1967 - Sep. 30, 1967
Homogeneity of Thailand tektites and self- diffusion measurements of silicon, strontium, and potassium
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Homogeneity of Thailand tektites and self- diffusion measurements of silicon, strontium, and potassium
Multichannel system employing a radioisotope radiation source, strontium-90, radiation detector, and a silicon surface barrier detector, measures the local density of liquid hydrogen at various levels in a storage tank. The instrument contains electronic equipment for collecting the density information, and a data handling system for processing this information.
Fabrication and testing of diodes for pore-type dispenser, coated particle, and barium strontium cathodes
Tabulated data on genetic effects of strontium 85 gamma radiation on Neurospora
Superconducting transition temperatures calculated for semiconducting strontium titanates
Polaron coupling approximation applied to electron-longitudinal optical phonon interaction on spheroidal energy band surface of strontium titanate
Autoionization resonance in strontium iodine spectrum using photoelectric spectrometer
Zr doped superconducting ceramic strontium titanate, noting effective electron mass variations and transition temperature
Polarons large to nearly small transitions, studying ground state mass dependence on bare electron mass, electron-phonon interactions model, superconducting strontium titanate, etc
Process produces linearly responding surface barrier diodes. Hydrogen-fired, conducting strontium titanate crystals provide linear characteristics. The process uses space charge potentials and depletion layer phenomena to achieve conduction and insulation.
Strontium chloride lanthanum ion system with dynamic Jahn-Teller effect, indicating isotropic EPM spectrum resulting from averaging by relaxation
Inorganic photochromic and cathodochromic recording materials, examining transition metal doped strontium titanates, rare earth doped calcium fluorides and Fe or S doped sodalite
Electron paramagnetic resonance spectral investigation of dynamic Jahn-Teller effect in La doped strontium chloride, discussing structural variations as function of temperature
Since many radioisotopes accumulate in hair, this tropism was investigated by comparing the radioactivity of shaved with plucked hair collected from rats at various time intervals up to 24 hrs after intravenous injection of the ecologically important radioisotopes, iodine-131, manganese-54, strontium-85, and zinc-65. The plucked hair includes the hair follicles where biochemical transformations are taking place. The data indicate a slight surge of each radioisotpe into the hair immediately after injection, a variation of content of each radionuclide in the hair, and a greater accumulation of radioactivity in plucked than in shaved hair. These results have application not only to hair as a measure of exposure to radioisotopes, but also to tissue damage and repair at the hair follicle.
The results of an experimental evaluation of the real-time degradation characteristics of lithium-diffused silicon solar cells are reported. A strontium-90 radioisotope was used for simulation of a typical earth-orbital electron environment. The experiment was performed in an ion pump vacuum chamber with samples maintained at -50, +20, +50, and +80 C. Samples were illuminated during the 6-month exposure run with solar cell 1-5 characteristics measured periodically in situ. This 6-month exposure corresponded to a 1 MeV equivalent fluence of approximately 10 to the 14th power electrons/sq cm. Several types of lithium cells were irradiatied and compared directly with conventional N/P cells. The best lithium cells compared favorably with N/P cells, particularly at the higher test temperatures. With a slight improvement of initial performance characteristics, lithium cells appear feasible for 5 to 10 year missions at synchronous altitude. Based on the reported results and those of other irradiation experiments, lithium cells would appear to be superior to N/P cells in proton-dominated earth-orbital environments. Another important conclusion of the effort was that illuminated/loaded cells degrade more rapidly than do dark/unloaded cells. The irradiation experiment provided data of high quality with a high degree of confidence because of the experimental and statistical analysis techniques utilized.
The initial strontium isotopic composition of 15 mafic volcanic rocks from the southern Great Basin has been determined. Results indicate that the basalts must have been derived from unusual mantle material in which an originally high Rb/Sr ratio was markedly lowered during an earlier phase of magmatic activity.
Minerals were separated by an EM approach and with the aid of liquids of great density. An analysis of K, Rb, Ca, Sr, Ha, and rare earth elements was conducted by means of a mass spectrometer isotope dilution technique. The behavior of the divalent europium ions during the partition process was found to be very similar to that of divalent strontium ions, taking into consideration data of the partition coefficients between coexisting feldspars in acidic rocks.
Relative age measurements were made for 14 light plains areas, using 30X enlargements of Apollo 16 metric camera photography. Results indicate that: (1) Crater morphology and frequency studies consistently indicate that the Fra Mauro Formation has received 2.5 to 3 times as much impact flux as the Cayley Formation. (2) Crater counts and relative age dating indicate that the Cayley Formation is only slightly older than the oldest mare units. (3) Assuming the rubidium-strontium ages of Apollo 14 basalt breccias give minimum age for Fra Mauro Formation, the Cayley Formation must have been generated throughout a period of less than 100 million years, approximately 3.8 to 3.9 billion years ago. (4) The Cayley Formation ages obtained on the near side and far side are the same, indicating a synchrony throughout the moon in these units. (5) The linear relationship as predicted by the small impact erosion model between net accumulated flux and the maximum diameter of a crater that could be eroded below recognition is confirmed.