Search results for "Strain theory"

showing 10 items of 22 documents

Reversed polarized emission in highly strained a-plane GaN/AlN multiple quantum wells

2010

The polarization of the emission from a set of highly strained $a$-plane GaN/AlN multiple quantum wells of varying well widths has been studied. A single photoluminescence peak is observed that shifts to higher energies as the quantum well thickness decreases due to quantum confinement. The emitted light is linearly polarized. For the thinnest samples the preferential polarization direction is perpendicular to the wurtzite $c$ axis with a degree of polarization that decreases with increasing well width. However, for the thickest well the preferred polarization direction is parallel to the $c$ axis. Raman scattering, x-ray diffraction, and transmission electron microscopy studies have been p…

010302 applied physicsPhysicsElectron densityCondensed matter physicsLinear polarizationOscillator strengthQuantum point contact: Physics [G04] [Physical chemical mathematical & earth Sciences]Infinitesimal strain theory02 engineering and technology021001 nanoscience & nanotechnologyCondensed Matter Physics01 natural sciencesElectronic Optical and Magnetic MaterialsCondensed Matter::Materials Science: Physique [G04] [Physique chimie mathématiques & sciences de la terre]Quantum dotQuantum mechanics0103 physical sciences[PHYS.COND.CM-MS]Physics [physics]/Condensed Matter [cond-mat]/Materials Science [cond-mat.mtrl-sci]Degree of polarization0210 nano-technologyQuantum wellComputingMilieux_MISCELLANEOUS
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The influence of rock heterogeneity on the scaling properties of simulated and natural stylolites

2009

International audience; Stylolites are among the most prominent deformation patterns in sedimentary rocks that document localized pressure solution. Recent studies revealed that stylolite roughness is characterized by two distinct scaling regimes. The main goal of the present study is to decipher whether this complex scaling behavior of stylolites is caused by the composition of the host-rock, i.e. heterogeneities in the material, or is governed by inherent processes on respective scales, namely the transition from a surface energy to an elastic energy dominated regime, as theoretically predicted. For this purpose we have developed a discrete numerical technique, based on a lattice spring m…

010504 meteorology & atmospheric sciences[SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]CompactionCompaction[SDU.STU.PE]Sciences of the Universe [physics]/Earth Sciences/Petrography[SDU.STU]Sciences of the Universe [physics]/Earth SciencesSurface finish010502 geochemistry & geophysics01 natural sciencesScalingPhysics::Geophysics[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryGeotechnical engineering[PHYS.COND.CM-SM]Physics [physics]/Condensed Matter [cond-mat]/Statistical Mechanics [cond-mat.stat-mech]ScalingComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesQuenched noiseElastic energyGeologyMechanicsRoughnessSurface energyPressure solution13. Climate action[SDU]Sciences of the Universe [physics]StyloliteFinite strain theoryStylolitePressure solutionGeology
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Experimental modeling of viscous inclusions in a circular high-strain shear rig: Implications for the interpretation of shape fabrics and deformed en…

2002

[1] Deformation experiments with initially spherical and prolate viscous inclusions suspended in a viscous Newtonian matrix in a circular high strain annular shear rig provide insights on the shape development of inclusions in high strain shear zones during progressive deformation. Inclusions with a specific viscosity ratio with respect to the matrix material show distinct types of three-dimensional shape development. For instance, at a high viscosity ratio between matrix and inclusion a pulsating ellipsoid develops, which both continuously rotates and changes its shape from a sphere to an ellipsoid and back to a sphere. The experiments show that the shape of an inclusion that has a viscosi…

Atmospheric ScienceEcologyPaleontologySoil ScienceMineralogyForestryMechanicsAquatic ScienceOceanographyEllipsoidPower lawPhysics::Fluid DynamicsViscosityGeophysicsShear (geology)RheologySpace and Planetary ScienceGeochemistry and PetrologyFinite strain theoryEarth and Planetary Sciences (miscellaneous)Newtonian fluidShear zoneGeologyEarth-Surface ProcessesWater Science and TechnologyJournal of Geophysical Research: Solid Earth
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Vertical ductile thinning and its contribution to the exhumation of high-pressure rocks: the Cycladic blueschist unit in the Aegean

