The Influence of Tidal Heating on the Habitability of Planets Orbiting White Dwarfs

被引:11
作者
Becker, Juliette [1 ]
Seligman, Darryl Z. [2 ,3 ]
Adams, Fred C. [4 ,5 ]
Styczinski, Marshall J. [6 ]
机构
[1] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
[2] Cornell Univ, Dept Astron, 122 Sci Dr, Ithaca, NY 14853 USA
[3] Cornell Univ, Carl Sagan Inst, 122 Sci Dr, Ithaca, NY 14853 USA
[4] Univ Michigan, Phys Dept, Ann Arbor, MI 48109 USA
[5] Univ Michigan, Astron Dept, Ann Arbor, MI 48109 USA
[6] Cornell Univ, Carl Sagan Inst, 122 Sci Dr, Ithaca, NY 14853 USA
基金
美国国家科学基金会;
关键词
TRANSITING PLANETS; INTERIOR STRUCTURE; KOZAI MIGRATION; GIANT PLANET; MASS; DISSIPATION; EVOLUTION; SYSTEMS; DEBRIS; EARTH;
D O I
10.3847/2041-8213/acbe44
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In recent years, there have been a growing number of observations indicating the presence of rocky material in short-period orbits around white dwarfs. In this Letter, we revisit the prospects for habitability around these post-main-sequence star systems. In addition to the typically considered radiative input luminosity, potentially habitable planets around white dwarfs are also subjected to significant tidal heating. The combination of these two heating sources can, for a narrow range of planetary properties and orbital parameters, continuously maintain surface temperatures amenable for habitability for planets around white dwarfs over timescales up to 10 Gyr. We show that for a specific locus of orbital parameter space, tidal heating can substantially extend the timescale of continuous habitability for a planet around a white dwarf.
引用
收藏
页数:8
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