Experiments in the NH3-H2O System in the [0-1 GPa] Pressure Range -- Implications for the Deep Liquid Layer of Large Icy Satellites

Details Experiments in the NH3-H2O System in the [0-1 GPa] Pressure Range -- Implications for the Deep Liquid Layer of Large Icy Satellites Experiments in the NH3-H2O System in the [0-1 GPa] Pressure Range -- Implications for the Deep Liquid Layer of Large Icy Satellites

Mar 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002lpi....33.1461p&link_type=abstract

33rd Annual Lunar and Planetary Science Conference, March 11-15, 2002, Houston, Texas, abstract no.1461

Physics

Scientific paper

Experiments in the NH3-H2O system show that
peritectic melting temperature undergoes a jump between 450 and 500 MPa.
These results shed new light on the internal structure of Titan,
especially the fact that the ocean might be thinner than expected.

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