Radioanalytical methods for the non-destructive analysis of lunar samples
Identifieur interne : 000381 ( Istex/Curation ); précédent : 000380; suivant : 000382Radioanalytical methods for the non-destructive analysis of lunar samples
Auteurs : Z. Anda [Tchécoslovaquie] ; J. Benada [Tchécoslovaquie] ; J. Kuncí [Tchécoslovaquie] ; M. Vobeck [Tchécoslovaquie] ; J. Frána [Tchécoslovaquie]Source :
- Journal of Radioanalytical Chemistry [ 0022-4081 ] ; 1972-08-01.
Descripteurs français
- Wicri :
- topic : Réacteur nucléaire.
English descriptors
- KwdEn :
- Acta, Activation, Activation analysis, Activation products, Analyticai peak, Analytical peak, Analytical peaks, Analytical possibilities, Apollo, Atomic absorption, Average value, Basic matrix, Channel number, Chem, Chonnel number, Compton, Compton continuum, Conf, Cooling time, Cooling times, Cosmochim, Czechoslovak academy, Detection limit, Detector, Emission spectroscopy, Excitation source, Experimental conditions, Exposure time, First reaction, Fluorescence spectrum, Geochim, Good agreement, High compton continuum background, High concentrations, Inaa, Inner diameter, Instrumental neutron activation analysis, Instrumental photon, Intense peak, Interference contribution, Interference reaction, Isotopic ratios, Largest area, Lunar, Lunar fines, Lunar materials, Lunar samples, Lunar science conf, Lunar science conference, Lunar soil, Lunar soils, Mass spectrometry, Methods table, Mineral components, Mineral fractions, Mylar foil, Neutron, Neutron activation, Neutron activation analysis, Neutron activation products, Neutron component, Neutron flux, Nuclear reactions, Nuclear reactor, Original samples, Original spectrum, Other authors, Paraffin block, Parenthesis, Particular elements, Peak, Peak area, Photon, Pneumatic tube device, Proc, Proportional counters, Radioanal, Radioanal chem, Radioanalytical, Radioanalytical methods, Radioanalytical methods table, Radiochemical separation, Radioisotopic, Radioisotopic fluorescence analysis, Randa, Reactor core, Reference numbers, Rock fragment, Sample container, Scintillation detector, Semiconductor spectrometry, Smaller samples, Spectrometer resolution, Submilligram samples, Terrestrial rocks, Thermal column, Time development, Trace elements, Unidentified mineral, Unpublished, Unpublished proceedings, Uranium contents, Various authors.
- Teeft :
- Acta, Activation, Activation analysis, Activation products, Analyticai peak, Analytical peak, Analytical peaks, Analytical possibilities, Apollo, Atomic absorption, Average value, Basic matrix, Channel number, Chem, Chonnel number, Compton, Compton continuum, Conf, Cooling time, Cooling times, Cosmochim, Czechoslovak academy, Detection limit, Detector, Emission spectroscopy, Excitation source, Experimental conditions, Exposure time, First reaction, Fluorescence spectrum, Geochim, Good agreement, High compton continuum background, High concentrations, Inaa, Inner diameter, Instrumental neutron activation analysis, Instrumental photon, Intense peak, Interference contribution, Interference reaction, Isotopic ratios, Largest area, Lunar, Lunar fines, Lunar materials, Lunar samples, Lunar science conf, Lunar science conference, Lunar soil, Lunar soils, Mass spectrometry, Methods table, Mineral components, Mineral fractions, Mylar foil, Neutron, Neutron activation, Neutron activation analysis, Neutron activation products, Neutron component, Neutron flux, Nuclear reactions, Nuclear reactor, Original samples, Original spectrum, Other authors, Paraffin block, Parenthesis, Particular elements, Peak, Peak area, Photon, Pneumatic tube device, Proc, Proportional counters, Radioanal, Radioanal chem, Radioanalytical, Radioanalytical methods, Radioanalytical methods table, Radiochemical separation, Radioisotopic, Radioisotopic fluorescence analysis, Randa, Reactor core, Reference numbers, Rock fragment, Sample container, Scintillation detector, Semiconductor spectrometry, Smaller samples, Spectrometer resolution, Submilligram samples, Terrestrial rocks, Thermal column, Time development, Trace elements, Unidentified mineral, Unpublished, Unpublished proceedings, Uranium contents, Various authors.
