Prediction of neutron induced activation. volume 4 - nap gamma radiation library final report, 14 may 1964 - 31 jan. 1966
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The concentrations of aluminum, manganese, sodium, chromium, iron, cobalt, and 12 rare earth elements were determined by neutron activation analysis using slow neutrons. Oxygen and silicon were determined using a fast neutron generator. Mossbauer spectroscopy was used to investigate iron compounds in Luna 16 regolith samples from the upper part of the core.
Gallium abundance measured in carbonaceous, enstatite and chondrite meteorites, using neutron activation technique
Element abundance in various chondrite groups determined by neutron activation technique
Calibration of argon gas neutron activation sampling device
Rare-earth element abundance patterns in Hawaiian basalts determined by neutron activation analysis
Element abundance in chondrules and meteorites measured by instrumental neutron activation analysis, and indium behavior in chondrites
Silicon abundances in chondrules from different chondrites by neutron activation analysis
Quartz pebbles from the Roter Kamm impact crater (the Namib Desert, SWA/Namibia) were examined for evidence of impact-induced hydrothermal activity, using results from microprobe analyses, neutron activation analyses, transmission IR spectroscopy, and X-ray diffractometry. It was found that the pebbles consisted of pure quartz, which contains three different types of fluid inclusions. These were identified as primary inclusions (5-10 microns) that record the formation conditions of the quartz, very small (less than 1 micron) secondary inclusions associated with the grain boundaries, and late inclusions of irregular size. It is concluded that the quartz and the primary inclusions may provide evidence for a postimpact phase of extensive hydrothermal activity, generated by the residual heat from the kinetic energy of the impact.
Atomic absorption and emission spectroscopy, and neutron activation for ultratrace chemical analysis of materials for semiconductor
Element abundances determined by instrumental neutron activation analysis technique in individual chondrules separated from certain chondritic meteorites
Computer program for instrumental neutron activation analysis of chemical abundances in meteorites, examining gamma-ray spectra
Aluminum sputtering, and neutron activation analysis after cesium ion bombardment
Fast neutron activation cross sections of Se and Fe measured, noting subshell closure effect and isomer ratio
Instrumental neutron activation analysis of meteoritic and terrestrial specimens and separate chondrules to chart abundances of seven elements
Neutron activation and cesium-aluminum sputtering in oxygenated gas atmosphere
Neutron activation investigation of cesium ion sputtering of Al in rarefied oxygen atmosphere
Advances in the radiologic sciences have permitted the development of numerous noninvasive techniques for measuring the mineral content of bone, with varying degrees of precision, accuracy, and sensitivity. The techniques of standard radiography, radiogrammetry, photodensitometry, Compton scattering, neutron activation analysis, single and dual photon absorptiometry, and quantitative computed tomography (QCT) are described and reviewed in depth. Results from previous cross-sectional and longitudinal QCT investigations are given. They then describe a current investigation in which they studied 269 subjects, including 173 normal women, 34 patients with hyperparathyroidism, 24 patients with steroid-induced osteoporosis, and 38 men with idiopathic osteoporosis. Spinal quantitative computed tomography, radiogrammetry, and single photon absorptiometry were performed, and a spinal fracture index was calculated on all patients. The authors found a disproportionate loss of spinal trabecular mineral compared to appendicular mineral in the men with idiopathic osteoporosis and the patients with steroid-induced osteoporosis. They observed roughly equivalent mineral loss in both the appendicular and axial regions in the hyperparathyroid patients. The appendicular cortical measurements correlated moderately well with each other but less well with spinal trabecular QCT. The spinal fracture index correlated well with QCT and less well with the appendicular measurements. Knowledge of appendicular cortical mineral status is important in its own right but is not a valid predictor of axial trabecular mineral status, which may be disproportionately decreased in certain diseases. Quantitative CT provides a reliable means of assessing the latter region of the skeleton, correlates well with the spinal fracture index (a semiquantitative measurement of end-organ failure), and offers the clinician a sensitive means of following the effects of therapy.