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Updated: Jul 12, 2026

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Metal-silicate Partitioning at High Pressure and Temperature: Experimental Methods and a Protocol to Suppress Highly Siderophile Element Inclusions
Published on: June 13, 2015
Noble gas partitioning between metal and silicate under high pressures
Summary
Noble gases like helium and argon show very low partitioning into iron melts under high pressure. This suggests Earth
Area of Science:
- Geochemistry
- Planetary Science
- High-Pressure Mineral Physics
Background:
- Noble gases are important tracers for understanding planetary formation and evolution.
- The partitioning behavior of elements between different melts provides insights into core formation processes.
Purpose of the Study:
- To quantify the partitioning of noble gases (He, Ne, Ar, Kr, Xe) between silicate and iron melts.
- To assess the implications of noble gas partitioning for the composition of Earth's core.
Main Methods:
- Experimental measurements of noble gas partitioning.
- Experiments conducted under high pressures (up to 100 kilobars).
- Analysis of noble gas concentrations in coexisting silicate and iron melts.
Main Results:
- Noble gas partition coefficients between silicate and iron melts are significantly less than unity.
- Partition coefficients systematically decrease with increasing pressure.
- Helium, neon, argon, krypton, and xenon all exhibit this behavior.
Conclusions:
- Under equilibrium conditions, Earth's core would contain only negligible amounts of noble gases.
- The partitioning behavior suggests noble gases are largely excluded from the metallic core during planetary differentiation.
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