Abstract
Abstract: The elemental compositions of Apollo 11 and Apollo 12 lunar soil samples 10084,141 and 12070,83 and Apollo 12 rock fragment 12063,73 were determined by non-destructive radioanalytical methods. Main mineral fractions and glasses separated from these samples were analyzed as well. Instrumental neutron activation analysis (INAA) was used to determine Na, Mg, Al, Si, K, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Zr, Cs, Ba La, Ce, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Tm, Yb, Lu, Hf, Ta, W, Ir, Au, Th and U. A method of delayed neutron counting was used for the determination of uranium, and non-dispersive radioisotopic X-ray fluorescence analysis was applied to the determination of Ti, Fe, Sr, Y and Zr.
Url:
DOI: 10.1007/BF02514032
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<term>Activation</term>
<term>Activation analysis</term>
<term>Activation products</term>
<term>Analyticai peak</term>
<term>Analytical peak</term>
<term>Analytical peaks</term>
<term>Analytical possibilities</term>
<term>Apollo</term>
<term>Atomic absorption</term>
<term>Average value</term>
<term>Basic matrix</term>
<term>Channel number</term>
<term>Chem</term>
<term>Chonnel number</term>
<term>Compton</term>
<term>Compton continuum</term>
<term>Conf</term>
<term>Cooling time</term>
<term>Cooling times</term>
<term>Cosmochim</term>
<term>Czechoslovak academy</term>
<term>Detection limit</term>
<term>Detector</term>
<term>Emission spectroscopy</term>
<term>Excitation source</term>
<term>Experimental conditions</term>
<term>Exposure time</term>
<term>First reaction</term>
<term>Fluorescence spectrum</term>
<term>Geochim</term>
<term>Good agreement</term>
<term>High compton continuum background</term>
<term>High concentrations</term>
<term>Inaa</term>
<term>Inner diameter</term>
<term>Instrumental neutron activation analysis</term>
<term>Instrumental photon</term>
<term>Intense peak</term>
<term>Interference contribution</term>
<term>Interference reaction</term>
<term>Isotopic ratios</term>
<term>Largest area</term>
<term>Lunar</term>
<term>Lunar fines</term>
<term>Lunar materials</term>
<term>Lunar samples</term>
<term>Lunar science conf</term>
<term>Lunar science conference</term>
<term>Lunar soil</term>
<term>Lunar soils</term>
<term>Mass spectrometry</term>
<term>Methods table</term>
<term>Mineral components</term>
<term>Mineral fractions</term>
<term>Mylar foil</term>
<term>Neutron</term>
<term>Neutron activation</term>
<term>Neutron activation analysis</term>
<term>Neutron activation products</term>
<term>Neutron component</term>
<term>Neutron flux</term>
<term>Nuclear reactions</term>
<term>Nuclear reactor</term>
<term>Original samples</term>
<term>Original spectrum</term>
<term>Other authors</term>
<term>Paraffin block</term>
<term>Parenthesis</term>
<term>Particular elements</term>
<term>Peak</term>
<term>Peak area</term>
<term>Photon</term>
<term>Pneumatic tube device</term>
<term>Proc</term>
<term>Proportional counters</term>
<term>Radioanal</term>
<term>Radioanal chem</term>
<term>Radioanalytical</term>
<term>Radioanalytical methods</term>
<term>Radioanalytical methods table</term>
<term>Radiochemical separation</term>
<term>Radioisotopic</term>
<term>Radioisotopic fluorescence analysis</term>
<term>Randa</term>
<term>Reactor core</term>
<term>Reference numbers</term>
<term>Rock fragment</term>
<term>Sample container</term>
<term>Scintillation detector</term>
<term>Semiconductor spectrometry</term>
<term>Smaller samples</term>
<term>Spectrometer resolution</term>
<term>Submilligram samples</term>
<term>Terrestrial rocks</term>
<term>Thermal column</term>
<term>Time development</term>
<term>Trace elements</term>
<term>Unidentified mineral</term>
<term>Unpublished</term>
<term>Unpublished proceedings</term>
<term>Uranium contents</term>
<term>Various authors</term>
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<term>Activation</term>
