Saturn layered structure and homogeneous evolution models with different EOSs
Saturn layered structure and homogeneous evolution models with different EOSs
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DOI:
10.1016/j.icarus.2013.04.018
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发表时间:
2013-04
期刊:
影响因子:
3.2
通讯作者:
N. Nettelmann;Robert Püstow;R. Redmer
中科院分区:
文献类型:
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作者:
N. Nettelmann;Robert Püstow;R. Redmer
The core mass of Saturn is commonly assumed to be 10–25M⊕as predicted by interior models with various equations of state (EOSs) and the Voyager gravity data, and hence larger than that of Jupiter (0–10M⊕). 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 0–20M⊕for SCvH-i and Sesame EOS and of 0–17M⊕for LM-REOS. Assuming an atmospheric helium mass abundance of 18%, we find maximum atmospheric metallicities, Zatmof 7× solar for SCvH-i and Sesame-based models and a total mass of heavy elements, MZof 25–30M⊕. Some models are Jupiter-like. With LM-REOS, we find MZ=16–20M⊕, less than for Jupiter, and Zatm≲3× solar. For Saturn, we compute moment of inertia values λ=0.2355(5). Furthermore, we confirm that homogeneous evolution leads to cooling times of only ∼2.5Gyr, independent on the applied EOS. Our results demonstrate the need for accurately measured atmospheric helium and oxygen abundances, and of the moment of inertia for a better understanding of Saturn’s structure and evolution.