Mercury is the innermost and a less known terrestrial planet of the So
lar System. It possesses a very high density (5.3 g/cm-3 at 10 kbar),
a small but unexpected magnetic moment (6 x 10(-3) that of Earth), and
a tenuous exosphere; ground-based radar observations indicate that wa
ter ice may exist at the poles. There are still fundamental questions
about its accretion and cratering history, and its thermal and chemica
l evolution. The size of Mercury's magnetosphere is just 5% of that of
Earth; substorms last 5 min, on average, and their generation process
is influenced by the absence of an ionosphere. The model payload of M
ercury Orbiter includes a multi-spectral imager, a gamma- and X-ray de
tector, a magnetometer, charged-particle analysers, a wave receiver an
d an ion emitter for spacecraft potential control. The spacecraft, the
design of which is inherited from ESA's Cluster spacecraft, has a dry
mass of 626 kg and is stabilised at 10 rpm, but the telemetry antenna
is despun. The bit rate varies between 1.4 and 9 kb/s over the range
1.6-0.64 AU. The spacecraft, launched from Kourou with an Ariane-5, re
aches its destination after two gravity assists at Venus and two at Me
rcury. Its orbit is polar with periherm and apherm altitudes of 400 an
d 16 800 km, respectively. The spacecraft's operating lifetime around
Mercury is 3 Hermean years.