Search results for "Slab"

showing 10 items of 88 documents

ATOMISTIC CALCULATIONS OF (110) SURFACE RELAXATION FOR PEROVSKITE TITANATES

1999

Using a shell model, for the first time the (110) surface relaxations are calculated for SrTiO 3 and BaTiO 3 perovskites. The positions of atoms in 16 near-surface layers placed atop a slab of rigid ions are calculated. Strong surface rumpling and surface-induced dipole moments perpendicular to the surface are predicted for both the O-terminated and Ti-terminated surfaces.

Surface (mathematics)Condensed matter physicsChemistrySHELL modelRelaxation (NMR)Surfaces and InterfacesCondensed Matter PhysicsSurfaces Coatings and FilmsIonDipoleMaterials ChemistrySlabPerpendicularPerovskite (structure)Surface Review and Letters
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Computer Modeling of Defects and Surfaces in Advanced Perovskite Ferroelectrics

2000

The (110) surface relaxations are calculated for SrTiO3 and BaTiO3 perovskites. The positions of atoms in 16 near-surface layers placed atop a slab of rigid ions are optimized. Strong surface rumpling and surface-induced dipole moments perpendicular to the surface are predicted for both the O-terminated and Ti-terminated surfaces. Calculated optical properties of basic point defects – F-type centres and hole polarons – in KNbO3 are used for the interpretation of available experimental data.

Surface (mathematics)Materials scienceCondensed matter physicsGeneral EngineeringGeneral Physics and AstronomyPolaronCrystallographic defectIonCondensed Matter::Materials ScienceDipoleComputational chemistrySlabPerpendicularPerovskite (structure)Japanese Journal of Applied Physics
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Atomic and Electronic Structure of the Corundum (0001) Surface

1996

AbstractThe electronic structure and geometry of the Al terminated corundum (0001) surface were studied using a slab model within the ab-initio Hartree-Fock technique. The distance between the top Al plane and the next O basal plane is found to be considerably reduced on relaxation (by 0.57 Å, i.e. by 68% of the corresponding interlayer distance in the bulk). An interpretation of experimental photoelectron spectra (UPS Hel) and metastable impact electron spectra (MIES) is given. Calculated projected densities of states exhibit a strong dependence on the relaxation of surface atoms.

Surface (mathematics)Materials sciencePlane (geometry)MetastabilityPhysics::Atomic and Molecular ClustersengineeringSlabRelaxation (physics)CorundumElectronic structureengineering.materialMolecular physicsSpectral lineMRS Proceedings
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The ultimate message : a study of medieval tombstones in ducal Burgundy : 12th-16th centuries

2011

The tombstone has long been neglected by historians. As obituaries and wills, tombstones reveal as much the relationship of the deceased to death that the management of their memory by their heirs. This study first shows the wealth of medieval Burgundy graves goods. Typological diversity adds to the richness of iconography with large amounts of effigial monuments. Tombs materialize burial of prestige. Originally reserved for prelates and princes, burial ad ecclesiam progressively extended to the feudal aristocracy and the bourgeoisie. The location and the materialization of a burial monument also reflect the evolution of medieval piety. Epigraphy and iconography show the mutation of "gothic…

TombMoyen AgeSépultureBurialGisant[ SHS.HIST ] Humanities and Social Sciences/HistoryPlate tombeMonumentDalle funéraireTombeEpigraphyDeathIncised slabsRecumbent figureIconography[SHS.HIST] Humanities and Social Sciences/HistoryMiddle AgesTombstoneMort[SHS.HIST]Humanities and Social Sciences/HistoryEpigraphieIconographie
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Magmatism Along Lateral Slab Edges: Insights From the Diamante-Enotrio-Ovidio Volcanic-Intrusive Complex (Southern Tyrrhenian Sea)

2019

Volcanic‐intrusive complexes often formed along lateral slab edges as a consequence of subduction‐induced mantle flow. We investigate this process in the southern Tyrrhenian Sea by integrating multibeam bathymetry, seismic‐reflection data, regional magnetic anomalies data, and seismological data. The interpretation of the data highlights the presence of magmatic intrusions that locally reach the seafloor forming volcanic edifices. Chimneys, lava flows, and laccoliths are observed beneath and surrounding the volcanoes. The emplacement and cooling of the magma occurred during the Brunhes Chron. The volcanoes are not active even if the hydrothermal activity occurs. The volcanic‐intrusive compl…

Tyrrhenian Seageographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E Sedimentologicacalabrian acrccalabrian acrc; flat-topped seamount; slab tearing; STEP fault; subduction-induced mantle flow; Tyrrhenian SeaSettore GEO/03 - Geologia StrutturaleGeochemistryflat-topped seamountsubduction-induced mantle flowCalabrian Arc; flat-topped seamount; slab tearing; STEP fault; subduction-induced mantle flow; Tyrrhenian SeaCalabrian ArcGeophysicsCalabrian Arc Tyrrhenian Sea Subduction-induced mantle flow STEP fault slab tearing flat-topped seamount.VolcanoGeochemistry and PetrologySettore GEO/11 - Geofisica ApplicataMagmatismSlabslab tearingGeologySTEP faultCalabrian Arc Tyrrhenian Sea subduction induced mantle flow STEP fault slab tearing flat‐topped seamount
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Rates of convergence to equilibrium for collisionless kinetic equations in slab geometry

