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Nicolas Biver, Dominique Bockelée-Morvan, Pierre Colom, Jacques Crovisier,
John K. Davies, William R.F. Dent, Didier Despois, Eric Gérard, Emmanuel
Lellouch, Heike Rauer, Raphael Moreno, Gabriel Paubert
Abstract: Since soon after its discovery at 7 AU from the Sun, comet Hale-Bopp has
been studied by radio spectroscopy to investigate the gas species
associated with its activity. We present an extensive monitoring performed
with the Nançay, IRAM-30m and JCMT radio telescopes, showing the
progressive release of CO, CH OH, HCN, OH, H S, CS, H CO, CH CN
and HNC as the comet approached the Sun from 6.9 to 1.4 AU. These data
provide clues to the chemical and physical state of cometary ices and allow
us to investigate the fractionation processes that accompany their
sublimation upon solar heating. Simultaneous observations of the relative
intensities and line shapes of several transitions are used to measure the
expansion velocity and temperature of the cometary atmosphere and their
evolution with heliocentric distance, as well as to study possible
sublimation from icy grains. The more volatile species are relatively more
abundant in the coma far from the Sun, but there is no direct correlation
between overabundance and volatility. Evidences for H O sublimation from
icy grains are seen beyond 3.5 AU from the Sun. The change from a CO-driven
coma to a H O-driven coma occured at about 3 AU. The gas outflow
velocity and temperature increased with decreasing heliocentric distance.
Published in Science, 275, 1915 (1997).
lucas@iram.fr