Spectroscopy shows that accretion of rocky planetary material can change a white dwarf's visible colour — e.g., sodium and other elements in the atmosphere of WD J1330+6435 absorb orange wavelengths and leave a green tint. That means the remains of destroyed planets leave observable fingerprints in a star's light, giving astronomers a direct way to probe exoplanet composition long after the planets are gone.
— Provides a new, directly observable connection between planet destruction and stellar appearance, broadening how we study planetary systems and offering a vivid hook for public engagement with exoplanet science.
BeauHD
2026.10.17
100% relevant
The white dwarf WD J1330+6435 (≈326 ly) shows atmospheric sodium, calcium and lithium that models indicate absorb orange light and produce a green hue; results published in RAS Techniques and Instruments and reported by Space.com.
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