Search results for "OPEN BOUNDARY"

showing 2 items of 2 documents

Time-based Chern number in periodically driven systems in the adiabatic limit

2023

To define the topology of driven systems, recent works have proposed synthetic dimensions as a way to uncover the underlying parameter space of topological invariants. Using time as a synthetic dimension, together with a momentum dimension, gives access to a synthetic two-dimensional (2D) Chern number. It is, however, still unclear how the synthetic 2D Chern number is related to the Chern number that is defined from a parametric variable that evolves with time. Here we show that in periodically driven systems in the adiabatic limit, the synthetic 2D Chern number is a multiple of the Chern number defined from the parametric variable. The synthetic 2D Chern number can thus be engineered via h…

General Physics and AstronomyTDDFT Open boundary conditionsSettore FIS/03 - Fisica Della MateriaPhysical Review Research
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Stability of Flow with Viscous Dissipation in a Horizontal Porous Layer with an Open Boundary Having a Prescribed Temperature Gradient

2010

Published version of an article in the journal: Transport in Porous Media. The original publication is available at www.springerlink.com, http://dx.doi.org/10.1007/s11242-010-9588-6 A buoyancy-induced stationary flow with viscous dissipation in a horizontal porous layer is investigated. The lower boundary surface is impermeable and subject to a uniform heat flux. The upper open boundary has a prescribed, linearly varying, temperature distribution. The buoyancy-induced basic velocity profile is parallel and non-uniform. The linear stability of this basic solution is analysed numerically by solving the disturbance equations for oblique rolls arbitrarily oriented with respect to the basic velo…

VDP::Mathematics and natural science: 400::Mathematics: 410::Applied mathematics: 413PhysicsBuoyancyOPEN BOUNDARYGeneral Chemical EngineeringBoundary (topology)MechanicsRayleigh numberPOROUS LAYERengineering.materialCritical valueVISCOUS DISSIPATIONInstabilityCatalysisTHERMAL INSTABILITYPhysics::Fluid DynamicsTemperature gradientClassical mechanicsHeat fluxPRESCRIBED TEMPERATURE GRADIENTengineeringVDP::Technology: 500::Materials science and engineering: 520Linear stabilityTransport in Porous Media
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