Search results for "OCR"

showing 10 items of 13223 documents

Ion track template technology for fabrication of CdTe and CdO nanocrystals

2020

Abstract CdTe and CdO nanocrystals were synthesized by chemical deposition into a-SiO2/n-Si ion track template formed by 200 MeV Xe ion irradiation with the fluence of 108 ions/cm2. Depending on the temperature of the solution CdTe + CdO and single-phase CdO with a hexagonal crystal structure were obtained, respectively. The study of the current – voltage characteristics of the obtained structure with the single-phase CdO allows us to estimate the number of grain boundaries and the height of the potential barrier, as well as the n-type conductivity.

010302 applied physicsNuclear and High Energy PhysicsMaterials scienceIon trackPhysics::Medical PhysicsAnalytical chemistry02 engineering and technologyConductivity021001 nanoscience & nanotechnology01 natural sciencesFluenceCadmium telluride photovoltaicsIonCondensed Matter::Materials ScienceNanocrystal0103 physical sciencesRectangular potential barrierGrain boundary0210 nano-technologyInstrumentationNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms
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Unusual domain-wall motion in ferromagnetic semiconductor films with tetragonal anisotropy

2009

International audience; Magnetic field-driven domain-wall propagation in the flow regime is investigated in (Ga, Mn) As ferromagnetic semiconductor layers. Square-shape magnetic domains with an unexpected orientation of their edges, at pi/8 with respect to the anisotropy axes, are found. This is shown to arise from the effect of tetragonal magnetic anisotropy on domain-wall dynamics. Using a one-dimensional model for domain-wall motion and modeling domain growth by contour dynamics the shape and orientation of domains and their field range for existence are well reproduced. These results point to the key role of the vectorial nature of the order parameter in the dynamics of ferromagnetic do…

010302 applied physicsPhysicsCondensed matter physicsMagnetic domainDemagnetizing fieldCondensed Matter PhysicsMagnetocrystalline anisotropy01 natural sciencesMagnetic susceptibilityElectronic Optical and Magnetic MaterialsMagnetic anisotropyDomain wall (magnetism)Magnetic shape-memory alloy0103 physical sciences[PHYS.COND]Physics [physics]/Condensed Matter [cond-mat]Single domain010306 general physicsPhysical Review B
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Sub-nanosecond excitonic luminescence in ZnO:In nanocrystals

2019

The financial support of research European Union ERA.NET RUS_ST20170-51 . This work was partly supported by Russian Foundation for Basic Research, Russia , project No. 18-52-76002 . The sample preparation was carried out as part of SFERA II project -Transnational Access activities ( European Union 7th Framework Programme Grant Agreement N3126430 ).

010302 applied physicsRadiationMaterials scienceMorphology (linguistics)DopingKineticsAnalytical chemistrychemistry.chemical_elementTime-resolved luminescenceNanosecondVapour deposition01 natural sciences030218 nuclear medicine & medical imaging03 medical and health sciences0302 clinical medicineNanocrystalchemistry0103 physical sciences:NATURAL SCIENCES:Physics [Research Subject Categories]In [ZnO]Indium dopingLuminescenceInstrumentationScintillationIndium
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Diabetes and renin-angiotensin-aldosterone system: Implications for covid-19 patients with diabetes treatment management

2020

In the context of the COVID-19 continuous spreading, this paper focuses on the increased risk of diabetic patients regarding the metabolic control and the uncertainties related to SARS-CoV-2 infection. Chronic hyperglycaemia negatively affects the immune system, which triggers an increase of morbidity and mortality for viral infections. A key aspect of COVID-19 resides in the involvement of renin-angiotensin-aldosterone (RAAS) system that causes a cascade of reactions mediated by vasoactive peptides with implications in vasoconstriction, vascular permeability, oxidative stress remodelling and tissue injuries. Activation of RAAS at pulmonary level, is responsible for the local damage. Many q…

010405 organic chemistrybusiness.industry030209 endocrinology & metabolismContext (language use)Vascular permeabilityACEi ARBs COVID-19 Diabetes Of renin-angiotensin-aldosterone system RAAS SARS-CoV-2medicine.diseasemedicine.disease_causeBioinformatics01 natural sciences0104 chemical sciences03 medical and health sciences0302 clinical medicineImmune systemMetabolic control analysisDiabetes mellitusRenin–angiotensin systemmedicineGeneral Pharmacology Toxicology and Pharmaceuticsmedicine.symptombusinessVasoconstrictionOxidative stress
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The roles of microlites and phenocrysts during degassing of silicic magma

2022

Abstract Silicic magmas span a wide range of eruptive styles between explosive and effusive, and transitions between these styles are commonplace. Yet the triggers of switches in eruptive style remain poorly understood. Eruptions are mostly driven by degassing of magmatic water and their eruption style - effusive or explosive - is likely governed by the efficiency of outgassing as well as magma ascent rate. Microlites and phenocrysts are often purported to promote heterogeneous bubble nucleation and outgassing, both key variables in the degassing dynamics that become crucial in controlling the eruptive style. Here, in order to shed light on the role of nature, size and abundance of crystals…

010504 meteorology & atmospheric sciencesBubbleNucleationSilicicengineering.material010502 geochemistry & geophysics01 natural sciencesMicroliteMagmatic waterGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyMagmaRhyoliteEarth and Planetary Sciences (miscellaneous)engineeringPhenocrystPetrologyGeology0105 earth and related environmental sciencesEarth and Planetary Science Letters
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Essential features of the polytypic charoite-96 structure compared to charoite-90

