Total destruction of an entire planet sounds like the plot of a science fiction movie, but a team of astronomers has found evidence that this may have happened in an ancient cluster of stars at the edge of the Milky Way galaxy.
With several telescopes, including NASA’s Chandra X-ray Observatory, researchers have found evidence that a white dwarf star, the dense core of a star like the Sun that has run out of nuclear fuel, may have ripped apart a planet as it came too close.
But how could a white dwarf star, which is only about the size of the Earth, be responsible for such an extreme act?
The answer is gravity.
When a star reaches its white dwarf stage, nearly all of the material from the star is packed inside a radius of one hundredth that of the original star. This means that, for close encounters, the gravitational pull of the star and the associated tides, caused by the difference in gravity’s pull on the near and far sides of the planet, are greatly enhanced.
For example, the gravity at the surface of a white dwarf is over ten thousand times higher than the gravity at the surface of the Sun.
INTEGRAL and Chandra Composite
White dwarf star Sirius B. Credit: NASA
Researchers used the European Space Agency’s INTErnational Gamma-Ray Astrophysics Laboratory (INTEGRAL) to discover a new X-ray source near the center of the globular cluster NGC 6388.
Optical observations hinted that an intermediate-mass black hole with a mass equal to several hundred Suns or more resides at the center of NGC 6388. The X-ray detection by INTEGRAL then raised the intriguing possibility that the X-rays were produced by hot gas swirling towards an intermediate-mass black hole.
In a follow-up X-ray observation, Chandra’s excellent X-ray vision enabled the astronomers to determine that the X-rays from NGC 6388 were not coming from the putative black hole at the center of the cluster, but instead from a location slightly off to one side.
A new composite image shows NGC 6388 with X-rays detected by Chandra in pink and visible light from the Hubble Space Telescope in red, green, and blue, with many of the stars appearing to be orange or white. Overlapping X-ray sources and stars near the center of the cluster also cause the image to appear white.
With the central black hole ruled out as the potential X-ray source, the hunt continued for clues about the actual source in NGC 6388. The source was monitored with the X-ray telescope on board NASA’s Swift Gamma Ray Burst mission for about 200 days after the discovery by INTEGRAL.
Theoretical Disruption Models
The source became dimmer during the period of Swift observations. The rate at which the X-ray brightness dropped agrees with theoretical models of a disruption of a planet by the gravitational tidal forces of a white dwarf.
In these models, a planet is first pulled away from its parent star by the gravity of the dense concentration of stars in a globular cluster. When such a planet passes too close to a white dwarf, it can be torn apart by the intense tidal forces of the white dwarf.
The planetary debris is then heated and glows in X-rays as it falls onto the white dwarf. The observed amount of X-rays emitted at different energies agrees with expectations for a tidal disruption event.
The researchers estimate that the destroyed planet would have contained about a third of the mass of Earth, while the white dwarf has about 1.4 times the Sun’s mass.
While the case for the tidal disruption of a planet is not iron-clad, the argument for it was strengthened when astronomers used data from multiple telescopes to help eliminate other possible explanations for the detected X-rays.
For example, the source does not show some of the distinctive features of a binary containing a neutron star, such as pulsations or rapid X-ray bursts. Also, the source is much too faint in radio waves to be part of a binary system with a stellar-mass black hole.
Reference: M. Del Santo1, A. A. Nucita, Lodato5, L. Mann, F. De Paolis, J. Farihi, G. De Cesare and A. Segreto. The puzzling source IGR J17361-4441 in NGC 6388: a possible planetary tidal disruption event. MNRAS (October 11, 2014) 444 (1): 93-101. doi: 10.1093/mnras/stu1436
