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New models predict how 'lava planets' evolve and change over time

International research lead by York University professor sheds light on 'lava planets'
Artistic illustration of the internal structure of a lava planet in a cold state, showing a day‑side magma ocean overlain by a mineral atmosphere. The arrows indicate the direction of heat transport within the planet's interior and the thermal radiation emitted from its night side. Credit: Romain Jean-Jaques (Instagram: @romainjean.jacques)

A new paper led by a York University professor and in Nature Astronomy introduces a simple theoretical framework to describe the evolution of the coupled interior–atmosphere system of hot rocky exoplanets known as "lava planets."

"Lava planets are in such extreme orbital configurations that our knowledge of rocky planets in the solar system does not directly apply, leaving scientists uncertain about what to expect when observing lava planets," says first author Charles-Édouard Boukaré, Assistant Professor in York University's Department of Âé¶¹ÒùÔºics and Astronomy in the Faculty of Science.

"Our simulations propose a conceptual framework for interpreting their evolution and provide scenarios to probe their internal dynamics and chemical changes over time. These processes, though greatly amplified in lava planets, are fundamentally the same as those that shape rocky planets in our own solar system."

Exotic worlds may unveil processes driving planetary evolution

Lava planets are Earth- to super-Earth–sized worlds orbiting extremely close to their host stars, completing an orbit in less than a single Earth day. Much like Earth's moon, they are expected to be tidally locked, always showing the same face to their star. Their dayside surfaces reach such extreme temperatures that silicate rocks melt—and even vaporize—creating conditions unlike anything in our solar system. These exotic worlds, easily observable due to their ultra short orbital period, provide unique insights into the fundamental processes that shape planetary evolution.

Probing planetary interiors through atmosphere and surface properties

The study combines expertise in geophysical fluid mechanics, exoplanetary atmospheres, and mineralogy to explore how the compositions of lava planets evolve through a process akin to distillation. When rocks melt or vaporize, elements such as magnesium, iron, silicon, oxygen, sodium, and potassium partition differently between vapor, liquid, and solid phases. The unique orbital configuration of lava planets maintains vapor–liquid and solid–liquid equilibria over billions of years, driving long-term chemical evolution.

The paper, "The role of interior dynamics and differentiation on the surface and atmosphere of lava planets," was co-authored by Daphné Lemasquerier (University of St Andrews), Nicolas B. Cowan (McGill University), Lisa Dang (University of Waterloo), Henri Samuel, James Badro, Aurélien Falco and Sébastien Charnoz (Université Paris Cité).

Time evolution of the temperature field corresponding to Fig. 3. Credit: Nature Astronomy (2025). DOI: 10.1038/s41550-025-02617-4

Using unprecedented numerical simulations, the team predicts two end-member evolutionary states:

  • Fully molten interior (likely young planets): The atmosphere mirrors the bulk planetary composition, and heat transport within the molten interior keeps the nightside surface hot and dynamic.
  • Mostly solid interior (likely older planets): Only a shallow lava ocean remains on the dayside, and the atmosphere becomes depleted in elements such as sodium, potassium, and iron.

Testing hypotheses with the James Webb Space Telescope

Boukaré explains that this research on lava exoplanets began as a highly exploratory effort with few initial expectations. It builds on a novel modeling approach he developed to study molten rocky planets in collaboration with colleagues at the Institute de Âé¶¹ÒùÔºique du Globe de Paris, Université Paris Cité, published in Nature earlier this year.

What began as an exploratory study has since opened a promising new line of research. The predictions outlined in this work helped secure 100 hours of observation time on the James Webb Space Telescope (JWST)—the most advanced infrared observatory ever built, featuring a 6.5‑meter segmented mirror and ultra‑sensitive instruments capable of probing the earliest galaxies and the atmospheres of distant exoplanets with unprecedented precision. These upcoming JWST observations, led by co-author Prof. Dang, will directly test the theoretical framework proposed in this study.

"We really hope we can observe and distinguish old lava planets from young planets. If we can do this, it would mark an important step toward moving beyond the traditional snapshot view of exoplanets," says Boukaré.

More information: The role of interior dynamics and differentiation on the surface and in the atmosphere of lava planets, Nature Astronomy (2025). ,

Journal information: Nature , Nature Astronomy

Provided by York University

Citation: New models predict how 'lava planets' evolve and change over time (2025, July 29) retrieved 30 July 2025 from /news/2025-07-lava-planets-evolve.html
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