2011

AbstractCharoite, ideally (K,Sr,Ba,Mn)15–16(Ca,Na)32[(Si70(O,OH)180)](OH,F)4·nH20, is a rock-forming mineral from the Murun massif in Yakutia, Sakha Republic, Siberia, Russia, where it occurs in a unique alkaline intrusion. Charoite occurs as four different polytypes, which are commonly intergrown in nanocrystallme fibres. We report the structure of charoite-96(a =32.11(6),b =19.77(4),c =7.23(1) Å, β = 95.85(9)°,V =4565(24) Å3, space groupP21/m),which was solvedab initioby direct methods on the basis of 2676 unique electron diffraction reflections collected by automated diffraction tomography and refined toR1/wR2=0.34/0.37. The structure of charoite-96 is related to that of the charoite-90,…

010504 meteorology & atmospheric sciencesElectron crystallographyAb initiocrystal structure analysisengineering.material010502 geochemistry & geophysicscharoite polytypes01 natural sciencesSilicateNanocrystalline materialchemistry.chemical_compoundCrystallographyelectron crystallographychemistryOctahedronElectron diffractionGeochemistry and PetrologyGroup (periodic table)Charoitecharoite polytypes; crystal structure analysis; electron crystallography; electron diffraction; electron diffraction tomographyengineeringelectron diffractionelectron diffraction tomography0105 earth and related environmental sciences
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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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Origin of primitive ultra-calcic arc melts at crustal conditions — Experimental evidence on the La Sommata basalt, Vulcano, Aeolian Islands

2016

International audience; To interpret primitive magma compositions in the Aeolian arc and contribute to a better experimental characterization of ultra-calcic arc melts, equilibrium phase relations have been determined experimentally for the La Sommata basalt (Som-1, Vulcano, Aeolian arc). Som-1 (Na2O + K2O = 4.46 wt.%, CaO = 12.97 wt.%, MgO = 8.78 wt.%, CaO/Al2O3 = 1.03) is a reference primitive ne-normative arc basalt with a strong ultra-calcic affinity. The experiments have been performed between 44 and 154 MPa, 1050 and 1150 °C and from NNO + 0.2 to NNO + 1.9. Fluid-present conditions were imposed with H2O–CO2 mixtures yielding melt H2O concentrations from 0.7 to 3.5 wt.%. Phases encount…

010504 meteorology & atmospheric sciencesGeochemistryLiquidusengineering.material010502 geochemistry & geophysics01 natural sciencesPrimitive arc magmasMantle (geology)law.inventionVulcanoGeochemistry and PetrologylawUltra-calcic[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/VolcanologyPlagioclaseCrystallizationPetrology0105 earth and related environmental sciencesBasaltAeolian arcOlivineSettore GEO/07 - Petrologia E PetrografiaCrustGeophysics13. Climate actionPrimitive arc magmas Ultra-calcic Experiments Phase equilibria Vulcano Aeolian arcengineeringPhenocrystPhase equilibriaExperimentsGeology
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Quantitative models of hydrothermal fluid–mineral reaction: The Ischia case

2013

Abstract The intricate pathways of fluid–mineral reactions occurring underneath active hydrothermal systems are explored in this study by applying reaction path modelling to the Ischia case study. Ischia Island, in Southern Italy, hosts a well-developed and structurally complex hydrothermal system which, because of its heterogeneity in chemical and physical properties, is an ideal test sites for evaluating potentialities/limitations of quantitative geochemical models of hydrothermal reactions. We used the EQ3/6 software package, version 7.2b, to model reaction of infiltrating waters (mixtures of meteoric water and seawater in variable proportions) with Ischia’s reservoir rocks (the Mount Ep…

010504 meteorology & atmospheric sciencesGeochemistryMineralogyengineering.material010502 geochemistry & geophysics01 natural sciencesHydrothermal circulationHydrothermal systemGeochemistry and PetrologyMount Epomeo Green TuffPlagioclaseHydrothermal fluidIschia Island Reaction path modelling EQ3/60105 earth and related environmental sciencesMineralSettore GEO/08 - Geochimica E Vulcanologia13. Climate actionMeteoric waterengineeringPhenocrystSeawaterIschiaSaturation (chemistry)Clay mineralsGeologyGeochimica et Cosmochimica Acta
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Melt inclusions track melt evolution and degassing of Etnean magmas in the last 15 ka

2019

We present major elements compositions and volatiles contents of olivine-hosted melt inclusions from Etna volcano (Italy), which extend the existing database with the aim of interpreting the chemical variability of Etnean magmas over the last 15 ka. Olivine phenocrysts were selected from the most primitive Fall Stratified (FS) eruptive products of picritic composition (Mg# = 67–70, Fo 89–91 ), the Mt. Spagnolo eccentric lavas (Mg# = 52–64, Fo 82–88 ) and among the more recent 2002–2013 eruptive products (Mg# = 33–53, Fo 68–83 ). Crystal fractionation and degassing processes were modeled at temperatures of 1050–1300 °C, pressures <500 MPa, and oxygen fugacity between 1 and 2 log units abo…

010504 meteorology & atmospheric sciencesGeochemistryVolatile contentengineering.material010502 geochemistry & geophysics01 natural sciencesMantle (geology)Mineral redox bufferDegassingGeochemistry and PetrologySilicate melt inclusionPlagioclase0105 earth and related environmental sciencesMelt inclusionsFractional crystallization (geology)OlivineSpinelMelt differentiationGeologyEtna Silicate melt inclusions Volatile contents Melt differentiation Degassing13. Climate action[SDU]Sciences of the Universe [physics]engineeringPhenocrystEtnaGeology
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