A common origin of magnetism from planets to white dwarfs

Isolated magnetic white dwarfs have field strengths ranging from kilogauss to gigagauss. However, the origin of the magnetic field has not been hitherto elucidated. Whether these fields are fossil, hence the remnants of original weak magnetic fields amplified during the course of the evolution of th...

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Detalles Bibliográficos
Autores: Isern Vilaboy, Jordi, García-Berro Montilla, Enrique|||0000-0002-1623-5838, Kulebi, Baybar, Lorén Aguilar, Pablo
Tipo de recurso: artículo
Fecha de publicación:2017
País:España
Institución:Universitat Politècnica de Catalunya (UPC)
Repositorio:UPCommons. Portal del coneixement obert de la UPC
Idioma:inglés
OAI Identifier:oai:upcommons.upc.edu:2117/104213
Acceso en línea:https://hdl.handle.net/2117/104213
https://dx.doi.org/10.3847/2041-8213/aa5eae
Access Level:acceso abierto
Palabra clave:White dwarf stars
Stars--Magnetic fields
Stars - interiors
Estels nans
Camps magnètics solars
Àrees temàtiques de la UPC::Física::Astronomia i astrofísica
Descripción
Sumario:Isolated magnetic white dwarfs have field strengths ranging from kilogauss to gigagauss. However, the origin of the magnetic field has not been hitherto elucidated. Whether these fields are fossil, hence the remnants of original weak magnetic fields amplified during the course of the evolution of their progenitor stars, or are the result of binary interactions, or, finally, they are produced by other internal physical mechanisms during the cooling of the white dwarf itself, remains a mystery. At sufficiently low temperatures, white dwarfs crystallize. Upon solidification, phase separation of its main constituents, 12C and 16O, and of the impurities left by previous evolution occurs. This process leads to the formation of a Rayleigh–Taylor unstable liquid mantle on top of a solid core. This convective region, as it occurs in solar system planets like the Earth and Jupiter, can produce a dynamo able to yield magnetic fields of strengths of up to 0.1 MG, thus providing a mechanism that could explain magnetism in single white dwarfs.