Search results for "MINERALOGY"

showing 10 items of 1516 documents

Peculiarities of luminescent properties of cerium doped YAG transparent nanoceramics

2010

Abstract Optical and luminescence properties of transparent nanosized cerium doped Y 3 Al 5 O 12 (YAG:Ce) ceramics have been studied. YAG:Ce nanoceramics were obtained by means of low temperature and high pressure (LTHP) sintering method. Nanoceramic samples were sintered in the 2–8 GPa pressure range, whereas Ce 3+ concentration was varied in the 0.5–5 at. % range. It is shown that, in contrast to the single crystal, a strong rise of absorption coefficient was detected already at wavelength shorter than 400 nm in all nanoceramic samples studied. Furthermore, in nanoceramic samples unusual UV emission band near 3.1 eV was observed, which is not observed in the YAG:Ce single crystal. High pr…

RadiationMaterials scienceDopingAnalytical chemistrychemistry.chemical_elementSinteringMineralogyNanoceramicCeriumchemistryAttenuation coefficientvisual_artvisual_art.visual_art_mediumCeramicLuminescenceInstrumentationSingle crystalRadiation Measurements
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Quantitative X-ray diffraction phase analysis of airborne particulate collected by a cascade impactor sampler using the Rietveld full-pattern fitting…

1997

Samples of airborne particulate were collected at the “El Ingenio” site in Castellón (Spain) using a cascade impactor sampler. Quantitative analysis of present phases in the aerosol was performed using the full-pattern fitting Rietveld method. Quantitative information was obtained from refined individual scale factors and unit-cell volumes, obtained with a Rietveld refinement program. Quartz, calcite, and gypsum were encountered as major phases, and their size distribution and concentration in the atmosphere were calculated.

RadiationMaterials scienceRietveld refinementAnalytical chemistryMineralogyParticulatesCondensed Matter PhysicsAerosolPattern fittingX-ray crystallographyGeneral Materials SciencePhase analysisInstrumentationQuartzCascade impactorPowder Diffraction
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The luminescence of ZnO ceramics

2010

Abstract The luminescence properties of ZnO ceramics with grains 100–5000 nm sintered by different techniques from nanopowders were studied. The luminescence decay times were compared with that obtained for ZnO single crystal. The temperature dependence of non-exponential decay of defect luminescence (2.0–2.6 eV) was measured in wide time, intensity and temperature range. The luminescence decay kinetic at T ≤ 20 K shows the decay close to I(t) ∼ t−1 dependence. At temperature region 50–250 K the decay kinetics is more complicate since the TSL was observed in this temperature region. It is shown that the luminescence properties of NP and ceramics strongly depend on defect distribution on gra…

RadiationNanostructureMaterials scienceScanning electron microscopeAnalytical chemistrySinteringMineralogyAtmospheric temperature rangeThermoluminescencevisual_artvisual_art.visual_art_mediumCeramicLuminescenceInstrumentationSingle crystalRadiation Measurements
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Trap spectroscopy and tunnelling luminescence in feldspars

1998

Abstract Comparative studies of tunnel luminescence, thermally stimulated luminescence (TSL), and trap energy spectra by the fractional glow technique (FGT) have been made both with sanidine and microcline feldspars. After X-irradiation at LNT these feldspars show intense tunnelling afterglow. As the temperature is raised, several TSL glow peaks may be observed, starting at 135 K. An intense peak at 250 K is common to all four investigated microclines. In samples of sanidine, tunnelling afterglow overcomes TSL up to 250–260 K. With sanidine and microcline samples, the distributions of trap activation energies vs temperature obtained by the FGT are continuous and quasi-linear. Maxima in the …

RadiationPhotoluminescenceMicroclineChemistryAnalytical chemistryMineralogyengineering.materialSanidineThermoluminescenceAfterglowengineeringLuminescenceInstrumentationAlkali feldsparQuantum tunnellingRadiation Measurements
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Pb–Pb age, stable isotope and chemical composition of Archaean magnesite, Barberton Greenstone Belt, South Africa

2010

International audience; Trace-element, carbon, oxygen and lead-isotope analyses were carried out to determine the formation mode and crystallization age of magnesite from the Budd ultramafic complex of the Archaean Barberton Greenstone Belt, South Africa. Its significantly high Ti contents probably relate to a soluble Ti-rich accessory mineral, probably dissolved during magnesite precipitation. Primitive mantle-normalized REE patterns of the magnesite show negative Ce and Eu anomalies induced by two events: (1) the Eu anomaly indicates reducing conditions probably induced by the emplacement of the ultramafic source rock; (2) the Ce anomaly implies oxidizing conditions, probably during a hyd…

Radiogenic nuclide010504 meteorology & atmospheric sciencesStable isotope ratioArcheanGeochemistryMineralogyGeologyGreenstone belt010502 geochemistry & geophysics01 natural sciencesPlutonismHydrothermal circulationchemistry.chemical_compoundchemistry13. Climate actionUltramafic rockGeology0105 earth and related environmental sciencesMagnesiteJournal of the Geological Society
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Nanoparticles and their influence on radionuclide mobility in deep geological formations

