Published April 21, 2026 | Version 1.1.0
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PALEOS MgSiO₃ EoS Lookup Table for PROTEUS

  • 1. ROR icon University of Groningen

Description

PALEOS MgSiO₃ Lookup Tables for PROTEUS

Precomputed MgSiO₃ equation of state lookup tables generated with PALEOS, designed for the PROTEUS planetary interior model. The tables cover pressures up to 100 TPa, extending the EoS coverage to the regime relevant for super-Earth and sub-Neptune interiors.

Contents

Two table files are provided:

File Phase T range Resolution
paleos_mgsio3_tables_pt_proteus_solid.dat Solid 300 K → max(T_liquidus) 150 ppd
paleos_mgsio3_tables_pt_proteus_solid_highres.dat Solid 300 K → max(T_liquidus) 600 ppd
paleos_mgsio3_tables_pt_proteus_liquid.dat Liquid min(T_solidus) → 10⁵ K 150 ppd
paleos_mgsio3_tables_pt_proteus_liquid_highres.dat Liquid min(T_solidus) → 10⁵ K 600 ppd

Both tables share a common pressure grid: P = 0 Pa plus a log-uniform grid from 1 bar to 100 TPa at 150 or 600 points per decade. The temperature grids are also log-uniform at 150 or 600 points per decade. The temperature bounds are derived from the PROTEUS solidus and liquidus files: specifically min(T_solidus) and max(T_liquidus) as global bounds.

The grids are designed to be rectangular. Some points are missing where the EoS solver failed to converge; when reconstructing the full grid for interpolation, these entries should be filled with NaN. The nonconverging regions should not affect the physically relevant domain (beyond liquidus for the solid table, vapor/supercritical phase for the liquid table). 

Columns

Each row contains 10 columns, all in SI units:

  1. P — Pressure [Pa]
  2. T — Temperature [K]
  3. rho — Density [kg/m³]
  4. u — Specific internal energy [J/kg]
  5. s — Specific entropy [J/(kg·K)]
  6. cp — Isobaric heat capacity [J/(kg·K)]
  7. cv — Isochoric heat capacity [J/(kg·K)]
  8. alpha — Thermal expansion coefficient [K⁻¹]
  9. nabla_ad — Adiabatic gradient (d ln T / d ln P)_S [dimensionless]
  10. phase — Phase identifier

Phase selection

For the solid table, phase selection at each (P, T) point follows the full PALEOS MgSiO₃ phase diagram. At temperatures above the PALEOS melting curve (which can occur since the solid table extends to the PROTEUS liquidus), the code falls back to the solid phase stable just below the melting curve and evaluates that EoS at the requested temperature. The liquid table uses Wolf+Bower18 everywhere.

Generating the tables

The notebook to regenerate these tables is available in the PALEOS repository at utils/mgsio3_tables_proteus.ipynb. It contains a single clearly marked User Input cell where all parameters (file paths, P/T ranges, resolution, output filenames) can be adjusted.

* * *

Version log (1.1.0): covered all PROTEUS solidi/liquidi, implemented consistent U₀/S₀ per-phase shifts to ensure dS/dT > 0 everywhere and Gibbs-energy continuity at triple points, and generated high-resolution (600 ppd) tables.

Files

Files (1.4 GB)

Name Size Download all
md5:4b5c14255ca845880a2e940110861df1
44.1 MB Download
md5:f67e0f049fe5f3d5cba0adef6ab7632f
702.9 MB Download
md5:9cab570e3331b329c15715628a504fad
37.9 MB Download
md5:fddb2c3f392e1c2f73a326d702a98c70
604.5 MB Download

Additional details

Software

Repository URL
https://github.com/maraattia/PALEOS
Programming language
Python , Jupyter Notebook
Development Status
Active