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.
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