Search results for "noble ga"

showing 10 items of 59 documents

Noble gas magmatic signature of the Andean Northern Volcanic Zone from fluid inclusions in minerals

2021

Trace volatile elements like He are key for understanding the mantle source signature of magmas and to better constrain the relative roles of subduction and crustal processes to the variability of along-arc chemical and isotopic signatures of magmatic fluids. Here we report on noble gas abundances and isotopic data of Fluid Inclusions (FIs) in eruptive products and/or fumarolic gases from the Colombia-Ecuador segment of Andean Northern Volcanic Zone (NVZ). FIs in olivine phenocrysts from Ecuador (El Reventador, Cotopaxi and Tungurahua) yield air-normalized corrected He-3/He-4 ratios of 7.0-7.4 R-A, within the MORB range (8 +/- 1 R-A). With exception of the Cotopaxi lavas (opx = 50 km at the…

010504 meteorology & atmospheric sciencesGeochemistryAndean Volcanic Belt Helium voclanic gases Crustal thickness Fluid inclusions Helium Noble gases Northern Volcanic Zoneengineering.material010502 geochemistry & geophysics01 natural sciencesHeliumMantle (geology)Noble gaseGeochemistry and Petrology[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyCrustal thickneFluid inclusions[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentVolatilesFluid inclusions0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryOlivineSubductionGeologyNorthern Volcanic ZoneFluid inclusionNoble gasesCrustal thicknessVolcanoAndean Volcanic BeltengineeringPhenocrystGeology
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Geochemistry of Noble Gases and CO2 in Fluid Inclusions From Lithospheric Mantle Beneath Wilcza Góra (Lower Silesia, Southwest Poland)

2018

Knowledge of the products originating from the subcontinental lithospheric mantle (SCLM) is crucial for constraining the geochemical features and evolution of the mantle. This study investigated the chemistry and isotope composition (noble gases and CO2 ) of fluid inclusions (FI) from selected mantle xenoliths originating from Wilcza Góra (Lower Silesia, southwest Poland), with the aim of integrating their petrography and mineral chemistry. Mantle xenoliths are mostly harzburgites and sometimes bear amphiboles, and are brought to the surface by intraplate alkaline basalts that erupted outside the north-easternmost part of the Eger (Ohře) Rift in Lower Silesia. Olivine (Ol) is classified int…

010504 meteorology & atmospheric sciencesGeochemistryengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)chemistry.chemical_compoundNoble gasenoble gases CO2 fluid inclusions mantle xenoliths European mantle SCLM MORB metasomatismFluid inclusionsMetasomatismlcsh:ScienceAmphibole0105 earth and related environmental sciencesBasaltEuropean mantleOlivineSCLMmetasomatismPartial meltingAmbientaleFluid inclusionMORBMantle xenolithSilicatemantle xenolithsfluid inclusionschemistrynoble gasesengineeringGeneral Earth and Planetary Scienceslcsh:QCO2Geology
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Strongly SiO2-undersaturated, CaO-rich kamafugitic Pleistocene magmatism in Central Italy (San Venanzo volcanic complex) and the role of shallow dept…

2020

The Pleistocene (~460–265 ka) San Venanzo volcanic complex belongs to the IAP (Intra-Apennine Province) in central Italy, which comprises at least four small Pleistocene monogenetic volcanoes plus several unrooted pyroclastic deposits with peculiar mineralogical and whole-rock chemical compositions. San Venanzo products are strongly SiO2-undersaturated, CaO- and MgO-rich and show ultrapotassic serial character. The relatively common occurrence of calcite in the pyroclastic rocks and the overall high CaO content are interpreted in literature as primary mineral. The main rock facies at San Venanzo are calcite-rich scoria and lapilli tuffs, with minor massive lava flows, and a rare pegma…

010504 meteorology & atmospheric sciencesultrapotassicGeochemistryPyroclastic rockCarbonatite; Kamafugite; mantle plumes; noble gases; Roman comagmatic region; subduction; ultrabasic; ultrapotassicengineering.material010502 geochemistry & geophysicsKamafugite01 natural sciencesUltramafic rockCarbonatiteultrabasicRoman comagmatic region0105 earth and related environmental sciencesPeridotitegeographygeography.geographical_feature_categoryFractional crystallization (geology)Olivinemantle plumesVolcanic rockIgneous rocknoble gasesengineeringGeneral Earth and Planetary SciencesLeucitesubductionGeology
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A TWO-COMPONENT MANTLE EXTENDING FROM MT. ETNA TO HYBLEAN PLATEAU (EASTERN SICILY) AS INFERRED BY AN INTEGRATED APPROACH WITH NOBLE GASES, TRACE ELEM…

2012

A TWO-COMPONENT MANTLE EXTENDING FROM MT. ETNA TO HYBLEAN PLATEAUSettore GEO/07 - Petrologia E PetrografiaINTEGRATED APPROACH WITH NOBLE GASES TRACE ELEMENTS AND ISOTOPIC GEOCHEMISTRY.
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Sorption Kinetics of Xenon on MFI-Type Zeolite Molecular Sieves

