Search results for "Electron microprobe"

showing 10 items of 40 documents

MPI-DING reference glasses for in situ microanalysis: New reference values for element concentrations and isotope ratios

2006

We present new analytical data of major and trace elements for the geological MPI-DING glasses KL2-G, ML3B-G, StHs6/80-G, GOR128-G, GOR132-G, BM90/21-G, T1-G, and ATHO-G. Different analytical methods were used to obtain a large spectrum of major and trace element data, in particular, EPMA, SIMS, LA-ICPMS, and isotope dilution by TIMS and ICPMS. Altogether, more than 60 qualified geochemical laboratories worldwide contributed to the analyses, allowing us to present new reference and information values and their uncertainties (at 95% confidence level) for up to 74 elements. We complied with the recommendations for the certification of geological reference materials by the International Associ…

In situ010504 meteorology & atmospheric sciencesIsotopeTrace elementMineralogyElectron microprobeIsotope dilution010502 geochemistry & geophysics01 natural sciencesMicroanalysisGeophysics13. Climate actionGeochemistry and PetrologyReference valuesGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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A Raman calibration for the quantification of SO42-groups dissolved in silicate glasses: Application to natural melt inclusions

2017

Sulfur is an important volatile element involved in magmatic systems. Its quantification in silicate glasses relies on state-of-the-art techniques such as electronprobe microanalyses (EPMA) or X-ray absorption spectroscopy but is often complicated by the fact that S dissolved in silicate glasses can adopt several oxidation states (S6+for sulfates or S2-for sulfides). In the present work, we use micro-Raman spectroscopy on a series of silicate glasses to quantify the S content. The database is constituted by 47 silicate glasses of various compositions (natural and synthetic) with S content ranging from 1179 to 13 180 ppm. Most of the investigated glasses have been synthesized at high pressur…

Materials science010504 meteorology & atmospheric sciencesAbsorption spectroscopyS contentAnalytical chemistrychemistry.chemical_elementredox conditionsElectron microprobe010502 geochemistry & geophysicsmelt inclusions01 natural scienceschemistry.chemical_compoundsymbols.namesakeS speciationGeochemistry and PetrologyOxidizing agentSulfatesilicate glassSpectroscopyGeophysic0105 earth and related environmental sciencesMelt inclusionsmelt inclusionMicro-Raman spectroscopyredox conditionSulfurGeophysicschemistry13. Climate action[SDU]Sciences of the Universe [physics]symbolssilicate glaRaman spectroscopy
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Ultrathin metal films and inorganic clusters via thermodesorption of LB films

1991

Langmuir-Blodgett multilayers of cadmium arachidate and ferric stearate were investigated during heating in order to derive information on processes involved in thermodesorption and on the inorganic microstructures left on the substrate after thermodesorption. We studied these processes by X-ray induced photoelectron spectroscopy (XPS), interference enhanced reflection (IeR), Nomarsky microscopy, electron microprobe analysis and in the case of Fe57-ions by conversion electron Mossbauer spectroscopy (CEMS). Two different mechanisms of desorption were observed. In the case of cadmium arachidate multilayers it is shown that before desorption the film ruptures laterally and then forms droplets.…

Materials sciencePolymers and PlasticsOrganic ChemistryAnalytical chemistryNucleationSubstrate (electronics)Electron microprobeCondensed Matter Physicschemistry.chemical_compoundX-ray photoelectron spectroscopychemistryConversion electron mössbauer spectroscopyStearateDesorptionMaterials ChemistrymedicineFerricmedicine.drugMakromolekulare Chemie. Macromolecular Symposia
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Low Temperature Afterglow from SrAl <sub>2</sub>O <sub>4</sub>: EU, Dy, B Containing Glass

2020

SrAl2O4: Eu, Dy, B particles were added in a phosphate glass (90NaPO3-10NaF (in mol%)) using the direct doping method. For the first time, the composition of the particles prior to and after embedding them in the glass was analysed using EPMA analysis. Boron was found to be incorporated in already distorted surroundings creating new trapping centers in the particles which are thought to be favourable for the tunnelling process and so for the afterglow at 10K. Despite the partial decomposition of the particles, the glass exhibit afterglow at low temperature confirming to be promising materials for low temperature applications.

Materials sciencechemistryDopingAnalytical chemistrychemistry.chemical_elementPartial decompositionTrappingElectron microprobeBoronQuantum tunnellingPhosphate glassAfterglowSSRN Electronic Journal
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Electron microprobe technique for the determination of iron oxidation state in silicate glasses

2018

We present a new calibration for the determination of the iron oxidation state in silicate glasses by electron probe microanalysis (EPMA) with the "flank method." This method is based on the changes in both intensity and wavelength of the FeLα and FeLβ X-ray emission lines with iron oxidation state. The flank method utilizes the maximum difference for the FeLα and FeLβ spectra observed at the peak flanks between different standard materials, which quantitatively correlates with the Fe2+ content. Provided that this correlation is calibrated on reference materials, the Fe2+/ΣFe ratio can be determined for samples with known total Fe content. Two synthetic Fe-rich ferric and ferrous garnet end…

MicroprobeMaterials science010504 meteorology & atmospheric sciencesInorganic chemistryElectron microprobe010502 geochemistry & geophysics01 natural sciencesRedoxflank methodferric-ferrous ratioGeophysicsGeochemistry and PetrologyOxidation stateredox statepillow glassesSilicate glassMicroprobesilicate glasses0105 earth and related environmental sciences
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Morphological and chemical evolution of corundum (ruby and sapphire): Crystal ontogeny reconstructed by EMPA, LA-ICP-MS, and Cr3+Raman mapping

