Constraining the Bulk Composition of Disintegrating Exoplanets Using Combined Transmission Spectra from JWST and SPICA
Ayaka Okuya, Satoshi Okuzumi, Kazumasa Ohno, Teruyuki Hirano

TL;DR
This study demonstrates that combining JWST and SPICA infrared transmission spectra can effectively constrain the mineral composition of dust tails around disintegrating exoplanets, revealing their surface mineralogy.
Contribution
It introduces a method to use combined JWST and SPICA spectra to diagnose dust tail composition, enhancing the understanding of disintegrating exoplanets' surfaces.
Findings
JWST can detect silicate and carbide features with high confidence in suitable targets.
SPICA can distinguish between Fe- and Mg-rich crystalline silicates in the dust tails.
Combined spectra improve constraints on planetary surface mineralogy.
Abstract
Disintegrating planets are ultra-short-period exoplanets that appear to have a comet-like dust tail. They are commonly interpreted as low-mass planets whose solid surface is evaporating and whose tail is made of recondensing minerals. Transmission spectroscopy of the dust tails could thus allow us to directly probe the elementary compositions of the planets. Previous work already investigated the feasibility of such observations using the JWST mid-infrared instrument. In this study, we explore if one can obtain a strong constrain on the tail composition by adding spectroscopy at longer wavelengths using SPICA mid-infrared instrument. We use a simple model for the spatial distribution of the dust tails and produce their synthetic transmission spectra assuming various dust compositions. We find that combined infrared spectra from JWST and SPICA will allow us to diagnose various components…
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