PSR J1719−1438 b

PSR J1719−1438 b

Artist's conception of PSR J1719-14 b
Discovery
Discovered by	Matthew Bailes et al.
Discovery site	Melbourne, Australia
Discovery date	August 25, 2011
Detection method	Pulsar timing
Orbital characteristics
Semi-major axis	0.004 AU (600,000 km)
Eccentricity	< 0.06
Orbital period (sidereal)	0.090706293 d 2.176951032 h
Time of periastron	2,455,235.51652439
Star	PSR J1719−1438
Physical characteristics
Mean radius	≤0.4 RJ ≤4 R🜨
Mass	~1.02 MJ (~330 ME)
Mean density	≥23 g cm−3

PSR J1719−1438 b is an extrasolar planet that was discovered on August 25, 2011, in orbit around PSR J1719−1438, a millisecond pulsar. The pulsar planet is most likely composed largely of crystalline carbon but with a density far greater than diamond. PSR J1719-1438 b orbits so closely to its host star that its orbit would fit inside the Sun. The existence of such carbon planets had been theoretically postulated.

Observational history

PSR J1719−1438 was first observed in 2009 by a team headed by Matthew Bailes of Swinburne University of Technology in Melbourne, Australia. The orbiting planet was published in the journal Science on August 25, 2011. The planet was confirmed through pulsar timing, in which small modulations detected in the highly regular pulsar signature are measured and extrapolated. Observatories in Britain, Hawaii, and Australia were used to confirm these observations.

Host star

Main article: PSR J1719−1438

PSR J1719−1438 is a pulsar some 4,000 light-years (1,200 parsecs) away from Earth in the Serpens Cauda constellation, approximately one minute from the border with Ophiuchus. The pulsar completes more than 10,000 rotations a minute. It is approximately 12 miles (19 kilometers) across but with 1.4 solar masses.

Characteristics

PSR J1719−1438 b was, at the time of its August 25, 2011, discovery, the densest planet ever discovered, at nearly 20 times the density of Jupiter (about 23 times the density of water). It is slightly more massive than Jupiter. It is thought to be composed of oxygen and carbon (as opposed to hydrogen and helium, the main components of gas giants like Jupiter and Saturn).

The oxygen is most likely on the surface of the planet, with increasingly higher quantities of carbon deeper inside the planet. The intense pressure acting upon the planet suggests that the carbon is crystallized, much like diamond is.

PSR J1719−1438 b orbits its host star with a period of 2.17 hours and at a distance of 0.89 solar radii (619,173 km or 384,736 mi).

Formation

It is highly unlikely that this planet would have formed before its parent pulsar, as the resulting supernova would destroy any nearby planets. It has been proposed that PSR J1719−1438 b is not a planet but a star. Specifically, PSR J1719−1438 b was a yellow dwarf star similar to the Sun in a binary with PSR J1719−1438, a higher-mass star. PSR J1719−1438 swelled up to become a red supergiant, but the yellow dwarf star survived the supernova. Billions of years later, PSR J1719−1438 b became a red giant and then a white dwarf. The gravity from the pulsar stole hydrogen and helium, and the remaining carbon crystallized, forming the diamond planet.

See also

• WASP-12b, a carbon planet
• BPM 37093, a carbon star
• EF Eridani, a star system with a compact star and a degraded planetary-mass former star

Further reading

• Bailes, M.; Bates, S. D.; Bhalerao, V.; Bhat, N. D. R.; Burgay, M.; Burke-Spolaor, S.; d'Amico, N.; Johnston, S.; Keith, M. J.; et al. (2011). "Transformation of a Star into a Planet in a Millisecond Pulsar Binary" (PDF). Science. 333 (6050): 1717–20. arXiv:1108.5201. Bibcode:2011Sci...333.1717B. doi:10.1126/science.1208890. PMID 21868629. S2CID 206535504.
• "A Planet made of Diamond" (Press release). Max Planck Institute for Radio Astronomy. August 25, 2011. Archived from the original on September 14, 2011. Retrieved August 26, 2011.
• Correa, Alfredo A.; Bonev, Stanimir A.; Galli, Giulia (2006). "Carbon under extreme conditions: Phase boundaries and electronic properties from first-principles theory". Proceedings of the National Academy of Sciences. 103 (5): 1204–8. Bibcode:2006PNAS..103.1204C. doi:10.1073/pnas.0510489103. PMC 1345714. PMID 16432191.