2008

The contribution of vertical ductile thinning to the exhumation of high-pressure rocks is evaluated by estimating finite strain in 75 exhumed high-pressure rocks of the Cycladic blueschist unit in the Aegean Sea, Greece, and western Turkey. Strain data indicate heterogeneous deformation; principal stretches are 1.24–5.03 for S X , 0.63–2.53 for S Y and 0.10–0.81 for S Z , with a tensor average of S X : S Y : S Z =1.52:1.28:0.51. A 1D numerical model, which integrates velocity gradients along a vertical flow path with a steady-state orogen, is used to estimate the contribution of ductile thinning of the overburden of the high-pressure rocks to exhumation. Using a strain-rate law that is prop…

BlueschistOverburdenThinningFinite strain theoryHigh pressureFlow (psychology)Vertical flowGeologyDeformation (engineering)PetrologyGeologyJournal of the Geological Society
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A note on the higher order strain and stress tensors within deformation gradient elasticity theories: Physical interpretations and comparisons

2016

Abstract Higher order strain and stress tensors encompassed within gradient elasticity theories are discussed with a particular concern to the physical meaning of double and triple stresses. A single rule is shown to hold for the physical interpretation of the indices of a higher order stress tensor both within distortion gradient and strain gradient theories, whereas the analogous Mindlin’s rule holds only within distortion gradient theories. Double and triple stresses are discussed separately with the aid of simple illustrative examples. A corrigendum to a previous paper by the author (IJSS 50 (2013) 3749–3765) is also presented.

Cauchy stress tensorApplied MathematicsMechanical EngineeringMathematical analysisGeometry02 engineering and technologyElasticity (physics)021001 nanoscience & nanotechnologyCondensed Matter PhysicsStrain gradient020303 mechanical engineering & transports0203 mechanical engineeringMechanics of MaterialsModeling and SimulationFinite strain theoryGeneral Materials ScienceSingle rule0210 nano-technologyMathematicsInternational Journal of Solids and Structures
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The fabric attractor

1997

Abstract The nature of fabric accumulation in high strain zones such as ductile shear zones depends on the nature and orientation of flow eigenvectors or apophyses. Some flow apophyses can act as ‘attractors’ of material lines or principal finite strain axes. This paper explains the nature of such attractors and discusses their significance and orientation in different monoclinic flow types. In ductile shear zones, strain values are high enough to show the effect of attractors in deformed rocks clearly. The concept of attractors can be used in deformation modelling, and can help in understanding the accumulation of deformation fabrics in homogeneous and inhomogeneous flow, e.g. around boudi…

Condensed Matter::Materials ScienceFlow (mathematics)Strain (chemistry)Finite strain theoryOrientation (geometry)AttractorGeologyGeotechnical engineeringGeometryDeformation (engineering)Shear zoneEigenvalues and eigenvectorsGeologyJournal of Structural Geology
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The tensor of interaction of a two-level system with an arbitrary strain field

2007

The interaction between two-level systems (TLS) and strain fields in a solid is contained in the diagonal matrix element of the interaction hamiltonian, $\delta$, which, in general, has the expression $\delta=2[\gamma]:[S]$, with the tensor $[\gamma]$ describing the TLS ``deformability'' and $[S]$ being the symmetric strain tensor. We construct $[\gamma]$ on very general grounds, by associating to the TLS two objects: a direction, $\hat\bt$, and a forth rank tensor of coupling constants, $[[R]]$. Based on the method of construction and on the invariance of the expression of $\delta$ with respect to the symmetry transformation of the solid, we conclude that $[[R]]$ has the same structure as …

