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Physical Sciences and Mathematics Commons

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Astrophysics and Astronomy

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Composition

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Full-Text Articles in Physical Sciences and Mathematics

On The Composition Of Young, Directly Imaged Giant Planets, Julianne I. Moses, Mark S. Marley, K. Zahnle, M. R. Line, Jonathan J. Fortney, T. S. Barman, Channon Visscher, Nikole K. Lewis, M. J. Wolff Sep 2016

On The Composition Of Young, Directly Imaged Giant Planets, Julianne I. Moses, Mark S. Marley, K. Zahnle, M. R. Line, Jonathan J. Fortney, T. S. Barman, Channon Visscher, Nikole K. Lewis, M. J. Wolff

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The past decade has seen significant progress on the direct detection and characterization of young, self-luminous giant planets at wide orbital separations from their host stars. Some of these planets show evidence for disequilibrium processes like transport-induced quenching in their atmospheres; photochemistry may also be important, despite the large orbital distances. These disequilibrium chemical processes can alter the expected composition, spectral behavior, thermal structure, and cooling history of the planets, and can potentially confuse determinations of bulk elemental ratios, which provide important insights into planet-formation mechanisms. Using a thermo/photochemical kinetics and transport model, we investigate the extent to which disequilibrium …


Chemistry Of Impact-Generated Silicate Melt-Vapor Debris Disks, Channon Visscher, Bruce Fegley Jr. Jan 2013

Chemistry Of Impact-Generated Silicate Melt-Vapor Debris Disks, Channon Visscher, Bruce Fegley Jr.

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In the giant impact theory for lunar origin, the Moon forms from material ejected by the impact into an Earth-orbiting disk. Here we report the initial results from a silicate melt-vapor equilibrium chemistry model for such impact-generated planetary debris disks. In order to simulate the chemical behavior of a two-phase (melt+vapor) disk, we calculate the temperature-dependent pressure and chemical composition of vapor in equilibrium with molten silicate from 2000 to 4000 K. We consider the elements O, Na, K, Fe, Si, Mg, Ca, Al, Ti, and Zn for a range of bulk silicate compositions (Earth, Moon, Mars, eucrite parent body, …