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Audouin Dollfus : ウィキペディア英語版
Audouin Dollfus

Audouin Charles Dollfus (November 12, 1924 – October 1, 2010〔 http://www.enseignementsup-recherche.gouv.fr/cid53433/deces-de-audouin-dollfus-astronome-et-aeronaute-francais.html〕〔(Audouin Charles Dollfus 1924–2010 )〕) was a French astronomer and aeronaut, specialist in studies of the solar system and discoverer of Janus, a moon of Saturn.
==Life and career==
He was born in Paris to Charles Dollfus.
He studied at the University of Paris, obtaining a doctorate in physical
sciences in 1955. Beginning in 1946, Dollfus worked as an astronomer at the Meudon
Observatory, following his advisor and mentor Bernard Lyot. In particular, he
directed the Laboratory of Solar System Physics there. Until his passing, he was
an honorary astronomer at the Paris Observatory. Most of his work was
carried out based on observations from the Pic du Midi Observatory, and his preferred research method
is the use of polarized light as a diagnostic of the properties of solar system objects.
Through patient and persistent research and the development of new observational techniques,
he was able to obtain many remarkable results.
Dollfus has published more than 300 scientific
publications, relating primarily to astrophysics of the solar system.
Before the Viking spacecraft landed on Mars, the composition of the
Martian surface was the subject of many debates.
Dollfus tried to determine the composition of the Martian desert, through
comparison with the appearance
in polarized light of
several hundred terrestrial minerals.
He found that only pulverized limonite
(Fe2O3) corresponded with the appearance of Mars, and concluded that the Martian surface could be
composed of iron oxide. However, another astronomer, Gerald Kuiper of the
University of Chicago, disagreed with this conclusion, believing that fine-grained
igneous rocks were a better fit to the data, but subsequent observations proved
Dollfus correct.
By using the polarization of light, it is possible to detect an atmosphere
around a planet or natural satellite. In 1950, most scientists thought that
Mercury, because of its small size, had probably lost its atmosphere due to
molecular escape into space. Dollfus announced that he had detected a very
small atmosphere, again using polarization measurements made at the Pic du Midi
Observatory in the French Pyrenees. His discovery contradicted the previous
theoretical predictions based on the kinetic theory of gases. Dollfus estimated
that the atmospheric pressure at the surface of Mercury was approximately 1 mm
of mercury. The nature of gas composing this atmosphere was unknown but thought
to be a dense, heavy gas. It was however certain that the atmosphere of Mercury
must be less than 1/300th that of the Earth. Currently, it is known that the
atmosphere of Mercury is very thin indeed: only 10−15 bar, with the total mass
of the atmosphere not exceeding 1000 kg.
Mercury has dark zones which contrast with a brighter bottom; this was observed
first by Giovanni Schiaparelli in 1889. By using the refracting
telescope of the Pic du Midi Observatory, Dollfus was able in 1959 to
clearly resolve surface features as small as 300 km.
Dollfus also studied the possible presence of an atmosphere around the Moon.
The rate of dissipation into space of any gases on the Moon (except for certain
rare heavy elements) is so high that no substantial atmosphere is
possible. The presence of any atmosphere should be detectable by the
polarization of light; Bernard Lyot and later Dollfus showed that there was
no detectable polarization, thereby confirming the theoretical prediction that
the Moon lacks an atmosphere.
In 1966, Dollfus discovered Janus, a small inner moon of
Saturn. He made this discovery by observing at a time when
the rings, very close to Janus, were nearly edge-on to the Earth and thus
practically invisible. At this time he probably also observed Epimetheus,
a smaller moon which shares the same orbit as Janus, but he did not realize
these were two separate objects and it is Richard Walker that holds
credit for this discovery.

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