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A theoretical investigation into the trapping of noble gases by clathrates on Titan
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A theoretical investigation into the trapping
of noble gases by clathrates on Titan
Caroline Thomas, Sylvain Picaud,
Olivier Mousis and Vincent Ballenegger
Universite? de Franche-Comte?, Institut UTINAM,
CNRS/INSU, UMR 6213, 25030 Besanc?on Cedex, France
Abstract
In this paper, we use a statistical thermodynamic approach to quantify the effi-
ciency with which clathrates on the surface of Titan trap noble gases. We consider
different values of the Ar, Kr, Xe, CH4, C2H6 and N2 abundances in the gas phase
that may be representative of Titan’s early atmosphere. We discuss the effect of the
various parameters that are chosen to represent the interactions between the guest
species and the ice cage in our calculations. We also discuss the results of varying
the size of the clathrate cages. We show that the trapping efficiency of clathrates
is high enough to significantly decrease the atmospheric concentrations of Xe and,
to a lesser extent, of Kr, irrespective of the initial gas phase composition, provided
that these clathrates are abundant enough on the surface of Titan. In contrast, we
find that Ar is poorly trapped in clathrates and, as a consequence, that the at-
mospheric abundance of argon should remain almost constant. We conclude that
the mechanism of trapping noble gases via clathration can explain the deficiency
in primordial Xe and Kr observed in Titan’s atmosphere by Huygens, but that this
mechanism is not sufficient to explain the deficiency in Ar.
Key words: Titan; Clathrates; Atmosphere; Noble gases; Cassini-Huygens
1 Introduction
Saturn’s largest satellite, Titan, has a thick atmosphere, primarily consisting of
nitrogen, with a few percent of methane (Niemann et al., 2005). An unexpected
feature of this atmosphere is that no primordial noble gases, other than Ar,
were detected by the Gas Chromatograph Mass Spectrometer (GCMS) aboard
Email address: caroline.thomas@univ-fcomte.fr
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