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Extrasolar Carbon Planets

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arxiv astro-ph/0504214 v2 pith:BGINYYTR submitted 2005-04-08 astro-ph

classification astro-ph
keywords planetscarboncompoundsextrasolarformhighotherprotoplanetary
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We suggest that some extrasolar planets <~ 60 Earth masses will form substantially from silicon carbide and other carbon compounds. Pulsar planets and low-mass white dwarf planets are especially good candidate members of this new class of planets, but these objects could also conceivably form around stars like the Sun. This planet-formation pathway requires only a factor of two local enhancement of the protoplanetary disk's C/O ratio above solar, a condition that pileups of carbonaceous grains may create in ordinary protoplanetary disks. Hot, Neptune-mass carbon planets should show a significant paucity of water vapor in their spectra compared to hot planets with solar abundances. Cooler, less massive carbon planets may show hydrocarbon-rich spectra and tar-covered surfaces. The high sublimation temperatures of diamond, SiC, and other carbon compounds could protect these planets from carbon depletion at high temperatures.

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Cited by 2 Pith papers

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score. Full citation record

  1. Host--Non-host Differences in Stellar Chemistry, Activity, and Birth Radius: Hints of Distinct Formation Environments for Earth-like Planets and Sub-Neptunes

    astro-ph.SR 2026-08 conditional novelty 6.0 of 10

    After age-mass matching and bias correction, host and non-host stars are chemically similar overall, but Earth-like and sub-Neptune hosts show opposite O, Mg, and Si trends, and sub-Neptune hosts are less active and b...

  2. Carbon, oxygen, and iron abundances in disk and halo stars. Implications of 3D non-LTE spectral line formation

    astro-ph.SR 2019-08 conditional novelty 6.0 of 10

    Applying 3D non-LTE corrections to C I and O I lines removes the 1D LTE turnover in [C/O] versus [O/H] and reveals a higher C/O in thin-disk planet hosts.

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