Thermocapillary effects during the melting of phase-change materials in microgravity: steady and oscillatory flow regimes

Salgado Sanchez, Pablo ORCID: https://orcid.org/0000-0001-9528-4285, Ezquerro Navarro, José Miguel ORCID: https://orcid.org/0000-0002-8863-298X, Fernández Fraile, José Javier ORCID: https://orcid.org/0000-0003-0865-9320 and Rodríguez Otero, Jacobo ORCID: https://orcid.org/0000-0002-3561-7276 (2020). Thermocapillary effects during the melting of phase-change materials in microgravity: steady and oscillatory flow regimes. "Journal of Fluid Mechanics", v. 908 (n. A20); ISSN 00221120. https://doi.org/10.1017/jfm.2020.852.

Descripción

Título: Thermocapillary effects during the melting of phase-change materials in microgravity: steady and oscillatory flow regimes
Autor/es:
Tipo de Documento: Artículo
Título de Revista/Publicación: Journal of Fluid Mechanics
Fecha: 7 Diciembre 2020
ISSN: 00221120
Volumen: 908
Número: A20
Materias:
Palabras Clave Informales: Design; Energy-Storage; Heat-Transfer Enhancement; Marangoni Convection; Marangoni Number Convection; Melting; Metal; Nepcm; Pattern Formation; Pcm; Rectangular Cavity; Solidification; Solidification/Melting
Escuela: E.T.S. de Ingeniería Aeronáutica y del Espacio (UPM)
Departamento: Aeronaves y Vehículos Espaciales
Licencias Creative Commons: Reconocimiento - Sin obra derivada - No comercial

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Resumen

A detailed numerical investigation of thermocapillary effects during the melting of phase-change materials in microgravity is presented. The phase-change transition is analysed for the high-Prandtl-number material n-octadecane, which is enclosed in a two-dimensional rectangular container subjected to isothermal conditions along the lateral walls. The progression of the solid/liquid front during the melting leaves a free surface, where the thermocapillary effect acts driving convection in the liquid phase. The nature of the flow found during the melting depends on the container aspect ratio, Gamma, and on the Marangoni number, Ma. For large Gamma, this flow initially adopts a steady return flow structure characterised by a single large vortex, which splits into a series of smaller vortices to create a steady multicellular structure (SMC) with increasing Ma. At larger values of Ma, this SMC undergoes a transition to oscillatory flow through the appearance of a hydrothermal travelling wave (HTW), characterised by the creation of travelling vortices near the cold boundary. For small Gamma, the thermocapillary flow at small to moderate Ma is characterised by an SMC that develops initially within a thin layer near the free surface. At larger times, the SMC evolves into a large-scale steady vortical structure. With increasing applied Ma, a complex oscillatory mode is observed. This state, referred to as an oscillatory standing wave (OSW), is characterised by the pulsation of the vortical structure. Finally, for an intermediate Gamma both HTWand OSWmodes can be found depending on Ma.

Más información

ID de Registro: 87337
Identificador DC: https://oa.upm.es/87337/
Identificador OAI: oai:oa.upm.es:87337
URL Portal Científico: https://portalcientifico.upm.es/es/ipublic/item/9095086
Identificador DOI: 10.1017/jfm.2020.852
URL Oficial: https://www.cambridge.org/core/journals/journal-of...
Depositado por: iMarina Portal Científico
Depositado el: 30 Ene 2025 10:31
Ultima Modificación: 31 Ene 2025 13:07