Planetary systems commonly survive the evolution of single stars, as evidenced by terrestrial-like planetesimal debris observed orbiting and polluting the surfaces of white dwarfs (1, 2). This letter reports the identification of a circumbinary dust disk surrounding a white dwarf with a substellar companion in a 2.27 hr orbit. The system bears the dual hallmarks of atmospheric metal pollution and infrared excess (3, 4), however the standard (flat and opaque) disk configuration is dynamically precluded by the binary. Instead, the detected reservoir of debris must lie well beyond the Roche limit in an optically thin configuration, where erosion by stellar irradiation is relatively rapid. This finding demonstrates that rocky planetesimal formation is robust around close binaries, even those with low mass ratios.
1The formation and evolution of planetary systems around close binary stars is a challengingproblem, yet provides insight into the growth of planetesimals within evolving protoplanetary disks and planet formation in general. The small but increasing number of transiting circumbinary planets detected with Kepler (5, 6) are providing the first tests of theoretical formation models. To date, it has been shown that in situ formation is unfavorable for most of these Neptune-to Jupiter-sized bodies due to the destructive, dynamical effects of the central binary on planetesimal agglomeration in the regions where the planets currently orbit (7,8,9). However, for a range of masses including small planets, recent models predict favorable conditions for planetesimal growth within the snow line, and thus promoting efficient terrestrial planet formation around binaries (10,11,12).Atmospheric pollution in white dwarf stars offers a unique and powerful window into the assembly and chemistry of terrestrial exoplanets. There are now more than three dozen planetary system remnants made evident based on thermal and line emission from circumstellar disks (2), and several hundred where photospheric metals indicate ongoing or recent accretion of planetary debris (13). The current paradigm of disrupted and accreted asteroids has been unequivocally confirmed by numerous studies, including the recent detection of complex and rapidly evolving photometric transits from debris fragments orbiting near the Roche limit of one star (14,15, 16). To date, all polluted white dwarfs with detailed analyses indicate the sources are rocky planetesimals comparable in both mass and composition to large Solar System asteroids (17, 18,1), and thus objects that formed within a snow line. These findings unambiguously demonstrate that large planetesimal formation in the terrestrial zone of stars is robust and common.Until now, over 90% of such dusty and polluted white dwarf systems have been discovered among single stars, with a small fraction belonging to sufficiently wide binaries (a ≫ 100 AU) where the evolution of each star -and any associated planetary system -proceeds as a singleton. The white dwarf SDSS J155720.77+091624.6 (hereafter SDSS 1557) ...