Search results for "CREEP"

showing 10 items of 167 documents

On the hydro-mechanical behaviour of remoulded and natural Opalinus Clay shale

2016

The geo-energy sector makes use of advanced technologies such as shale gas extraction, CO2 sequestration and nuclear waste geological disposal that rely on the exploitation of shale formations. Due to the great depths involved in these applications and the difficulties in retrieving intact samples, remoulded shale specimens are often adopted for hydro-mechanical testing. Remoulded and intact shales may substantially differ in their hydro-mechanical behaviour due to the particular structure of the natural material, which is the result of diagenesis and burial history. This paper presents an experimental campaign aimed at (i) characterizing the role of diagenesis and depth for Opalinus Clay s…

Shale gasEffective stress0211 other engineering and technologiesCompaction02 engineering and technology010502 geochemistry & geophysics01 natural sciencesGeotechnical engineeringdiagenesis.PorosityOpalinus Clay021101 geological & geomatics engineering0105 earth and related environmental sciencesDiagenesiSettore ICAR/07 - GeotecnicaGeologyGeotechnical Engineering and Engineering GeologyDiagenesisPermeability (earth sciences)intrinsic propertiesCreepHydro-mechanical behaviourremoulded shalesOil shaleGeologyIntrinsic propertieRemoulded shale
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Shear elasticity of mixed cyanide orientational glass

1993

Four mixed crystals of KBr:KCN and NaCN:KCN, complemented by KCN, have been investigated by torque-shear measurements. The real and imaginary parts of the shear compliance ${\mathit{s}}_{44}$ at a measuring frequency of 2 Hz have been determined. Zero-field-cooling--field-cooling--remanent-shear-strain cycles have been performed. For (KBr${)}_{0.47}$(KCN${)}_{0.53}$ the creep after zero-field cooling and the elastic aftereffect after field cooling have been followed within a time window from 0.1 to ${10}^{4}$ s. Results on the nonlinear part of the shear compliance have been obtained. It is shown that the field-cooled strain represents the static limit of the elastic response. The results a…

Shear elasticitychemistry.chemical_classificationchemistry.chemical_compoundSpin glassMaterials scienceCreepchemistryShear (geology)CyanideThermodynamicsElasticity (economics)Orientational glassInorganic compoundPhysical Review B
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Stress induced grain boundary migration in very soluble brittle salt

1999

Abstract Grain boundary migration (GBM) was studied in-situ at room temperature, atmospheric pressure and an applied diffmfwerential stress of ∼9.5 MPa under the optical microscope, in a wet aggregate of an elastic-brittle salt (sodium chlorate). The aggregate was previously deformed predominantly by a combination of grain boundary sliding, pressure solution and cataclastic solution creep. After deformation, but when the sample was still under differential stress, undeformed, fracture-free grains were observed to grow at the cost of deformed, intensely fractured grains. GMB rates typically fell in the range 2--10 μm/day. GBM took place only as long as the sample was under stress. Boundaries…

Stress (mechanics)BrittlenessCreepMineralogyGeologyPressure solutionCataclastic rockDeformation (engineering)Composite materialDifferential stressGeologyGrain Boundary SlidingJournal of Structural Geology
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On the thermodynamics of listric faults

2004

We investigate a novel fully coupled thermal-mechanical numerical model of the crust in order to trace the physics of interaction of its brittle and ductile layers. In a unified approach these layers develop in a natural transition as a function of the state variables pressure, deviatoric stress, temperature and strain-rate. We find that the main storage of elastic energy lies in the domain where brittle and ductile strain-rates overlap so that shear zones are attracted to this zone of maximum energy dissipation. This dissipation appears as a local heat source (shear heating). The brittle-ductile transition zone evolves through extreme weakening by thermo-mechanical feedback. The physics of…

Stress (mechanics)BrittlenessCreepShear (geology)Space and Planetary ScienceTransition zoneElastic energyThermodynamicsGeologyDissipationShear zoneGeologyEarth, Planets and Space
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The structure of reactive grain-boundaries under stress containing confined fluids

2006

We present numerical experiments on structure development in grain-boundaries during dissolution–precipitation creep. Two solids that are represented by an elastic spring configuration are pressed together with a compressible fluid in the grain-boundary. The solid can dissolve or precipitate depending on elastic and surface energy as well as fluid pressure and concentration of dissolved material in the fluid. We perform a number of numerical experiments with different starting configurations that represent a large-scale island-channel interface with solid–solid contacts across the islands, a rough grain-boundary interface with a fluid along the whole interface and a smooth thin-film interfa…