2012

International audience; This article gives an overview of the current status of knowledge concerning the role of nanoparticles (inorganic and organic) in deep geological host rocks and the potential influence of these nanoparticles on radionuclide migration in far-field systems. The manuscript is not intended to be a full review paper or overview paper concerning nanoparticles, here the intention is to refer to recent publications but to highlight the progress made in the 6th framework project IP FUNMIG (Fundamental processes of radionuclide migration) and the open literature over the past 5 a concerning the process understanding of nanoparticle related issues in the three host rock formati…

RadionuclideChemistry[SDE.MCG]Environmental Sciences/Global ChangesDiffusionNanoparticleMineralogy02 engineering and technology010501 environmental sciences021001 nanoscience & nanotechnology01 natural sciencesPollutionConcentration ratio[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeochemistry and PetrologySilicate mineralsBentoniteErosionEnvironmental Chemistry0210 nano-technologyGroundwaterInstitut für Biochemie und Biologie0105 earth and related environmental sciences
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Cosmic-ray exposure ages of pallasites

2015

We analyzed cosmogenic nuclides in metal and/or silicate (primarily olivine) separated from the main-group pallasites Admire, Ahumada, Albin, Brahin, Brenham, Esquel, Finmarken, Glorieta Mountain, Huckitta, Imilac, Krasnojarsk, Marjalahti, Molong, Seymchan, South Bend, Springwater, and Thiel Mountains and from Eagle Station. The metal separates contained an olivine fraction which although small, <1 wt% in most cases, nonetheless contributes significantly to the budgets of some nuclides (e.g., up to 35% for Ne-21 and Al-26). A correction for olivine is therefore essential and was made using model calculations and/or empirical relations for the production rates of cosmogenic nuclides in iron …

RadionuclideOlivineMeteoroidGeochemistryMineralogyengineering.materialSilicateParent bodychemistry.chemical_compoundGeophysicschemistryMeteoriteSpace and Planetary ScienceengineeringNuclideCosmogenic nuclideGeologyMeteoritics &amp; Planetary Science
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Natural radioactivity in a volcanic island: Ustica, Southern Italy

1997

Abstract Gamma-ray spectrometric measurements were performed on rocks and soils of the island of Ustica (Southern Italy) to quantify the concentrations of the natural radionuclides. The 238U, 232Th, and 40K concentration ranges (15–164, 16–174, and 201–1350 Bq kg−1, respectively) were compared with mineralogical and chemical data obtained by XRD and XRF analyses. The observed levels of the primordial radionuclides corresponded to the magmatological features of the rocks. Soil samples generally showed specific gamma-ray activities not directly correlatable to those measured in the underlying rocks. A survey was also perormed to measure air kerma in outdoor and indoor environments using therm…

Radionuclideeducation.field_of_studyRadiationSoil testVolcanic islandHealth impactPopulationMineralogychemistry.chemical_elementRadonchemistryEnvironmental chemistrySoil waterEnvironmental scienceeducationNatural radioactivityApplied Radiation and Isotopes
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Correlation of radioactivity measurements, air kerma rates and geological features of Sicily

2006

Abstract Sicily, the largest Mediterranean island (with an extension of about 25 000 km 2 ), exhibits a very wide variety of lithologies, ranging from sedimentary to metamorphic and volcanic rocks. Principal component analysis (PCA) and hierarchical cluster analysis (HCA) have been applied to air kerma values measured by thermoluminescent dosimetry in several sites and to data of radionuclide concentrations, geochemical and mineralogical features of rocks and soils sampled in 29 sites of Sicily to point out similarities among different lithologies. The study was devoted to find multiple correlations and allow a better classification of Sicilian lithotypes. Samples of rocks and soils have be…

Radionuclidegeographyeducation.field_of_studyRadiationgeography.geographical_feature_categorySoil testLithologyPopulationMineralogyNatural radioactivity Sicily Elemental concentration Mineralogy Environmental doseVolcanic rockPetrographyKermaSedimentary rockeducationInstrumentationGeologyRadiation Measurements
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Number, Mass and Volume Distributions of Mineral Aerosol and Soils of the Sahara

1983

Abstract A direct method will be described to determine the complete mineral size distribution in aerosol (xylene-insoluble component) and soils (water-insoluble component) covering a size range from 0.01 up to 100 μm and 1000 μm radius, respectively, by using a combination of a scanning electron microscope, optical microscope and sieving. Aerosol and soil samples from the Sahara have been investigated. All mineral aerosol size distributions indicate a maximum between 0.06 and 0.08 μm radius and mineral particles have been found in the Aitken size range down to 0.02 μm radius. The concentration decrease toward larger particles is not uniform and shows considerable variations below 0.5 μm an…

Range (particle radiation)Materials scienceOptical microscopeSoil testVolume (thermodynamics)Scanning electron microscopelawSoil waterGeneral EngineeringMineralogyRadiusAerosollaw.inventionJournal of Climate and Applied Meteorology
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