Two-dimensional hydrodynamic simulations show that tidally assisted escape of vapor from the lunar magma ocean can explain the Moon's sodium and potassium depletion, and predict a leading/trailing surface dichotomy.
LavAtmos: An open source chemical equilibrium vaporisation code for lava worlds
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abstract
To date, over 500 short-period rocky planets with equilibrium temperatures above 1500 K have been discovered. Such planets are expected to support magma oceans, providing a direct interface between the interior and the atmosphere. This provides a unique opportunity to gain insight into their interior compositions through atmospheric observations. A key process in doing such work is the vapor outgassing from the lava surface. LavAtmos is an open-source code that calculates the equilibrium chemical composition of vapor above a dry melt for a given composition and temperature. Results show that the produced output is in good agreement with the partial pressures obtained from experimental laboratory data as well as with other similar codes from literature. LavAtmos allows for the modeling of vaporization of a wide range of different mantle compositions of hot rocky exoplanets. In combination with atmospheric chemistry codes, this enables the characterization of interior compositions through atmospheric signatures.
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astro-ph.EP 1years
2024 1verdicts
CONDITIONAL 1representative citing papers
citing papers explorer
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Hydrodynamical simulations of proto-Moon degassing
Two-dimensional hydrodynamic simulations show that tidally assisted escape of vapor from the lunar magma ocean can explain the Moon's sodium and potassium depletion, and predict a leading/trailing surface dichotomy.