2016

The term “ ontogeny ,” which is commonly used in biology, was introduced into the Earth sciences in 1961 to include the genesis and evolution of single crystals and crystal aggregates. The term encompasses nucleation , growth , alteration , and destruction . We present results of studies concerning the ontogeny of natural corundum (rubies and sapphires), and the chemical and morphological evolution of corundum crystals from deposits in Africa (Kenya, Tanzania, Madagascar) and Southeast Asia (Vietnam). Trace-element compositions indicative for different corundum habits were determined by rim-to-rim LA-ICP-MS and electron microprobe analyses. Raman spectroscopy was applied for Cr 3+ photolumi…

Morphology (linguistics)010504 meteorology & atmospheric sciencesAnalytical chemistryMineralogyCorundumCrystal growthElectron microprobeengineering.material010502 geochemistry & geophysics01 natural sciencesCrystalchemistry.chemical_compoundsymbols.namesakeGeophysicschemistryGeochemistry and PetrologyengineeringSapphiresymbolsRaman spectroscopy0105 earth and related environmental sciencesEMPAAmerican Mineralogist
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Preliminary corrosion studies of P-91 in flowing lead–lithium with and without magnetic field for Indian lead–lithium ceramic breeder test blanket mo…

2014

To study the corrosion of P-91 (9% chromium and 1% molybdenum) material with lead–lithium (Pb–Li) eutectic, two experiments were carried out in a forced convection loop, at eutectic temperature of 550 °C. The first experiment was carried out at a velocity of 15 cm s−1 for 1000 h and the second experiment, at a velocity of 30 cm s−1 for 2700 h. In both the experiments, P-91 sample coupons were exposed to Pb–Li flow in the presence and absence of magnetic field. Samples were analyzed using an optical microscope, scanning electron microscope (SEM) and electron probe micro-analyzer (EPMA). Micro-Vickers hardness testing was also carried out. Dissolution of elements into liquid metal is the main…

Nuclear and High Energy PhysicsMaterials scienceScanning electron microscopeMetallurgychemistry.chemical_elementElectron microprobeCondensed Matter PhysicsIndentation hardnessCorrosionlaw.inventionChromiumchemistryOptical microscopeMolybdenumlawEutectic systemNuclear Fusion
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Incomplete retention of radiation damage in zircon from Sri Lanka

2004

A suite of 18 zircon gemstones from placers in the Highland/Southwestern Complex, Sri Lanka, were subjected to a comprehensive study of their radiation damages and ages. The investigation included X-ray diffraction, Raman and PL spectroscopy, electron microprobe, PIXE and HRTEM analysis, as well as (U-Th)/He and SHRIMP U-Th-Pb age determinations. Zircon samples described in this study are virtually homogeneous. They cover the range from slightly metamict to nearly amorphous. Generally concordant U-Th-Pb ages averaging 555 ± 11 Ma were obtained. Late Ordovician zircon (U-Th)/He ages scattering around 443 ± 9 Ma correspond reasonably well with previously determined biotite Rb-Sr ages for rock…

PLOMBURANIUMGeochemistryMineralogy550 - Earth sciencesElectron microprobeengineering.materialDATATIONZIRCONIUMMetamictizationSTRONTIUMGeochemistry and PetrologyANALYSE SPECTRALERadiation damageZIRCONRadiogenic nuclideALTERATIONMETAMICTISATIONIRRADIATIONGeophysicsHomogeneousengineeringMICROSTRUCTURESri lankaBiotiteGeologyRADIOACTIVITEZircon
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The structural and dielectric properties of the Na0.96Li0.04NbO3ceramics

2007

Ceramic samples Na0.96Li0.04NbO3 were obtained using ceramic technology. The phase and structural analysis, the microstructure, EDS and EPMA, dielectric and hysteresis loops measurements have been performed. The dielectric and hysteresis loops measurements of Na0.96Li0.04NbO3 have been carried out. The dielectric measurements were performed both without and under axial pressure up to 120 MPa. It was shown that Na0.96Li0.04NbO3 ceramics have orthorhombic symmetry at room temperature and undergo a first order phase transition at a temperature of about 570 K. The axial pressure shifts the phase transition temperature and decreases the hysteresis in field-polarisation and field-strain dependenc…

Phase transitionMaterials scienceAxial pressureElectron microprobeDielectricMicrostructureCondensed Matter::Materials ScienceHysteresisCrystallographyCondensed Matter::Superconductivityvisual_artPhase (matter)visual_art.visual_art_mediumGeneral Materials ScienceCeramicComposite materialInstrumentationPhase Transitions
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Low temperature measurements by infrared spectroscopy in $CoFe_2O_4$ ceramic

2012

In this paper results of new far-infrared and middle-infrared measurements (wavenumber range of 4000cm-1 - 100cm-1) in the range of the temperature from 300K to 8K of the CoFe2O4 ceramic are presented. The bands positions and their shapes are the same in the wide temperature range. The quality of the sample was investigated by X-ray, EDS and EPMA studies. The CoFe2O4 reveals the cubic structure (Fd-3m) in the temperature range from 85K to 360 K without any traces of distortion. On the current level of knowledge the polycrystalline CoFe2O4 does not exhibit phase transition in the temperature range from 8 K to 300 K.

Phase transitionMaterials scienceQC1-999FT-FIRft-firAnalytical chemistryFOS: Physical sciencesGeneral Physics and AstronomyInfrared spectroscopyElectron microprobeTemperature measurement$CoFe_2O_4$CeramicCondensed Matter - Materials ScienceRange (particle radiation)Physicscobalt spinel ferriteMaterials Science (cond-mat.mtrl-sci)Atmospheric temperature rangecofe2o4visual_artinfraredvisual_art.visual_art_mediumCrystalliteft-mirFT-MIR
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