Systems hosting multiple giant planets are important laboratories for understanding planetary formation and migration processes. We present a nearly decade-long Doppler spectroscopy campaign from the Keck-I telescope to characterize the two transiting giant planets orbiting Kepler-511 on orbits of 27 days and 297 days. The radial velocity measurements yield precise masses for both planets, which we use to infer their bulk heavy element content. Both planets contain approximately 30 Earth masses of heavy elements, but their bulk metallicities (i.e., the ratio between metal mass and total mass) are drastically different (0.86 ± 0.04 and 0.22 ± 0.04 respectively). Envelope mass loss cannot account for this difference due to the relatively large orbital distance and mass of the inner planet. We conclude that the outer planet underwent runaway gas accretion while the inner planet did not. This bifurcation in accretion histories is likely a result of the accretion of gas with very different metallicities by the two planets or the late formation of the inner planet from a merger of sub-Neptunes. Kepler-511 uniquely demonstrates how giant planet formation can produce strikingly different outcomes even for planets in the same system.
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Chachan et al. (2024) studied this question.
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