The interior structure of Mercury: what we know, what we expect from BepiColombo

Citation
T. Spohn et al., The interior structure of Mercury: what we know, what we expect from BepiColombo, PLANET SPAC, 49(14-15), 2001, pp. 1561-1570
Citations number
27
Categorie Soggetti
Space Sciences
Journal title
PLANETARY AND SPACE SCIENCE
ISSN journal
00320633 → ACNP
Volume
49
Issue
14-15
Year of publication
2001
Pages
1561 - 1570
Database
ISI
SICI code
0032-0633(200112)49:14-15<1561:TISOMW>2.0.ZU;2-1
Abstract
The BepiColombo mission is planned to very accurately measure the gravity f ield, the topography, and the tidal Love numbers of Mercury. In this paper, we review our present knowledge of the interior structure and show how the data from BepiColombo can be used to improve on our knowledge. We show tha t our present estimates of the core mass and volume depend mostly on our co nfidence in cosmochemically constrained values of the average silicate shel l and core densities. The moment of inertia (MOI) C about the rotation axis will be determined very accurately from the degree 2 components of the gra vity field and from measurements of the obliquity and the libration frequen cy of the rotation axis. The ratio C-m/C between the MOI of the solid plane t to the MOI of the planet, both about the rotation axis, will additionally be obtained. If the core is liquid or if there is a liquid outer core, C-m /C will be around 0.5. In this case, C-m can be identified with the MOI of the silicate shell. If the core is solid, C-m/C will be about 1. The MOI C can be used to test and refine present models but will most likely not per se help to increase the confidence in the two-layer model beyond the presen t level, at least if there is a substantial inner core. C and C-m/C can be used to calculate the inner core radius and the outer core density, assumin g the silicate shell density and the inner core density are given by cosmoc hemistry. The accuracy of the outer core density estimate depends largely o n the confidence in the cosmochemical data. The inner core radius can be de termined to the accuracy of the densities if the inner core radius is great er than 0.5 core radii. These values can be checked against the Love number of the planet. The higher order components of the gravity field can be use d to estimate core-mantle boundary undulations and crust thickness variatio ns. The former will dominate the gravity field at long wavelength, while th e latter will dominate at short wavelengths. (C) 2001 Elsevier Science Ltd. All rights reserved.