Search results for "grain"

showing 10 items of 752 documents

Effect of surface disorder on the domain structure of PLZT ceramics

2017

ABSTRACTPb1-xLax(Zr0.65Ti0.35)1-x/4O3 (PLZT x/65/35) ceramics were studied by Piezoresponse Force Microscopy in order to understand the origin of domain structure as a function of La content. We show that the domain topology is mainly determined by the composition and grain size. The characteristic correlation length decreases with increasing La content, being sensitive also to the synthesis method. The behavior of the correlation length is linked to the macroscopic properties, showing a strong increase of disorder with La doping. The roughness exponent for the domain wall in PLZT 9/65/35 is close to 2/3 indicating 1D character of domain walls in relaxors.

010302 applied physicsSurface (mathematics)Materials scienceCondensed matter physicsDoping02 engineering and technology021001 nanoscience & nanotechnologyCondensed Matter Physics01 natural sciencesGrain sizeElectronic Optical and Magnetic MaterialsDomain wall (magnetism)Piezoresponse force microscopyvisual_art0103 physical sciencesDomain (ring theory)Roughness exponentvisual_art.visual_art_mediumCeramic0210 nano-technologyFerroelectrics
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ZnMgO-based UV photodiodes: a comparison of films grown by spray pyrolysis and MBE

2016

Detecting the UV part of the spectrum is fundamental for a wide range of applications where ZnMgO has the potential to play a central role. The shortest achievable wavelength is a function of the Mg content in the films, which in turn is dependent on the growth technique. Moreover, increasing Mg contents lead to an electrical compensation of the films, which directly affects the responsivity of the photodetectors. In addition, the metal-semiconductor interface and the presence of grain boundaries have a direct impact on the responsivity through different gain mechanisms. In this work, we review the development of ZnMgO UV Schottky photodiodes using molecular beam epitaxy and spray pyrolysis…

010302 applied physicsTelecomunicacionesMaterials sciencebusiness.industrySchottky diodePhotodetector02 engineering and technology021001 nanoscience & nanotechnology01 natural sciencesPhotodiodelaw.inventionResponsivityWavelengthSemiconductorlaw0103 physical sciencesOptoelectronicsGrain boundary0210 nano-technologybusinessMolecular beam epitaxy
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Production of dense nanostructured materials using FAPAS and SPS techniques

2011

International audience

010302 applied physics[CHIM.MATE] Chemical Sciences/Material chemistryMaterials scienceNanostructured materialsMetallurgySpark plasma sintering[CHIM.MATE]Chemical Sciences/Material chemistry02 engineering and technology021001 nanoscience & nanotechnology01 natural sciencesGrain size[ CHIM.MATE ] Chemical Sciences/Material chemistry0103 physical sciences0210 nano-technologyComputingMilieux_MISCELLANEOUS
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Is there a global carbonate layer in the oceanic mantle?

2021

co-auteur étranger; International audience; Previous modeling of carbonate subduction by high‐pressure experimentation has allowed to propose scenarios for bulk carbon return to the mantle, but the detailed transfer mechanisms have seldom been studied. We monitored carbonate – silicate reactions by combining high‐pressure experiments and synchrotron‐based x‐ray diffraction. Carbonates break down at moderate pressure and high temperature and CO2 is trapped at grain boundaries. Further isothermal compression yields melting, which may control continuous carbon introduction, first in the mantle wedge, and next, away from the wedge. Carbon presence has been discussed in a variety of magmatic con…

010504 meteorology & atmospheric sciencesMantle wedgeSubductionchemistry.chemical_element010502 geochemistry & geophysics01 natural sciencesIsothermal processMantle (geology)Plate tectonicschemistry.chemical_compoundGeophysicschemistry13. Climate actionLithosphere[SDU]Sciences of the Universe [physics]General Earth and Planetary SciencesCarbonateGrain boundaryCompression (geology)PetrologyCarbonGeology0105 earth and related environmental sciences
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Strain rate dependence for evolution of steady state grain sizes: Insights from high-strain experiments on ice

2019

Abstract Understanding of the microstructural evolution and equilibrium grain size development during steady state tertiary flow is essential in order to improve our knowledge of ice and rock deformation. This contribution presents results from in situ transmitted light deformation experiments of natural glacier ice, with the development of the microstructure in a tertiary flow regime. We conducted one relative slower ( 1 × 10 − 6 1/s) and two relative faster-strain rate ( 2 × 10 − 6 1/s) pure shear experiments at −10 °C, up to a shortening of ∼57%. Microstructure development was followed by time-lapse observations, and two new microstructure-based indicators, the ‘seeding rate’ and the ‘mi…

010504 meteorology & atmospheric sciencesMechanicsSlip (materials science)Pure shearStrain rate010502 geochemistry & geophysicsMicrostructure01 natural sciencesGrain sizeGeophysicsSpace and Planetary ScienceGeochemistry and PetrologyParticle-size distributionEarth and Planetary Sciences (miscellaneous)SeedingGeology0105 earth and related environmental sciencesStress concentrationEarth and Planetary Science Letters
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Acoustic properties of ancient shallow-marine carbonates: effects of depositional environments and diagenetic processes (Middle Jurassic, Paris Basin…

