Search results for " petrology"

showing 10 items of 1353 documents

Humidity effects on gravitational settling and Brownian diffusion of atmospheric aerosol particles

1977

The dependency on relative humidity of the settling velocity of aerosol particles in stagnant air and of the diffusion coefficient due to Brownian motion of aerosol particles was computed for six aerosol types and different particles sizes in dry state. The computations are based (1) on mean bulk densities of dry aerosol particles obtained from measurements or from the knowledge of the chemical composition of the particles, (2) on micro-balance measurements of the water uptake per unit mass of dry aerosol substance versus water activity at thermodynamic equilibrium, and (3) on measurements of the equilibrium water activity of aqueous sea salt solutions. The results show a significant depend…

Materials scienceThermodynamic equilibriumDiffusionThermodynamicsHumidityrespiratory systemAtmospheric sciencescomplex mixturesAerosolGeophysicsDeposition (aerosol physics)SettlingGeochemistry and PetrologyParticleRelative humidityPhysics::Atmospheric and Oceanic PhysicsPure and Applied Geophysics PAGEOPH
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Optical studies of Y3(Al,Ga)5O12:Ce3+,Cr3+,Nd3+ nano-phosphors obtained by the Pechini method

2019

The Y-3(Al,Ga)(5)O-12:Ce3+,Cr3+,Nd3+ (YAGG) nano-phosphors with homogeneous particle-size distribution, low aggregation and average crystalline size of about 65 nm were obtained using a modified Pechini method. Only slight aggregation of the crystallites occurs after post-annealing at 1100 degrees C. The intense Ce3+ bands in the excitation spectra of the Ce3+,Cr3+,Nd3+ co-doped materials monitoring the Cr3+ emission at 690 nm indicate energy transfer from Ce(3+ )to Cr3+. Weak Nd3+ lines are observed, as well. In addition, the emission of Nd3+ at 1060 nm with excitation of Ce3+ and Cr3+ confirms the Ce3+/Cr3+ to Nd3+ energy transfer. The short average luminescence decay times for the Ce3+ e…

Materials scienceThermoluminescence3+Analytical chemistryPhosphor02 engineering and technologyGeneral Chemistry010402 general chemistry021001 nanoscience & nanotechnology01 natural sciencesThermoluminescenceCe0104 chemical sciencesPersistent luminescenceGeochemistry and PetrologyHomogeneousRare earthNano-NIR persistent luminescenceNano-phosphorCrystallite0210 nano-technologyLuminescenceExcitationSettore CHIM/02 - Chimica FisicaJournal of Rare Earths
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Simulating permeability reduction by clay mineral nanopores in a tight sandstone by combining computer X-ray microtomography and focussed ion beam sc…

2021

Solid earth 12(1), 1 - 14 (2021). doi:10.5194/se-12-1-2021

Materials scienceX-ray microtomography550010504 meteorology & atmospheric sciencesIon beamScanning electron microscopeGeography & travelStratigraphySoil ScienceMineralogy010502 geochemistry & geophysics01 natural sciences550 Earth scienceslcsh:StratigraphyGeochemistry and Petrologyddc:550Porositylcsh:QE640-6990105 earth and related environmental sciencesEarth-Surface Processesddc:910lcsh:QE1-996.5PaleontologyGeologyMicroporous materialPetroleum reservoir550 Geowissenschaftenlcsh:GeologyPermeability (earth sciences)GeophysicsTomography
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2020

Abstract. Residual pressure can be preserved in mineral inclusions, e.g. quartz-in-garnet, after exhumation due to differential expansion between inclusion and host crystals. Raman spectroscopy has been applied to infer the residual pressure and provides information on the entrapment temperature and pressure conditions. However, the amount of residual pressure relaxation cannot be directly measured. An underestimation or overestimation of residual pressure may lead to significant errors between calculated and actual entrapment pressure. This study focuses on three mechanisms responsible for the residual pressure modification: (1) viscous creep; (2) plastic yield; (3) proximity of inclusion …

Materials scienceYield (engineering)010504 meteorology & atmospheric sciencesStratigraphyNucleationPaleontologySoil ScienceThermodynamicsGeologyRadius010502 geochemistry & geophysicsResidual01 natural sciencessymbols.namesakeGeophysicsCreepGeochemistry and PetrologysymbolsRelaxation (physics)Inclusion (mineral)Raman spectroscopy0105 earth and related environmental sciencesEarth-Surface ProcessesSolid Earth
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Characterisation of Apatites as Potential Uranium Reference Materials for Fission-track Dating by LA-ICP-MS

2015

We report homogeneity tests on large natural apatite crystals to evaluate their potential as U reference materials for apatite fission-track (AFT) thermochronology by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS). The homogeneity tests include the measurements of major element concentrations by electron probe microanalysis (EPMA), whereas for U concentration, isotope dilution (ID) ICP-MS and laser ablation (LA) ICP-MS were employed. Two apatite crystals are potential reference materials for LA-ICP-MS analysis: a 1 cm3 fraction of a Durango crystal (7.5 μg g−1 U) and a 1 cm3 Mud Tank crystal (6.9 μg g−1 U). The relative standard deviation (1 RSD) of the U concentrat…

Materials sciencechemistryGeochemistry and PetrologyLa icp msvisual_artAnalytical chemistryvisual_art.visual_art_mediumchemistry.chemical_elementGeologyUraniumFission track datingApatiteNuclear chemistryGeostandards and Geoanalytical Research
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High-pressure crystal structure investigation of synthetic Fe2SiO4 spinel.

