Saturn layered structure and homogeneous evolution models with different EOSs
N. Nettelmann, R. Puestow, R. Redmer

TL;DR
This study re-evaluates Saturn's internal structure and evolution using recent gravity data and various equations of state, revealing similar core mass ranges and emphasizing the importance of precise atmospheric composition measurements.
Contribution
It compares different EOSs for Saturn, providing updated core mass estimates and insights into its composition and evolution, highlighting the need for accurate atmospheric data.
Findings
Core mass ranges of 0-20 ME across EOSs
Maximum atmospheric metallicity of 7x solar for some models
Homogeneous evolution leads to ~2.5 Gyr cooling time
Abstract
The core mass of Saturn is commonly assumed to be 10-25 ME as predicted by interior models with various equations of state (EOSs) and the Voyager gravity data, and hence larger than that of Jupiter (0-10 ME). We here re-analyze Saturn's internal structure and evolution by using more recent gravity data from the Cassini mission and different physical equations of state: the ab initio LM-REOS which is rather soft in Saturn's outer regions but stiff at high pressures, the standard Sesame-EOS which shows the opposite behavior, and the commonly used SCvH-i EOS. For all three EOS we find similar core mass ranges, i.e. of 0-20 ME for SCvH-i and Sesame EOS and of 0-17 ME for LM-REOS. Assuming an atmospheric helium mass abundance of 18%, we find maximum atmospheric metallicities, Zatm of 7x solar for SCvH-i and Sesame-based models and a total mass of heavy elements, MZ of 25-30 ME. Some models…
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