2010

17 pages; International audience; Examination of petrophysical properties (acoustic velocity, porosity, permeability, and density) and petrographical characteristics (texture, facies composition, and diagenesis) of more than 250 core plugs from the Middle Jurassic carbonates of the eastern Paris Basin provides insights into the parameters controlling acoustic velocities in relatively low-porosity carbonate rocks ({Phi} < 20%). The pore-type observations reveal distinct acoustic velocities in samples with intergranular macropores and samples with micropores in subhedral micrite, such that velocities in microporous mudstone–wackestone (lagoonal) deposits are greater than in macroporous grains…

010504 meteorology & atmospheric sciencesPetrophysicsCompaction[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/PetrographyMineralogyGeology010502 geochemistry & geophysicsCementation (geology)[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesDiagenesisGrainstone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesMarlCarbonate rockGeology0105 earth and related environmental sciences[ SDU.STU.PE ] Sciences of the Universe [physics]/Earth Sciences/Petrography
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Effect of strain rate cycling on microstructures and crystallographic preferred orientation during high-temperature creep

2016

Strain rate histories and strain magnitude are two crucial factors governing the evolution of dynamic recrystallized grain size and crystallographic preferred orientation (CPO) in rocks and ice masses. To understand the effect of cyclic variations in strain rate or non-steady-state deformation, we conducted two-dimensional, coaxial plane strain experiments with time-lapse observations from a fabric analyzer. There is a continuous reequilibration of microstructure and CPO development associated with constant and oscillating strain rate cycles. These can be correlated with c -axis small circle distributions, diagnostic of dynamic recrystallization involving new grain nucleation and grain boun…

010504 meteorology & atmospheric sciencesStrain (chemistry)NucleationGeologyStrain rate010502 geochemistry & geophysics01 natural sciencesGrain sizeCrystallographyCreepDynamic recrystallizationDeformation (engineering)Geology0105 earth and related environmental sciencesPlane stressGeology
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Intermediate-depth earthquake generation and shear zone formation caused by grain size reduction and shear heating

2015

cited By 23; The underlying physics of intermediate-depth earthquakes have been an enigmatic topic; several studies support either thermal runaway or dehydration reactions as viable mechanisms for their generation. Here we present fully coupled thermomechanical models that investigate the impact of grain size evolution and energy feedbacks on shear zone and pseudotachylite formation. Our results indicate that grain size reduction weakens the rock prior to thermal runaway and significantly decreases the critical stress needed for thermal runaway, making it more likely to result in intermediate-depth earthquakes at shallower depths. Furthermore, grain size is reduced in and around the shear z…

010504 meteorology & atmospheric sciencesThermal runawaySubduction[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Geology[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Geodynamics010502 geochemistry & geophysics01 natural sciencesGrain sizeMatrix (geology)13. Climate actionShear zonePetrologyGeologyStrengthening mechanisms of materialsSeismology0105 earth and related environmental sciencesMylonite
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Modelling of stylolite geometries and stress scaling

2012

International audience; In this contribution we present numerical simulations of stylolite growth to decipher the effects of initial rock heterogeneity and stress on their morphology. We show that stylolite growth in a rock with a uniform grain size produces different patterns than stylolite growth in a rock with a bimodal grain size distribution. Strong pinning of large heterogeneities produce stylolite structures that are dominated by pronounced teeth, whereas a uniform grain size leads to spikes and a roughness that shows variable wavelengths. We compare the simulated stylolites with natural examples and show that the model can reproduce the real structures. In addition we show that stro…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]stress-gauge[SDE.MCG]Environmental Sciences/Global ChangesCompaction[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]Surface finishpressure solution010502 geochemistry & geophysics01 natural sciencesPhysics::Geophysics[PHYS.MECA.MEMA]Physics [physics]/Mechanics [physics]/Mechanics of materials [physics.class-ph]Stress (mechanics)Geochemistry and Petrology[SPI.MECA.MEMA]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Mechanics of materials [physics.class-ph]Earth and Planetary Sciences (miscellaneous)compactionGeotechnical engineeringScaling0105 earth and related environmental sciencesstyloliteMechanicsself-affinityGrain sizeGeophysicsSpace and Planetary ScienceStyloliteParticle-size distributionPressure solutionnumerical modelGeology[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/MineralogyEarth and Planetary Science Letters
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Natural gas hydrate investigations by synchrotron radiation X-ray cryo-tomographic microscopy (SRXCTM)

2008

[1] We report the 3D microstructure analyses of natural gas hydrates sampled from Gulf of Mexico. The samples were characterized by synchrotron radiation X-ray cryo-tomographic microscopy (SRXCTM) using the ‘TOMCAT’ beam line at the Swiss Light Source (SLS). The SRXCTM demonstrates its applicability to unlock some microscopic features of the marine hydrates, in particular of crystallite size and grain boundary network. The gas hydrate domains are surrounded by a network of pores of typically a few micrometers, which are largely due to decomposition. Out of the SRXCTM data, the porosity, total volume of the voids, the void surface area and number of the total gas-filled voids have been calcu…

010504 meteorology & atmospheric sciencesbusiness.industryClathrate hydrateSynchrotron radiationMineralogy010502 geochemistry & geophysics01 natural sciencesGeophysicsNatural gasGeneral Earth and Planetary SciencesGrain boundaryCrystallitePorositybusinessHydrateGeologySwiss Light Source0105 earth and related environmental sciencesGeophysical Research Letters
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