Japan Geoscience Union Meeting 2024

Presentation information

[E] Oral

P (Space and Planetary Sciences ) » P-CG Complex & General

[P-CG19] Exoplanet

Tue. May 28, 2024 9:00 AM - 10:30 AM 102 (International Conference Hall, Makuhari Messe)

convener:Takanori Kodama(Earth-Life Science Institute, Tokyo Institute of Technology), Shota Notsu(Earth and Planetary System Science Group, Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Yui Kawashima(Tohoku University), Mayuko Mori(The University of Tokyo), Chairperson:Takanori Kodama(Earth-Life Science Institute, Tokyo Institute of Technology), Shota Notsu(Earth and Planetary System Science Group, Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo)


9:30 AM - 9:45 AM

[PCG19-03] Low densities, eccentricities, and entropies in the young, compact multi-planet system V1298 Tau

*John Livingston1, Erik Petigura2, Trevor David3, Jerome de Leon4, Akihiko Fukui4, Norio Narita4, Motohide Tamura4,1 (1.ABC/NAOJ, 2.UCLA, 3.Flatiron, 4.University of Tokyo)

Keywords:Transits, Transit timing variations, Young planetary systems, Photoevaporation

Close-in planetary systems are ubiquitous in the Galaxy, with constituent planet sizes that rarely exceed four times the size of Earth. The discovery of four large (5–10 Earth radii) planets transiting the young star V1298 Tau hinted that close-in, gaseous planets start off larger and with lower densities than the typical systems observed at mature stages. This interpretation is supported by planet formation models which predict larger sizes and lower densities for planets at young ages. It was surprising, then, when high planetary masses and densities were inferred for the two outer planets in the V1298 Tau system from radial velocity measurements. Here we report the results of a campaign to measure planet masses in the V1298 Tau system through transit-timing variations. We measure masses in the range of 3-21 Earth masses, corresponding to densities of 0.02-0.26 g/cm3. Dynamical simulations confirm our preferred orbital solutions are stable on timescales of 106 yr and allow us to reject alternative solutions with higher planet masses. These low planetary densities are compatible with the substantial contraction and/or loss of H/He envelopes over timescales of at least tens of millions of years, and suggest the occurrence of rapid mass-loss during disk dispersal and a corrsponding decrease in entropy known as "boil-off".