Search results for "Silicate"

showing 10 items of 413 documents

Fabrication and characterization of barium silicate ultrathin films as an alternative gate oxide

2008

Down-scaling of elementary CMOS elements requires the replacement of SiO2 as a gate oxide. By the identification of the formation conditions of barium silicate in direct contact of a silicon substrate, this study revealed a potential candidate. First of all, a reaction between Ba and SiO2 leading to the formation of barium silicate as been evidenced by in-situ XPS and SR-PES analyses. Then, barium silicate films have been elaborated by oxygen and barium co-deposition at 580 °C. Thermal treatments under vacuum showed that barium silicate was thermally stable up to 900 °C. TEM and SIMS ex-situ analyses revealed a sharp interface with the substrate. Finally, an experimental setup dedicated to …

[CHIM.MATE] Chemical Sciences/Material chemistrysilicate de baryuminterfacial reactivity[ CHIM.MATE ] Chemical Sciences/Material chemistrybarium silicateXPS[CHIM.MATE]Chemical Sciences/Material chemistry[PHYS.COND]Physics [physics]/Condensed Matter [cond-mat]SR-PESréactivité interfaciale[PHYS.COND] Physics [physics]/Condensed Matter [cond-mat]high-k[ PHYS.COND ] Physics [physics]/Condensed Matter [cond-mat]
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Dissolved silica in the Garonne River waters : changes in the weathering dynamics

2000

The major ion chemistry of the Garonne River is indicative of seasonal variations in the weathering dynamics of the drainage basin. Using the geochemical model MEGA for calculation of the contribution of atmospheric CO2 to the total bicarbonate fluxes exported by the Garonne River allows estimations of the concentrations of the major dissolved elements that originate from silicate- and carbonate-rock weathering. The molecular ratio SiO2/Al2O3 was calculated for the 1989–1992 period to identify the main type of weathering in the Garonne River, and montmorillonite was shown to be the major mineral occurring in the weathering products. The seasonal variations of the SiO2/Al2O3 ratio also showe…

[SDE] Environmental SciencesConcentrationDissolved silica[SDV]Life Sciences [q-bio]Drainage basin010501 environmental sciences010502 geochemistry & geophysics01 natural sciencesDissolved materialsDrainage basinsStream transportchemistry.chemical_compoundGaronne RiverEarth and Planetary Sciences (miscellaneous)ComputingMilieux_MISCELLANEOUSGeneral Environmental ScienceWater Science and TechnologyMineralgeography.geographical_feature_categoryHYDROLOGIEGéochimieGeneral EngineeringSilica6. Clean waterHalides[SDV] Life Sciences [q-bio]EuropeGEOCHIMIEEnvironmental chemistry[SDE]Environmental SciencesFranceWestern EuropeWeatheringSeasonal variationsChloridesmedicineEnvironmental Chemistry0105 earth and related environmental sciencesEcologie EnvironnementHydrologygeographyHydrochemistrySeasonalitymedicine.diseaseGéologie appliquéeSilicateMontmorilloniteGironde Francechemistry13. Climate actionPeriod (geology)General Earth and Planetary Sciences
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Study of parameters endogeneous and exogeneous to ordinary Portland ciment influencing hydration of its main phase : tricalcium silicate

2012

This work devoted to study various parameters influencing hydration of silicate phase main Ordinary Portland Cement (OPC) was performed at the Laboratoire Interdisciplinaire Carnot de Bourgogne (ICB). This study is part of the project "Crystal Growth Control" initiated by BASF in order to monitor and provide the best as possible the hydration of Ordinary Portland Cement. The dissolution of alite, like the pure C3S one, is fast in pure water. Speed decreases with deviation from equilibrium and the concentration of aluminates ions in solution. There is also an adsorption on the surface of the aluminum which is into the alite and released by dissolution. Germination and growth of C-S-H has bee…

[SPI.OTHER]Engineering Sciences [physics]/OtherInorganic saltsOrdinary Portland cement[ SPI.OTHER ] Engineering Sciences [physics]/OtherSilicate tricalcique[SPI.OTHER] Engineering Sciences [physics]/OtherHydratationTricalcium silicateHydrationCiment Portland OrdinaireCinétiqueKineticsSels inorganiquesAlite[CHIM.OTHE] Chemical Sciences/Other[ CHIM.OTHE ] Chemical Sciences/OtherCroissance C-S-HC-S-H GrowthAluminium[CHIM.OTHE]Chemical Sciences/OtherDissolution
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The role of melt composition on aqueous fluid vs. silicate melt partitioning of bromine in magmas

2018

International audience; Volcanogenic halogens, in particular bromine, potentially play an important role in the ozone depletion of the atmosphere. Understanding bromine behaviour in magmas is therefore crucial to properly evaluate the contribution of volcanic eruptions to atmospheric chemistry and their environmental impact. To date, bromine partitioning between silicate melts and the gas phase is very poorly constrained, with the only relevant experimental studies limited to investigation of synthetic melt with silicic compositions. In this study, fluid/melt partitioning experiments were performed using natural silicate glasses with mafic, intermediate and silicic compositions. For each co…

atmospheric chemistry010504 meteorology & atmospheric sciencesbromine[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSilicicarc magma010502 geochemistry & geophysics01 natural sciencesfluid/melt partitioningVolcanic Gaseschemistry.chemical_compoundGeochemistry and PetrologyEarth and Planetary Sciences (miscellaneous)eventPetrologyGeophysic0105 earth and related environmental sciencesMelt inclusionsevent.disaster_typeBasaltAndesiteSettore GEO/07 - Petrologia E PetrografiadegassingSilicatearc magmasSettore GEO/08 - Geochimica E VulcanologiaGeophysicschemistry13. Climate actionSpace and Planetary ScienceMagmaMaficGeology
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The geochemistry of Tl and its isotopes during magmatic and hydrothermal processes: The peralkaline Ilimaussaq complex, southwest Greenland

