Mass and eccentricity constraints on the planetary debris orbiting the white dwarf WD 1145+017
arXiv:1609.02563 · doi:10.1093/mnras/stw2293
Abstract
Being the first of its kind, the white dwarf WD 1145+017 exhibits a complex system of disintegrating debris which offers a unique opportunity to study its disruption process in real time. Even with plenty of transit observations there are no clear constraints on the masses or eccentricities of such debris. Using -body simulations we show that masses greater than approximately kg (a tenth of the mass of Ceres) or orbits that are not nearly circular () dramatically increase the chances of the system becoming unstable within two years, which would contrast with the observational data over this timespan. We also provide a direct comparison between transit phase shifts detected in the observations and by our numerical simulations.
Accepted to MNRAS
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Cited by in corpus (15)
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- Explaining the variability of WD 1145+017 with simulations of asteroid tidal disruption
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- Evidence for eccentric, precessing gaseous debris in the circumstellar absorption towards WD 1145+017
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- The lifetimes of planetary debris discs around white dwarfs
- Constraining the origin of the planetary debris surrounding ZTF J0139+5245 through rotational fission of a triaxial asteroid
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