2011

AbstractThe crystal structure of Fe2SiO4 spinel at room temperature was investigated at seven different pressures by X-ray diffraction, using a diamond anvil cell to examine the influence of Fe substitution on ringwoodite behaviour at high pressure. The results compared with those of a pure Mg endmember show that the substitution of Fe into the spinel structure causes only small changes in the compression rate of coordination polyhedra and the distortion of the octahedron. The data show that the compression rate for the octahedron and tetrahedron in (Mg,Fe)2SiO4 can be considered statistically equal for FeO6 and MgO6, as well as for SiO4 in both the endmembers. This shows why almost identic…

Materials sciencehigh pressure; X-ray diffraction; single crystal; synthetic Fe2SiO4 spinel010504 meteorology & atmospheric scienceshigh pressure X-ray diffraction single crystal synthetic Fe2SiO4 spinelX ray diffractionSpinel550 - Earth sciencesCrystal structureengineering.material01 natural scienceshigh pressure; X ray diffraction; single crystal; synthetic Fe2SiO4 spinelX-ray diffractionCrystallographyRingwooditehigh pressureOctahedronsynthetic Fe2SiO4 spinelGeochemistry and PetrologyX-ray crystallographyengineeringTetrahedronsingle crystalSingle crystal0105 earth and related environmental sciencesSolid solution
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Validation of matrix diffusion modeling

2010

Abstract Crystalline rock has been chosen as the host medium for repository of highly radioactive spent nuclear fuel in Finland. Radionuclide transport takes place along water-carrying fractures, and matrix diffusion has been indicated as an important retarding mechanism that affects the transport of mobile fission and activation products. The model introduced here for matrix diffusion contains a flow channel facing a porous matrix with stagnant water into which tracer molecules advected in the channel can diffuse. In addition, the possibility of a finite depth of the matrix and an initial tracer distribution (‘contamination’) in the matrix are included in the model. In order to validate th…

Matrix (mathematics)GeophysicsExperimental systemGeochemistry and PetrologyChemistryElectrical resistivity and conductivityFissionTRACERAnalytical chemistryMechanicsDiffusion (business)PorosityIonPhysics and Chemistry of the Earth, Parts A/B/C
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CO2-recycling to the deep convecting mantle

2006

Institut fur Geowissenschaften, Johann Wolfgang Goethe-Universitat Frankfurt, 60054 Frankfurt, Germany (f.brenker@ em.uni-frankfurt.de) Max Planck Institute for Chemistry, Mainz, Germany (cvollmer@mpch-mainz.mpg.de) Ghent University, Department of Analytical Chemistry, Belgium (Laszlo.Vincze@UGent.be) University of Antwerp, Department of Chemistry, Belgium (bart.vekemans@ua.ac.be; koen.janssens@ua.ac.be) Institute of Experimental Physics, University of Debrecen, Hungary (szaloki@tigris.klte.hu) Institut fur Geowissenschaften, Johannes Gutenberg-Universitat, Mainz, Germany (nasdala@uni-mainz.de) KM Diamond Exploration Ltd., Vancouver, Canada (felixvkaminsky@cs.com)

Max planck instituteGeochemistry and PetrologyGeochemistryMantle (geology)GeologyGeochimica et Cosmochimica Acta
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Contrasting shell growth strategies in two Mediterranean bivalves revealed by oxygen-isotope ratio geochemistry: The case of Pecten jacobaeus and Gly…

2019

International audience; High-resolution stable-isotope ratio data (delta O-18, delta O-18) were used to study growth strategies of two bivalve species, Pecten jacobaeus (calcitic shell) and Glycymeris pilosa (aragonitic shell) from the North Adriatic Sea. The principal objectives of this study were to identify the period of the year when the growth line is formed in the shell of two target species, to identify the main growing season of these two species, to identify the environmental drivers of shell growth, and to evaluate the potential applicability of delta O-18 and delta O-18 values for the reconstruction of environmental variability. Samples were collected from the North Adriatic Sea …

Mediterranean climate010504 meteorology & atmospheric sciencesPecten jacobaeusTemperature salinity diagramsGrowing seasonMediterranean010502 geochemistry & geophysics01 natural sciencesBivalve shellsWater columnSclerochronologyGeochemistry and PetrologySclerochronology14. Life underwaterAdriatic0105 earth and related environmental sciencesbiologyACLGeologyOxygen isotope ratio cyclebiology.organism_classificationOceanographyStable-isotope ratio geochemistrySeawater[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeologysclerochronology ; Mediterranean ; Adriatic ; stable-isotope ratio geochemistry ; bivalve shells
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The late Hauterivian Faraoni "Oceanic Anoxic Event" at Río Argos (southern Spain): an assessment on the level of oxygen depletion.

2013

14 pages; International audience; An integrated study of multiple geochemical proxies (TOC, δ13Ccarb, trace metallic elements, iron speciation) on the late Hauterivian Faraoni Oceanic Anoxic Event has been performed along the hemi-pelagic section of Río Argos (south-eastern Spain) in order to better constrain the environmental perturbations linked to this event in the Subbetic domain. In the studied section, the TOC is relatively low (b0.5 wt.%) except for one sample at the base of the Faraoni horizon, where it reaches 1.5 wt.%. The δ13Ccarb signal is characterized by a minor long-term increase, primarily attributed to an enhanced organic matter burial. However, both organic and isotopic si…

Mediterranean climate010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesIron cycle010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesLate HauterivianCarbon cyclePaleontologyIron cycleGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryFaraoni EventOrganic matter0105 earth and related environmental scienceschemistry.chemical_classificationHorizon (archaeology)GeologyCarbon cycle[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryAnoxic watersOAEDiagenesis[ SDE.MCG ] Environmental Sciences/Global ChangeschemistryProductivity (ecology)Oxygen concentration variations[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeology
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