<term>Activation analysis</term>
<term>Activation products</term>
<term>Analyticai peak</term>
<term>Analytical peak</term>
<term>Analytical peaks</term>
<term>Analytical possibilities</term>
<term>Apollo</term>
<term>Atomic absorption</term>
<term>Average value</term>
<term>Basic matrix</term>
<term>Channel number</term>
<term>Chem</term>
<term>Chonnel number</term>
<term>Compton</term>
<term>Compton continuum</term>
<term>Conf</term>
<term>Cooling time</term>
<term>Cooling times</term>
<term>Cosmochim</term>
<term>Czechoslovak academy</term>
<term>Detection limit</term>
<term>Detector</term>
<term>Emission spectroscopy</term>
<term>Excitation source</term>
<term>Experimental conditions</term>
<term>Exposure time</term>
<term>First reaction</term>
<term>Fluorescence spectrum</term>
<term>Geochim</term>
<term>Good agreement</term>
<term>High compton continuum background</term>
<term>High concentrations</term>
<term>Inaa</term>
<term>Inner diameter</term>
<term>Instrumental neutron activation analysis</term>
<term>Instrumental photon</term>
<term>Intense peak</term>
<term>Interference contribution</term>
<term>Interference reaction</term>
<term>Isotopic ratios</term>
<term>Largest area</term>
<term>Lunar</term>
<term>Lunar fines</term>
<term>Lunar materials</term>
<term>Lunar samples</term>
<term>Lunar science conf</term>
<term>Lunar science conference</term>
<term>Lunar soil</term>
<term>Lunar soils</term>
<term>Mass spectrometry</term>
<term>Methods table</term>
<term>Mineral components</term>
<term>Mineral fractions</term>
<term>Mylar foil</term>
<term>Neutron</term>
<term>Neutron activation</term>
<term>Neutron activation analysis</term>
<term>Neutron activation products</term>
<term>Neutron component</term>
<term>Neutron flux</term>
<term>Nuclear reactions</term>
<term>Nuclear reactor</term>
<term>Original samples</term>
<term>Original spectrum</term>
<term>Other authors</term>
<term>Paraffin block</term>
<term>Parenthesis</term>
<term>Particular elements</term>
<term>Peak</term>
<term>Peak area</term>
<term>Photon</term>
<term>Pneumatic tube device</term>
<term>Proc</term>
<term>Proportional counters</term>
<term>Radioanal</term>
<term>Radioanal chem</term>
<term>Radioanalytical</term>
<term>Radioanalytical methods</term>
<term>Radioanalytical methods table</term>
<term>Radiochemical separation</term>
<term>Radioisotopic</term>
<term>Radioisotopic fluorescence analysis</term>
<term>Randa</term>
<term>Reactor core</term>
<term>Reference numbers</term>
<term>Rock fragment</term>
<term>Sample container</term>
<term>Scintillation detector</term>
<term>Semiconductor spectrometry</term>
<term>Smaller samples</term>
<term>Spectrometer resolution</term>
<term>Submilligram samples</term>
<term>Terrestrial rocks</term>
<term>Thermal column</term>
<term>Time development</term>
<term>Trace elements</term>
<term>Unidentified mineral</term>
<term>Unpublished</term>
<term>Unpublished proceedings</term>
<term>Uranium contents</term>
<term>Various authors</term>
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<front><div type="abstract" xml:lang="en">Abstract: The elemental compositions of Apollo 11 and Apollo 12 lunar soil samples 10084,141 and 12070,83 and Apollo 12 rock fragment 12063,73 were determined by non-destructive radioanalytical methods. Main mineral fractions and glasses separated from these samples were analyzed as well. Instrumental neutron activation analysis (INAA) was used to determine Na, Mg, Al, Si, K, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Zr, Cs, Ba La, Ce, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Tm, Yb, Lu, Hf, Ta, W, Ir, Au, Th and U. A method of delayed neutron counting was used for the determination of uranium, and non-dispersive radioisotopic X-ray fluorescence analysis was applied to the determination of Ti, Fe, Sr, Y and Zr.</div>
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