Silicon Gas on an Exoplanet: The Clouds Have Lifted ✛ ✦

Original: "The CRIMSON survey I: super-stellar SiO in the directly imaged companion TWA 5 B from high-resolution M-band spectroscopy"
arXiv:2606.03824v1 · 2026-06-02 · CC BY 4.0 · 1 min
For the first time, silicon monoxide, a telltale gas that sandy clouds are absent, has been detected in the atmosphere of a directly imaged planet.

Planet TWA5B is a young exoplanet giant, 25 times heavier than Jupiter, made mostly of hydrogen and helium and orbiting a pair of red dwarfs in the constellation Hydra. Its atmosphere is surprisingly clear: by spreading its light into a rainbow (spectroscopy), astronomers peered through it like clean glass and found no sandy haze. Instead, they spotted signatures of water and carbon monoxide (CO, with carbon and oxygen), and then an unexpected trace: gaseous silicon monoxide (SiO).

On Earth, this gas would instantly clump into sand, but at 2400 °C the silicon drifts freely, never forming clouds. This is the first solid detection of gaseous silicon in a directly imaged planet’s atmosphere. The abundance of SiO reveals it was born far from its star, where the planet-forming disk was loaded with icy grains. No sandy silicate dust fogs the view: we can see straight through to the atmosphere’s depths.

From now on, this gas acts as a telltale: if SiO is scarce on a cooler planet, dense sand clouds are hiding it. Future JWST observations will apply this diagnosis to other scorching worlds.

Silicon monoxide (SiO) is a molecule that appears as a gas both in the atmospheres of hot exoplanets and in interstellar space, born in supernova shockwaves. On Earth, it quickly freezes into solid silicates, the very stuff of sand.

[\mathrm{Si}/\mathrm{H}] = 1.41 \pm 0.2 \,\mathrm{dex}
Logarithmic measure of silicon enrichment relative to hydrogen compared to the Sun. A value of 1.41 dex means silicon is 26 times the solar level.
\mathrm{C/O} = 0.26 \pm 0.05
The carbon-to-oxygen ratio is a chemical indicator of where in the protoplanetary disk the planet formed. A value below 0.8 is typical of regions beyond the CO snow line, where carbon is locked in solid ices.
Scientists
Christian DopplerD. B. McLaughlinDidier QuelozMichel MayorR. A. RossiterDavid Charbonneau
Concepts
titanium oxide silicon carbide carbon to oxygen ratio silicon carbon monoxide sulfur dioxide titan gas cloud sodium gas dust young stellar object glycine chemical galactic archaeology mantle rocky planet magnesium cosmic dust analysis galactic halo cloud