2014

Abstract We use thallium (Tl) concentrations, K/Rb, K/Tl and Rb/Tl ratios and Tl isotopes in minerals from the alkaline to peralkaline Ilimaussaq complex (South Greenland) to trace magmatic differentiation, crustal assimilation, magmatic degassing, ore precipitation and hydrothermal metasomatism. Closed-system magmatic differentiation is marked by a coherent decrease of K/Tl- and K/Rb-ratios, whereas crustal assimilation results in a strong Tl-enrichment, causing low K/Tl-ratios compared to K/Rb-ratios. Thallium isotopes show only slight changes during orthomagmatic differentiation and the assimilation of crustal material cannot be traced, since the isotopic composition of the average crust…

biologyGeochemistryMineralogyGeologyengineering.materialbiology.organism_classificationPeralkaline rockHydrothermal circulationMagmatic waterAstrophylliteGeochemistry and PetrologySilicate mineralsengineeringIgneous differentiationMetasomatismLileGeologyChemical Geology
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Controlling the spatial distribution of aluminum in ZSM-5 crystals

1993

Abstract The spatial distribution of aluminum over ZSM-5 crystals was systematically studied using electron microprobing on polished crystals. Crystals synthesized with TPABr as template exhibit a pronounced enrichment of aluminum in the crystal rim, essentially irrespective of the aluminum source employed, although aluminum sources with organic anions are favoring less inhomogeneous profiles. With 1,6-hexanediol or from totally inorganic reaction gels, crystals with completely homogeneous aluminum profiles are obtained, even if the crystals grow larger than 50 μm. In the 1,6-hexanediol system the homogeneous profiles could be changed to profiles similar to the TPABr system by addition of K…

biologyInorganic chemistryGeneral Engineeringchemistry.chemical_elementGeneral ChemistryElectronElectron microprobeSilicateIonCrystalchemistry.chemical_compoundchemistryAluminiumbiology.proteinGeneral Materials ScienceZSM-5Organic anionMicroporous Materials
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CCDC 660799: Experimental Crystal Structure Determination

2008

Related Article: T.F.Mastropietro, D.Armentano, E.Grisolia, C.Zanchini, F.Lloret, M.Julve, G.De Munno|2008|Dalton Trans.||514|doi:10.1039/b713960h

catena-(bis(mu~2~-Guanine)-hexa-aqua-di-copper(ii) bis(tetrafluoroborate) hexafluorosilicate)Space GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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CCDC 843438: Experimental Crystal Structure Determination

2012

Related Article: N.Marino, D.Armentano, G.De Munno, J.Cano, F.Lloret, M.Julve|2012|Inorg.Chem.|51|4323|doi:10.1021/ic202740b

catena-(bis(mu~2~-hydroxo)-(mu~2~-22'-bipyrimidine)-di-copper(ii) hexa-aqua-manganese(ii) hexafluorosilicate tetrahydrate)Space GroupCrystallographyCrystal SystemCrystal StructureCell ParametersExperimental 3D Coordinates
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Uptake of actinides by calcium silicate hydrate (C-S-H) phases

2018

Abstract The sorption of actinides (Th, U – Am) was studied in dependence of the solid-to-liquid (S/L) ratio (0.5–20.0 g/L) and the calcium-to-silicon (C:S) ratio. The C:S ratio was varied between 1.80 and 0.70 to simulate the changing composition of the C-S-H phases during cement degradation from high to low C:S ratios. The decrease of the calcium content in the C-S-H phases by time is accompanied by a decrease in pH in the corresponding suspensions from 12.6 to 10.2. X-ray photoelectron spectroscopy (XPS) of the C-S-H phases showed an increasing depletion of Ca on the surface with increasing C:S ratio in comparison to the composition of the solid phase as a whole. The sorption experiments…

cementTechnology02 engineering and technology010501 environmental sciences01 natural sciencesRedoxAmchemistry.chemical_compoundX-ray photoelectron spectroscopyGeochemistry and PetrologyOxidation statePhase (matter)Environmental ChemistryThCalcium silicate hydrateSpectroscopy0105 earth and related environmental sciencesUactinideshigh-energy resolution X-ray absorption near-edge structure (HR-XANES)SorptionX-ray photoelectron spectroscopy (XPS)Pu021001 nanoscience & nanotechnologyPollutionNpC-S-Hchemistryradioactive wasteSorptionAbsorption (chemistry)0210 nano-technologyddc:600Nuclear chemistry
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Influence of Sodium on the Structure and HDS Activity of Co–Mo Catalysts Supported ON Silica and Aluminosilicate

2000

Abstract Structural changes and catalytic performances of hydrodesulfurization (HDS) Co–Mo catalysts, supported on amorphous aluminosilicate (ASA) and amorphous SiO 2 were investigated as a function of the amount of sodium ions added to the supports. The catalysts were prepared according to the incipient wet impregnation method using (NH 4 ) 6 Mo 7 O 24 as molybdenum precursor and CoCl 2 or Co(NO 3 ) 2 as cobalt precursor. Structural and morphological characterisations of the materials were performed with X-ray diffraction (XRD) and surface area measurements (BET). In the case of the ASA-supported catalysts, increasing the amount of sodium resulted in a gradual decrease of the catalyst surf…

chemistryAluminosilicateSodiumInorganic chemistrychemistry.chemical_elementPhysical and Theoretical ChemistryHeterogeneous catalysisCristobaliteHydrodesulfurizationCobaltCatalysisCatalysisAmorphous solidJournal of Catalysis
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