Search results for "Physics::Fluid Dynamics"

showing 10 items of 662 documents

Development of branching brittle and ductile shear zones: A numerical study

2017

Continental collision zones are usually associated with large-scale strike-slip shear zones. In most cases these shear zones are complex and consist of multiple strands, varying in width, length, and total displacement. Here we present 2-D numerical models to simulate the formation of such shear zones at different depth levels within the crust, under either brittle (frictional/plastic) or ductile conditions. Localization of shear zones is initiated by a material contrast (heterogeneity) of the material parameters. We systematically test the rate of strain-weakening in brittle and in ductile regimes to understand its influence on the development of shear zone networks. Our simulations sugges…

010504 meteorology & atmospheric sciencesGeometry010502 geochemistry & geophysics01 natural sciencesCondensed Matter::Soft Condensed MatterPhysics::Fluid DynamicsShear rateSimple shearStress fieldGeophysicsBrittlenessShear (geology)Geochemistry and PetrologyCritical resolved shear stressShear stressGeotechnical engineeringShear zoneGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
researchProduct

2D Hydro-Mechanical-Chemical Modeling of (De)hydration Reactions in Deforming Heterogeneous Rock: The Periclase-Brucite Model Reaction

2020

Deformation at tectonic plate boundaries involves coupling between rock deformation, fluid flow, and metamorphic reactions, but quantifying this coupling is still elusive. We present a new two-dimensional hydro-mechanical-chemical numerical model and investigate the coupling between heterogeneous rock deformation and metamorphic (de)hydration reactions. We consider linear viscous compressible and power-law viscous shear deformation. Fluid flow follows Darcy's law with a Kozeny-Carman type permeability. We consider a closed isothermal system and the reversible (de)hydration reaction: periclase and water yields brucite. Fluid pressure within a circular or elliptical inclusion is initially bel…

010504 meteorology & atmospheric sciencesShear zoneChemical process modelingMetamorphic rockThermodynamicsNumerical simulationengineering.materialDeformation (meteorology)010502 geochemistry & geophysics01 natural sciencesPhysics::GeophysicsPhysics::Fluid DynamicsGeochemistry and PetrologyFluid dynamicsCoupling (piping)Brucite-Periclase reaction0105 earth and related environmental sciencesBruciteReaction-induced weakeningGeophysics13. Climate actionengineeringHydro-Mechanical-Chemical modelPericlaseShear zoneGeologyRock deformation coupled to reactions
researchProduct

2019

Abstract. The flow of fluids through porous media such as groundwater flow or magma migration is a key process in geological sciences. Flow is controlled by the permeability of the rock; thus, an accurate determination and prediction of its value is of crucial importance. For this reason, permeability has been measured across different scales. As laboratory measurements exhibit a range of limitations, the numerical prediction of permeability at conditions where laboratory experiments struggle has become an important method to complement laboratory approaches. At high resolutions, this prediction becomes computationally very expensive, which makes it crucial to develop methods that maximize …

010504 meteorology & atmospheric sciencesStratigraphyFinite differencePaleontologySoil ScienceReynolds numberGeologyMechanics010502 geochemistry & geophysics01 natural sciencesStencilNon-Newtonian fluidPhysics::GeophysicsPhysics::Fluid DynamicsPermeability (earth sciences)symbols.namesakeGeophysicsGeochemistry and PetrologyFluid dynamicsNewtonian fluidsymbolsPorous mediumGeology0105 earth and related environmental sciencesEarth-Surface ProcessesSolid Earth
researchProduct

Transition to turbulence in serpentine pipes

2017

Abstract The geometry considered in the present work (serpentine pipe) is a sequence of U-bends of alternate curvature. It is characterized by pipe diameter, d = 2a and bend diameter, D = 2c. The repeated curvature inversion forces the secondary flow pattern, typical of all flows in curved ducts, to switch between two mirror-like configurations. This causes (i) pressure drop and heat or mass transfer characteristics much different from those occurring either in a straight pipe or in a constant-curvature pipe, and (ii) an early loss of stability of the base steady-state flow. In the present work, four values of the curvature δ = a/c (0.2, 0.3, 0.4 and 0.5) were considered. For each value of …

020209 energyPrandtl number02 engineering and technologySerpentine pipeCondensed Matter PhysicCurvature01 natural sciences010305 fluids & plasmasPhysics::Fluid Dynamicssymbols.namesakeEngineering (all)Computational fluid dynamic0103 physical sciences0202 electrical engineering electronic engineering information engineeringSecondary flowSettore ING-IND/19 - Impianti NucleariPhysicsPressure dropTurbulenceGeneral EngineeringReynolds numberMechanicsCondensed Matter PhysicsSecondary flowTransition to turbulenceClassical mechanicsHeat fluxFlow conditioningsymbolsBifurcation
researchProduct

Energy-based fluid–structure model of the vocal folds

2020

AbstractLumped elements models of vocal folds are relevant research tools that can enhance the understanding of the pathophysiology of many voice disorders. In this paper, we use the port-Hamiltonian framework to obtain an energy-based model for the fluid–structure interactions between the vocal folds and the airflow in the glottis. The vocal fold behavior is represented by a three-mass model and the airflow is described as a fluid with irrotational flow. The proposed approach allows to go beyond the usual quasi-steady one-dimensional flow assumption in lumped mass models. The simulation results show that the proposed energy-based model successfully reproduces the oscillations of the vocal …

