Publications des scientifiques de l'IRD

Deguen R., Alboussiere T., Cardin Philippe. (2013). Thermal convection in Earth's inner core with phase change at its boundary. Geophysical Journal International, 194 (3), p. 1310-1334. ISSN 0956-540X.

Titre du document
Thermal convection in Earth's inner core with phase change at its boundary
Année de publication
2013
Type de document
Article référencé dans le Web of Science WOS:000323442800005
Auteurs
Deguen R., Alboussiere T., Cardin Philippe
Source
Geophysical Journal International, 2013, 194 (3), p. 1310-1334 ISSN 0956-540X
Inner core translation, with solidification on one hemisphere and melting on the other, provides a promising basis for understanding the hemispherical dichotomy of the inner core, as well as the anomalous stable layer observed at the base of the outer core-the so-called F-layer which might be sustained by continuous melting of inner core material. In this paper, we study in details the dynamics of inner core thermal convection when dynamically induced melting and freezing of the inner core boundary (ICB) are taken into account. If the inner core is unstably stratified, linear stability analysis and numerical simulations consistently show that the translation mode dominates only if the viscosity eta is large enough, with a critical viscosity value, of order similar to 3 x 10(18) Pa s, depending on the ability of outer core convection to supply or remove the latent heat of melting or solidification. If eta is smaller, the dynamic effect of melting and freezing is small. Convection takes a more classical form, with a one-cell axisymmetric mode at the onset and chaotic plume convection at large Rayleigh number. eta being poorly known, either mode seems equally possible. We derive analytical expressions for the rates of translation and melting for the translation mode, and a scaling theory for high Rayleigh number plume convection. Coupling our dynamic models with a model of inner core thermal evolution, we predict the convection mode and melting rate as functions of inner core age, thermal conductivity, and viscosity. If the inner core is indeed in the translation regime, the predicted melting rate is high enough, according to Alboussiere et al.'s experiments, to allow the formation of a stratified layer above the ICB. In the plume convection regime, the melting rate, although smaller than in the translation regime, can still be significant if eta is not too small. Thermal convection requires that a superadiabatic temperature profile is maintained in the inner core, which depends on a competition between extraction of the inner core internal heat by conduction and cooling at the ICB. Inner core thermal convection appears very likely with the low thermal conductivity value proposed by Stacey & Loper, but nearly impossible with the much higher thermal conductivity recently put forward by Sha & Cohen, de Koker et al. and Pozzo et al. We argue however that the formation of an iron-rich layer above the ICB may have a positive feedback on inner core convection: it implies that the inner core crystallized from an increasingly iron-rich liquid, resulting in an unstable compositional stratification which could drive inner core convection, perhaps even if the inner core is subadiabatic.
Plan de classement
Géophysique interne [066]
Identifiant IRD
PAR00010825
Contact