Viscoelastic Tides of Mercury and the Determination of its Inner Core Size

G. Steinbrügge, S. Padovan, H. Hussmann, T. Steinke, A. Stark, J. Oberst

Research output: Contribution to journalArticleScientificpeer-review

6 Citations (Scopus)
27 Downloads (Pure)

Abstract

We computed interior structure models of Mercury and analyzed their viscoelastic tidal response. The models are consistent with MErcury Surface, Space Environment, GEochemistry, and Ranging mission inferences of mean density, mean moment of inertia, moment of inertia of mantle and crust, and tidal Love number k2. Based on these constraints we predict the tidal Love number h2 to be in the range from 0.77 to 0.93. Using an Andrade rheology for the mantle the tidal phase-lag is predicted to be 4° at maximum. The corresponding tidal dissipation in Mercury's silicate mantle induces a surface heat flux smaller than 0.16 mW/m2. We show that, independent of the adopted mantle rheological model, the ratio of the tidal Love numbers h2 and k2 provides a better constraint on the maximum inner core size with respect to other geodetic parameters (e.g., libration amplitude or a single Love number), provided it responds elastically to the solar tide. For inner cores larger than 700 km, and with the expected determination of h2 from the upcoming BepiColombo mission, it may be possible to constrain the size of the inner core. The measurement of the tidal phase-lag with an accuracy better than ≈0.5° would further allow constraining the temperature at the core-mantle boundary for a given grain size and therefore improve our understanding of the physical structure of Mercury's core.

Original languageEnglish
Pages (from-to)2760-2772
Number of pages13
JournalJRG Planets
Volume123
Issue number10
DOIs
Publication statusPublished - 2018

Keywords

  • h
  • inner core
  • Mercury
  • tides

Fingerprint Dive into the research topics of 'Viscoelastic Tides of Mercury and the Determination of its Inner Core Size'. Together they form a unique fingerprint.

Cite this