0209 industrial biotechnologyControl and OptimizationGlottisComputer scienceApplied MathematicsAirflow02 engineering and technologyMechanicsFold (geology)ArticlesConservative vector field01 natural sciencesCompressible flowPhysics::Fluid Dynamics020901 industrial engineering & automationmedicine.anatomical_structureFlow (mathematics)Control and Systems EngineeringComputer Science::SoundVocal folds0103 physical sciencesmedicine010301 acousticsEnergy (signal processing)
researchProduct

A note on higher order Melnikov functions

2005

We present several classes of planar polynomial Hamilton systems and their polynomial perturbations leading to vanishing of the first Melnikov integral. We discuss the form of higher order Melnikov integrals. In particular, we present new examples where the second order Melnikov integral is not an Abelian integral.

Abelian integralPolynomialPure mathematicsMathematics::Dynamical SystemsApplied MathematicsMathematical analysisMathematics::Classical Analysis and ODEsPhysics::Fluid DynamicsNonlinear Sciences::Chaotic DynamicsPlanarDiscrete Mathematics and CombinatoricsOrder (group theory)Nonlinear Sciences::Pattern Formation and SolitonsMathematicsQualitative Theory of Dynamical Systems
researchProduct

Numerical approach to problems of gravitational instability of geostructures with advected material boundaries

1998

SUMMARY We present a numerical approach for solving 2-D mantle flow problems where the chemical composition changes abruptly across intermediate boundaries. The method combines a Galerkin-spline technique with a method of integration over regions bounded by advected interfaces to represent discontinuous variations of material parameters. It allows direct approximation of a natural free surface position, instead of a posteriori calculation of topography from the normal stress at the upper free-slip boundary. We formulate a model where a viscous incompressible fluid filling a square box is divided into layers (not necessarily horizontal) by advected boundaries, across which the density and vi…

AdvectionBoundary (topology)Eulerian pathGeophysicsMechanicsClassification of discontinuitiesDiapirPhysics::GeophysicsPhysics::Fluid Dynamicssymbols.namesakeGeophysicsGeochemistry and PetrologyPosition (vector)AsthenosphereFree surfacesymbolsGeologyGeophysical Journal International
researchProduct

Adaptive BEM for Low Noise Propeller Design

2009

A potential-based Boundary Element Method is presented for the aerodynamic and acoustic design of propel- lers at on- and off-design point conditions. Using an adaptive method, a family of airfoil sections is selected to produce the required performance (thrust, torque and efficiency versus advance ratio) at different cruise flight levels. Climb condi- tions are also considered in order to check the off-design point performance. Once the available airfoil data have been stored in a database, the code processes the families of airfoils to generate a complete geometry for a propeller of the specified performance with an optimized noise emission. The computational scheme adjusts the blade geom…

AirfoilChord (geometry)Ffowcs Williams-Hawkings equationComputer scienceAcousticspropeller designPropellerBlade geometryAerodynamicsboundary element methodPhysics::Fluid DynamicsNoiseAeroacoustic optimizationClimbAdvance ratio
researchProduct

On strong solutions of the differential equations modeling the steady flow of certain incompressible generalized Newtonian fluids

2007

In this paper we discuss a system of partial differential equations describing the steady flow of an incompressible fluid and prove the existence of a strong solution under suitable assumptions on the data. In the 2D-case this solution turns out to be of class C^{1,\alpha}.

Algebra and Number TheoryPartial differential equationDifferential equationApplied MathematicsMathematical analysis510Physics::Fluid DynamicsStrong solutionsGeneralized Newtonian fluidFlow (mathematics)CompressibilityNewtonian fluidAnalysisMathematicsSt. Petersburg Mathematical Journal
researchProduct

Micro magnetofluidics: droplet manipulation of double emulsions based on paramagnetic ionic liquids

2013

The ability to control and manipulate discrete fluid droplets by magnetic fields offers new opportunities in microfluidics. A surfactant-free and easy to realize technique for the continuous generation of double emulsion droplets, composed of an organic solvent and a paramagnetic ionic liquid, is applied. The inner phase of the emulsion droplet consists of imidazolium-based ionic liquids with either iron, manganese, nickel or dysprosium containing anions which provide paramagnetic behaviour. The double emulsion droplets are dispersed in a continuous phase of FC-40. All substances - the organic phase, the paramagnetic ionic liquid and the continuous phase -are immiscible. The magnetic proper…

AnionsIronMicrofluidicsMicrofluidicsBiomedical EngineeringMixing (process engineering)Analytical chemistryIonic LiquidsBioengineeringBiochemistryPhysics::Fluid DynamicsMagneticsParamagnetismchemistry.chemical_compoundNickelPhase (matter)DysprosiumPhysics::Atomic and Molecular ClustersCoalescence (physics)ManganeseChemistryImidazolesGeneral ChemistryMagnetic fieldCondensed Matter::Soft Condensed MatterChemical engineeringMagnetIonic liquidEmulsionshuman activitiesLab on a Chip
researchProduct