1990

Kinetic uptake data for xenon adsorbed onto large and uniform silicalite-I crystals are presented over a temperature range of 121 K to 296 K. — Adsorption isotherms and corrected diffusion coefficients derived from the uptake curves are given. The heat of adsorption and activation energy of diffusion were estimated from the plots of reciprocal temperature against the logarithm of equilibrium pressure and corrected diffusion coefficients, respectively. — While the corrected diffusion coefficient is independent of coverage for the higher temperatures, it decreases significantly at the lower temperatures investigated (<170 K) when the limiting adsorption capacity has been reached. — Comparing …

AdsorptionXenonChemistryGeneral Chemical EngineeringDiffusionPhysical chemistryNoble gaschemistry.chemical_elementThermodynamicsSorptionActivation energyAtmospheric temperature rangeOrder of magnitudeBerichte der Bunsengesellschaft für physikalische Chemie
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Constrains on mantle, slab and crustal contributions to major volatiles and noble gases along the Andean Volcanic Belt

2020

Arc volcanism Andean Volcanic Belt Volcanic gas Volatiles Noble gas
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Sensitivity of noble gas NMR parameters to the heterocyclic ring proximity. Density functional theory studies of Ne–furan and Ar–furan complexes

2014

Theoretical modeling of noble gas interaction with furan as a simple heterocyclic ring was performed. The structures of neon–furan and argon–furan complexes were calculated at the MP2, M06-2X, CAM-B3LYP, APFD, and VSXC levels of theory using 6-311++G** basis set. The predicted 21Ne and 39Ar NMR chemical shifts for the Ne–furan and Ar–furan complexes calculated with pcS-3 and aug-pcS-3 basis sets were sensitive to the presence of the aromatic furan ring. Our results indicate a higher sensitivity of the neon and argon NMR probes than the previously reported 3He NMR spectroscopic parameters in studies of small heterocyclic rings containing the oxygen atom.

ArgonCarbon-13 NMR satellitemolecular modelingChemical shiftfuranOrganic Chemistry39Ar NMR spectrachemistry.chemical_elementNoble gasRing (chemistry)chemistry.chemical_compoundNeonchemistryComputational chemistryFuran21Ne NMR spectraGIAO NMR calculationsDensity functional theoryChemistry of Heterocyclic Compounds
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Ellipsometric thickness and coverage of physisorbed layers of Xe, Kr, Ar and N2 on graphite

1990

Multilayer isotherms of Xe, Kr, Ar and N2 physisorbed on graphite (001) have been studied by ellipsometry. It is shown that the model of Dignam and Fedyk provides an excellent basis for the interpretation of the ellipsometric thickness in terms of the coverage and the polarizability of the admolecules. For N2 conclusions concerning the orientation of the molecule are drawn.

ArgonKryptonchemistry.chemical_elementMineralogyNoble gasSurfaces and InterfacesCondensed Matter PhysicsMolecular physicsSurfaces Coatings and FilmsXenonPhysisorptionchemistryEllipsometryPolarizabilityMaterials ChemistryGraphiteSurface Science
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Investigation of the He solubility in H2O-CO2 bearing silicate liquids at moderate pressure: a new experimental method

2000

We have designed the first available experimental method capable to investigate the solubility of inert gases in H2O–CO2 bearing silicate melts in a large range of pressures. The method overcomes the difficulties imposed by the physical state of volatiles at room conditions. Experiments were done by using an internally heated pressure vessel, where sealed capsules containing the sample are introduced. The peculiarity of the method consists in the capability of loading, in accurately known proportions (even lower than ppm), volatiles in a gaseous state at room conditions. Gas is loaded as a weighed amount of a gas-bearing glass, which was previously prepared by using the same gas as a pressu…

BasaltsolubilityMineralogyNoble gaschemistry.chemical_elementheliumSilicatePressure vesselMantle (geology)chemistry.chemical_compoundpressureGeophysicschemistryChemical engineeringexperimental studiessilicate meltsSpace and Planetary ScienceGeochemistry and Petrologyexperimental studies; helium; pressure; silicate melts; solubilityEarth and Planetary Sciences (miscellaneous)SolubilityDissolutionGeologyHelium
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Relativistic coupled cluster calculations of the electronic structure of KrH+, XeH+ and RnH+

2012

Potential energy curves of NgH+ cations (Ng = Kr, Xe, Rn) were obtained by using four-component relativistic CCSD(T) coupled cluster calculations. Dissociation energies, equilibrium bond lengths, electronic properties, such as dipole moments and electric field gradients at the nuclei, and the related spectroscopic parameters of the electronic ground state have been determined. The results obtained for KrH+ and XeH+ are in good agreement with available experimental data, while those for RnH+ have been determined for the first time at this level of theory.

Bond lengthDipoleCoupled clusterChemistryElectric fieldRelativistic effects Coupled cluster Protonated noble gasesElectronic structurePhysical and Theoretical ChemistryAtomic physicsGround statePotential energyDissociation (chemistry)Theoretical Chemistry Accounts
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