2017

This work deals with free transport equations with partly diffuse stochastic boundary operators in slab geometry. Such equations are governed by stochastic semigroups in $L^{1}$ spaces$.\ $We prove convergence to equilibrium at the rate $O\left( t^{-\frac{k}{2(k+1)+1}}\right) \ (t\rightarrow +\infty )$ for $L^{1}$ initial data $g$ in a suitable subspace of the domain of the generator $T$ where $k\in \mathbb{N}$ depends on the properties of the boundary operators near the tangential velocities to the slab. This result is derived from a quantified version of Ingham's tauberian theorem by showing that $F_{g}(s):=\lim_{\varepsilon \rightarrow 0_{+}}\left( is+\varepsilon -T\right) ^{-1}g$ exists…

Work (thermodynamics)Generator (category theory)010102 general mathematicsBoundary (topology)Geometry[MATH.MATH-FA]Mathematics [math]/Functional Analysis [math.FA]01 natural sciencesDomain (mathematical analysis)Functional Analysis (math.FA)010101 applied mathematicsMathematics - Functional AnalysisMathematics - Analysis of PDEsBounded functionConvergence (routing)SlabFOS: Mathematics[MATH.MATH-AP]Mathematics [math]/Analysis of PDEs [math.AP]0101 mathematicsAnalysisSubspace topologyMathematicsMathematical physicsAnalysis of PDEs (math.AP)
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2D slab models of TiO2 nanotubes for simulation of water adsorption: Validation over a diameter range

2020

Financial support provided by Scientific Research Project for Students and Young Researchers Nr. SJZ/2019/2 realized at the Institute of Solid State Physics, University of Latvia is greatly acknowledged. Institute of Solid State Physics, University of Latvia as the Center of Excellence has received funding from the European Union’s Horizon 2020 Framework Programme H2020-WIDESPREAD-01-2016-2017-TeamingPhase2 under Grant Agreement No. 739508, project CAMART 2 .

Work (thermodynamics)NanotubeSlab modelMaterials scienceWater adsorptionGeneral Physics and Astronomy02 engineering and technology01 natural sciencesDFTNanomaterialsCondensed Matter::Materials ScienceAdsorptionLattice constant0103 physical sciences:NATURAL SCIENCES:Physics [Research Subject Categories]TiO2Water splitting010302 applied physicsNanotubes021001 nanoscience & nanotechnologylcsh:QC1-999Chemical physicsSlabWater splitting0210 nano-technologylcsh:PhysicsPhotocatalytic water splitting
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Experimental demonstration and numerical study of plasmon-soliton waves

2019

Merging the fields of plasmonics and nonlinear optics authorizes a variety of fascinating and original physical phenomena. In this work, we specifically study the combination of the strong light confinement ability of surface plasmon polaritons (SPP) with the beam self-trapping effect in a nonlinear optical Kerr medium. Although this idea of plasmon-soliton has been the subject of numerous theoretical papers since the eighties [1–4], up to now, no experimental evidence had been revealed yet. In the present study, a proper structure (Fig. 1a) has been designed and fabricated allowing the first experimental demonstration of these hybrid nonlinear waves merging spatial solitons and SPP. To be …

[PHYS.PHYS.PHYS-OPTICS] Physics [physics]/Physics [physics]/Optics [physics.optics]slab waveguidePhysics::Optics02 engineering and technology01 natural sciencesnonlinear waveguideslaw.invention010309 opticsmodellingKerr effetOpticslaw0103 physical sciencesplasmon-soliton waveschalcogneideself-focusingPlasmonPhysics[PHYS.PHYS.PHYS-OPTICS]Physics [physics]/Physics [physics]/Optics [physics.optics]business.industryNonlinear opticsspatial solitonsSelf-focusing021001 nanoscience & nanotechnologyLaserPolarization (waves)Surface plasmon polaritonLight intensityFemtosecond0210 nano-technologybusiness
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The role of slabs and oceanic plate geometry in the net rotation of the lithosphere, trench motions, and slab return flow

2012

International audience; [1] Absolute plate motion models with respect to a deep mantle reference frame (e.g., hot spots) typically contain some net rotation (NR) of the lithosphere. Global mantle flow models for the present-day plate setting reproduce similarly oriented NRs but with amplitudes significantly smaller than those found in some high NR Pacific hot spot reference frames. It is therefore important to understand the mechanisms of NR excitation, which we attempt here with two-dimensional cylindrical models of an idealized Pacific domain. We study the influence of slab properties, oceanic ridge position, continental keels, and a weak asthenospheric layer on NR and trench migration. F…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicstrench motions.slab dynamics[SDE.MCG]Environmental Sciences/Global Changestrench motionslithosphere-mantle interactionsnet rotation of the lithosphere
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Tectonics and seismicity of the Tindari Fault System, southern Italy: Crustal deformations at the transition between ongoing contractional and extens…

2006

The Tindari Fault System (southern Tyrrhenian Sea, Italy) is a regional zone of brittle deformation located at the transition between ongoing contractional and extensional crustal compartments and lying above the western edge of a narrow subducting slab. Onshore structural data, an offshore seismic reflection profile, and earthquake data are analyzed to constrain the present geometry of the Tindari Fault System and its tectonic evolution since Neogene, including the present seismicity. Results show that this zone of deformation consists of a broad NNW trending system of faults including sets of right-lateral, left-lateral, and extensional faults as well as early strike-slip faults reworked …

accommodation zoneseismicityTectonics seismicity subducting slab Tindari fault systemaccommodation zone; seismicity
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