Fig. 4

Central temperature (left column), central pressure (middle column), and M-R relation (right column) for the Type-1 planets. The different rows correspond to different assumed values for ΔTTBL (see annotations at the right). While the core temperature increases significantly for higher ΔTTBL the central pressure and radius remain vastly unaffected. The mass-radius relations for pure H2O, MgO and Fe are shown for reference.
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