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WD 2317+1830

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WD 2317+1830 is a white dwarf in the constellation Pegasus
WD 2317+1830

Artist's impression of a white dwarf with a disk
Credit: NOIRLab/NSF/AURA/J. da Silva
Image processing: M. Zamani and M. Kosari (NSF NOIRLab)
Observation data
Epoch J2000      Equinox J2000
Constellation Pegasus
Right ascension 23 17 26.74
Declination +18° 30′ 52.76″
Characteristics
Evolutionary stage white dwarf
Spectral type DZ
Apparent magnitude (G) 19.35
Astrometry
Radial velocity (Rv)25 ±31 km/s
Proper motion (μ) RA: -33.855 ±0.317 mas/yr
Dec.: -452.811 ±0.263 mas/yr
Parallax (π)26.4097 ± 0.3090 mas
Distance123 ± 1 ly
(37.9 ± 0.4 pc)
Details
Mass1.076+0.007
−0.008 M
Radius0.00793 ±0.00021 R
Surface gravity (log g)8.64 ±0.03 cgs
Temperature4557 ±63 K
Agecooling age: 6.388 Gyr
total age: 7.7+0.3
−0.4 Gyr
Other designations
SDSS J231726.72+183049.6, EQ J2317+1830, Gaia DR2 2818957013992481280
Database references
SIMBADdata

WD 2317+1830 (SDSS J231726.72+183049.6) is one of the first white dwarfs with lithium detected in its atmosphere. The white dwarf is surrounded by a debris disk and is actively accreting material. Researchers suggest that the presence of alkali metals indicates the accretion of crust material. Another work however cautions to use alkali metals as a single indicator of crust material. They suggest that such objects could be polluted by mantle material instead. An analysis in 2024 finds that the abundance of lithium is in agreement with Big Bang nucleosynthesis (BBN) and galactic nucleosynthesis. WD 2317+1830 likely was a star with sub-solar metallicity, which is evident from its old age, as well as from its thick disk or halo kinematics. This low metallicity means that the planetesimals that formed around this old white dwarf had a composition more similar to BBN abundances. The lithium-enhancement is not in agreement with the accretion of terrestrial continental crust material. The accretion of an exotic exoplanet is not ruled out, but the accretion of a primitive planetesimal is more likely. The accretion of an exomoon as a lithium source is excluded.

WD 2317+1830 was first discovered in 2021 from Gaia and SDSS data as a candidate white dwarf. A first spectral analysis was published in 2020, identifying it as a DZ white dwarf. In 2021 observations with the Gran Telescopio Canarias were published. The white dwarf is massive and has a mass of 1.00 ± 0.02 M. The cooling age was determined to be 9.5±0.2 Gyrs and the total age is 9.7±0.2 Gyrs. A more recent work found a higher temperature and younger cooling age of about 6.4 Gyrs. The researchers detected sodium, lithium and weak calcium absorption. The researchers also detected infrared excess, indicative of a debris disk, around this white dwarf. The disk is inclined by 70°, has an inner disk temperature of 1,500 K and an outer disk temperature of 500 K. In the past WD 2317+1830 had a mass of 4.8 ± 0.2 M and was likely a B-type star.

See also

References

  1. ^ Tremblay, P. -E.; Hollands, M. A.; Gentile Fusillo, N. P.; McCleery, J.; Izquierdo, P.; Gänsicke, B. T.; Cukanovaite, E.; Koester, D.; Brown, W. R.; Charpinet, S.; Cunningham, T.; Farihi, J.; Giammichele, N.; van Grootel, V.; Hermes, J. J. (2020-09-01). "Gaia white dwarfs within 40 pc - I. Spectroscopic observations of new candidates". Monthly Notices of the Royal Astronomical Society. 497 (1): 130–145. arXiv:2006.00965. Bibcode:2020MNRAS.497..130T. doi:10.1093/mnras/staa1892. ISSN 0035-8711.
  2. ^ Brown, A. G. A.; et al. (Gaia collaboration) (2021). "Gaia Early Data Release 3: Summary of the contents and survey properties". Astronomy & Astrophysics. 649: A1. arXiv:2012.01533. Bibcode:2021A&A...649A...1G. doi:10.1051/0004-6361/202039657. S2CID 227254300. (Erratum: doi:10.1051/0004-6361/202039657e). Gaia EDR3 record for this source at VizieR.
  3. ^ Hollands, Mark A.; Tremblay, Pier-Emmanuel; Gänsicke, Boris T.; Koester, Detlev; Gentile-Fusillo, Nicola Pietro (2021-05-01). "Alkali metals in white dwarf atmospheres as tracers of ancient planetary crusts". Nature Astronomy. 5 (5): 451–459. arXiv:2101.01225. Bibcode:2021NatAs...5..451H. doi:10.1038/s41550-020-01296-7. ISSN 2397-3366.
  4. ^ Bergeron, P.; Kilic, Mukremin; Blouin, Simon; Bédard, A.; Leggett, S. K.; Brown, Warren R. (2022-07-01). "On the Nature of Ultracool White Dwarfs: Not so Cool after All". The Astrophysical Journal. 934 (1): 36. arXiv:2206.03174. Bibcode:2022ApJ...934...36B. doi:10.3847/1538-4357/ac76c7. ISSN 0004-637X.
  5. ^ Kaiser, Benjamin C.; Clemens, J. Christopher; Blouin, Simon; Dennihy, Erik; Dufour, Patrick; Hegedus, Ryan J.; Reding, Joshua S. (2024-12-02). "The Origins of Lithium Enhancement in Polluted White Dwarfs". arXiv:2412.01878 .
  6. University of Warwick. "Vaporised crusts of Earth-like planets found in dying stars". warwick.ac.uk. Retrieved 2024-09-16.
  7. Putirka, Keith D.; Xu, Siyi (2021-11-01). "Polluted white dwarfs reveal exotic mantle rock types on exoplanets in our solar neighborhood". Nature Communications. 12 (1): 6168. arXiv:2111.03124. Bibcode:2021NatCo..12.6168P. doi:10.1038/s41467-021-26403-8. ISSN 2041-1723. PMC 8563750. PMID 34728614.
  8. info@noirlab.edu. "Rocky Exoplanets Are Even Stranger Than We Thought - A new astrogeology study suggests that most nearby rocky exoplanets are quite unlike anything in our Solar System". www.noirlab.edu. Retrieved 2024-09-16.
  9. Gentile Fusillo, N. P.; Tremblay, P. -E.; Cukanovaite, E.; Vorontseva, A.; Lallement, R.; Hollands, M.; Gänsicke, B. T.; Burdge, K. B.; McCleery, J.; Jordan, S. (2021-12-01). "A catalogue of white dwarfs in Gaia EDR3". Monthly Notices of the Royal Astronomical Society. 508 (3): 3877–3896. arXiv:2106.07669. Bibcode:2021MNRAS.508.3877G. doi:10.1093/mnras/stab2672. ISSN 0035-8711.
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