Chemical and Isotopic Homogeneity Between the L Dwarf CD-35 2722 B and its Early M Host Star
Gavin Wang, Jerry Xuan, Darío Picos, Zhoujian Zhang, Yapeng Zhang, Dimitri Mawet, Chih-Chun Hsu, Jason Wang, Geoffrey Blake, Jean-Baptiste Ruffio, Katelyn Horstman, Ben Sappey, Yinzi Xin, Luke Finnerty, Daniel Echeverri, Nemanja Jovanovic, Ashley Baker, Randy Bartos, Benjamin Calvin, Sylvain Cetre, Jacques-Robert Delorme, Greg Doppmann, Michael Fitzgerald, Joshua Liberman, Ronald López, Evan Morris, Jacklyn Pezzato-Rovner, Caprice Phillips, Tobias Schofield, Andrew Skemer, James Wallace, Ji Wang
TL;DR
CD-35 2722 B, a ~30 M_Jup L dwarf companion to a young AB Doradus member, is analyzed with high-resolution KPIC $K$-band spectroscopy to constrain bulk properties, chemical abundances, and cloud signatures. By retrieving equilibrium-chemistry abundances and testing different $P$–$T$ treatments, the study finds [M/H] for the host of $-0.16\pm0.25$ dex and [M/H] for the companion of $0.27^{+0.14}_{-0.13}$ dex, with C/O ≈ 0.55 and a robust detection of $^{13}$CO in the companion at ~5σ, giving $^{12}$CO/$^{13}$CO ≈ 159. The host and companion show chemical consistency within ~1.5σ for metallicity and ~0.6σ for isotopologue ratios, supporting formation via gravitational instability. The lack of definitive clouds in the $K$-band data highlights the sensitivity limitations of high-resolution near-infrared spectra to aerosols and motivates broader-wavelength observations. Together, the results inform planet–star formation pathways and illustrate the value of isotopologue and metallicity diagnostics in young, wide-separation substellar systems.
Abstract
CD-35 2722 B is an L dwarf companion to the nearby, $\sim 50-200$ Myr old M1 dwarf CD-35 2722 A. We present a detailed analysis of both objects using high-resolution ($R \sim 35,000$) $K$ band spectroscopy from the Keck Planet Imager and Characterizer (KPIC) combined with archival photometry. With a mass of $30^{+5}_{-4} M_{\mathrm{Jup}}$ (planet-to-host mass ratio 0.05) and projected separation of $67\pm4$ AU from its host, CD-35 2722 B likely formed via gravitational instability. We explore whether the chemical composition of the system tells a similar story. Accounting for systematic uncertainties, we find $\mathrm{[M/H]}=-0.16^{+0.03}_{-0.02} \mathrm{(stat)} \pm 0.25 \mathrm{(sys)}$ dex and $^{12}\mathrm{C}/^{13}\mathrm{C}=132^{+20}_{-14}$ for the host, and $\mathrm{[M/H]}=0.27^{+0.07}_{-0.06} (\mathrm{stat}) \pm 0.12 (\mathrm{sys})$ dex, $^{12}\mathrm{CO}/^{13}\mathrm{CO}=159^{+33}_{-24} \mathrm{(stat)}^{+40}_{-33} \mathrm{(sys)}$, and $\mathrm{C/O} = 0.55 \pm 0.01 (\mathrm{stat}) \pm 0.04 (\mathrm{sys})$ for the companion. The chemical compositions for the brown dwarf and host star agree within the $1.5σ$ level, supporting a scenario where CD-35 2722 B formed via gravitational instability. We do not find evidence for clouds on CD-35 2722 B despite it being a photometrically red mid-L dwarf and thus expected to be quite cloudy. We retrieve a temperature structure which is more isothermal than models and investigate its impact on our measurements, finding that constraining the temperature structure to self-consistent models does not significantly impact our retrieved chemical properties. Our observations highlight the need for data from complementary wavelength ranges to verify the presence of aerosols in likely cloudy L dwarfs.