Coupling constantPhysicsHistoryCondensed Matter - Materials SciencePhononIsotropyInfinitesimal strain theoryMaterials Science (cond-mat.mtrl-sci)FOS: Physical sciencesDisordered Systems and Neural Networks (cond-mat.dis-nn)Condensed Matter - Disordered Systems and Neural NetworksPolarization (waves)Computer Science ApplicationsEducationsymbols.namesakeQuantum mechanicsDiagonal matrixPerpendicularsymbolsHamiltonian (quantum mechanics)
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Flame foliation: Evidence for a schistosity formed normal to the extension direction

2007

Abstract Foliations are normally thought to develop approximately parallel to the XY-plane of the finite strain ellipsoid, i.e., perpendicular to the main shortening direction. We present a new type of schistosity named “flame foliation” that forms orthogonal to the main extension direction, approximately parallel to the YZ-plane of finite strain. Flame foliation consists of anastomosing biotite-rich selvedges overprinting S1 in pelitic layers of metaturbitites in NW Namibia. The biotite crystals in the selvedges are peculiar because they are oriented oblique or orthogonal to the flame foliation itself and parallel to the previous S1 cleavage, a feature no other foliation shows. In some cas…

CrenulationDeformation (mechanics)Finite strain theoryPlutonFoliation (geology)engineeringCleavage (geology)GeologyGeometryengineering.materialOverprintingBiotiteGeologyJournal of Structural Geology
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Statistical Properties of Generalized Strain Criterion for Multiaxial Random Fatigue

1989

ABSTRACT Statistical properties of generalized criterion of the maximum shear and normal strains on the fracture plane have been presented, Functions of probability distribution and spectral density of the equivalent strain have been analysed on the assumption that a random tensor of strain state is a six-dimensional stationary and ergodic Gaussian process. The expected value and variance of the equivalent strain have been determined as well. From spectral analysis a new limitation has been derived for extension of some multiaxial cyclic fatigue criteria to random loadings. It is connected with the fact that in some cases the frequency band of the equivalent strain is greater than that for …

Cyclic stressFrequency bandMathematical analysisSpectral densityInfinitesimal strain theoryExpected valueCombinatoricsCondensed Matter::Materials Sciencesymbols.namesakesymbolsErgodic theoryProbability distributionGaussian processMathematics
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Low-pressure ferroelastic phase transition in rutile-type AX2 minerals: cassiterite (SnO2), pyrolusite (MnO2) and sellaite (MgF2)

2019

The structural behaviour of cassiterite (SnO2), pyrolusite (MnO2) and sellaite (MgF2), i.e. AX2-minerals, has been investigated at room temperature by in situ high-pressure single-crystal diffraction, up to 14 GPa, using a diamond anvil cell. Such minerals undergo a ferroelastic phase transition, from rutile-like structure (SG: P42/mnm) to CaCl2-like structure (SG: Pnnm), at ≈ 10.25, 4.05 and 4.80 GPa, respectively. The structural evolution under pressure has been described by the trends of some structure parameters that are other than zero in the region of the low-symmetry phase’s stability. In particular, three tilting-angles (ω, ω′, ABS) and the metric distortion of the cation-centred oc…

DiffractionPhase transition010504 meteorology & atmospheric sciencesIonic bondingThermodynamicsengineering.material010502 geochemistry & geophysics01 natural scienceshigh-pressure diffraction ferroelastic phase transition cassiterite pyrolusite sellaiteGeochemistry and PetrologyCassiteriteGeneral Materials ScienceFerroelastic phase transition0105 earth and related environmental sciencesCassiterite; Ferroelastic phase transition; High-pressure diffraction; Pyrolusite; SellaitePyrolusiteSettore GEO/06 - MineralogiaChemistryCassiteriteSellaiteInfinitesimal strain theoryPyrolusiteOctahedronRutileengineeringHigh-pressure diffraction
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