Stress (mechanics)CreepGeochemistry and PetrologyGeologyGrain boundaryMechanicsPressure solutionDisplacement (fluid)DissolutionGeologySurface energyNeckingChemical Geology
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Effect of microcracking on pressure-solution strain rate: The Gratz grain-boundary model

1998

Different, but reasonable and well-accepted assumptions made about grain-boundary structure during pressure-solution (PS) creep may easily have an effect of more than 10 orders of magnitude on the calculated PS deformation rate. Understanding of grain-boundary structure during PS creep is therefore extremely important. Experimental evidence is presented in support of a grain-boundary model previously proposed by A. J. Gratz on the basis of observations on naturally deformed rocks. In this model, boundaries are assumed to have a static island-channel network structure. Channels are located where microcracks intersect the boundary. The rate of material transport is governed by thin-film diffu…

Stress (mechanics)CrystallographyOrders of magnitude (specific energy)CreepGeologyGrain boundaryMechanicsPressure solutionDiffusion (business)Strain rateDeformation (engineering)GeologyGeology
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Formation of dislocation patterns: Computer simulations

1996

Dislocations patterns have been extensively studied by means of TEM. In parallel, theoretical approaches have been developed by using two methods; reaction diffusion schemes and computer simulation models. This distinction is not rigid since some computer models include the former approach in their evolution equations. Independently from the difficulties each approach presents in formulating the collective behavior of dislocations, the aim of these studies is to exhibit simple dislocation patterns as persistent slip bands and/or cellular organization. In this context, computer simulations brought a methodology which undoubtedly is a complement to the existing approaches for dislocations. Ne…

Stress (mechanics)Dislocation creepPhysicsCollective behaviorMesoscopic physicsClassical mechanicsLüders bandReaction–diffusion systemContext (language use)Statistical physicsDislocationPhysical Review B
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<title>Indentation creep and stress relaxation in amorphous As-S-Se and As-S films</title>

2001

The indentation creep in as-deposited and photopolymerized As- S-Se and As-S films has been investigated. The results show pronounced relaxation of mechanical stresses in the films at room temperature. The relationship (sigma) equals B (epsilon) m between the deformation rate and the stress is observed and the values of the deformation rate sensitivity exponent m < 1 are found. The creep rate was found to be dependent on deposition conditions of layers, applied indentation load, structural state of the material and light irradiation during the creep test.© (2001) COPYRIGHT SPIE--The International Society for Optical Engineering. Downloading of the abstract is permitted for personal use only.

Stress (mechanics)Materials scienceCreepIndentationStress relaxationForensic engineeringRelaxation (physics)Diffusion creepComposite materialDeformation (engineering)Amorphous solidOptical Organic and Inorganic Materials
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Application of time–stress superposition to nonlinear creep of polyamide 66 filled with nanoparticles of various sizes

2007

The long-term tensile creep of polyamide 66 and its nanocomposites filled with 1 vol.% TiO2 nanoparticles 21 and 300 nm in diameter is studied. It is assumed that the dominant mechanisms of creep deformation are of viscoelastic nature, while the contribution of plastic strains is not essential in the stress (< 0.6 of the ultimate stress) and time (about 100 hours) ranges considered. The creep isochrones obtained show that the materials exhibit a nonlinear viscoelastic behaviour and the degree of nonlinearity is reduced significantly by incorporation of the nanoparticles. The evolution of viscoelastic strains is less pronounced for the nanocomposite filled with smaller nanoparticles. Smooth …

Stress (mechanics)Nonlinear systemNanocompositeMaterials scienceCreepUltimate tensile strengthGeneral EngineeringCeramics and CompositesStress relaxationRelaxation (physics)Composite materialViscoelasticityComposites Science and Technology
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Crystallographic preferred orientation development by dissolution–precipitation creep

2000

Abstract Crystallographic preferred orientations (CPOs) in deformed rocks are commonly interpreted as resulting from crystal plastic deformation mechanisms, where deformation is achieved by the movement of dislocations. In this paper we investigate the possibility of CPO-development by dissolution–precipitation creep or pressure solution. A numerical model is presented, which simulates the development of a grain aggregate that deforms by reaction-controlled dissolution–precipitation creep. Grains are simulated as rectangular boxes that change their shape by growth, or dissolution of their surfaces, depending on the normal stresses acting on the individual surfaces. Grains can also rotate du…

Stress (mechanics)Simple shearCrystalCrystallographyCreepGeologyPressure solutionPure shearDeformation (engineering)GeologyPhysics::GeophysicsPlane stressJournal of Structural Geology
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