The remnants of a destroyed planet have been seen crashing into the core of a long-dead sun-like star known as a white dwarf, astronomers revealed.
These observations, made using the NASA Chandra X-ray Observatory, confirm decades of indirect evidence that debris from disintegrating planets are sent hurtling into these stellar remnants over the course of billions of years.
A white dwarf is what remains of a star like the sun, after it burns through its fuel and sheds its outer layers. Leaving just a dense core.
The planetary remnants were observed heating up to 1.8 million degrees Fahrenheit as they hit the surface of G 29-38, a variable white dwarf 44 light years from the Earth, experts from the University of Warwick in England, explained.
Lead author, Timothy Cunningham, told MailOnline that this is the fate that could be awaiting the planets, moons and asteroids in the solar system in a few billion years.
However, it isn’t a rapid process, and doesn’t start until after the Red Giant phase, where the star sheds its outer layers. He said that planetary bodies will be gradually scattered, and then drawn in over billions of years and once it is close enough to the star to be destroyed, it will form a disc that slowly ‘drop feeds’ material to the star.
‘Current estimates put the average lifetime of these disks at around 100,000 – a million years,’ Dr Cunningham told MailOnline, adding it ‘would vary a lot depending on the mass of the planetary body which is destroyed.’
Artist’s impression of a white dwarf, G29—38, accreting planetary material from a circumstellar debris disk. When the planetary material hits the white dwarf surface, a plasma is formed and cools via detectable X-ray emission
Researchers used X-rays to detect rocky and gaseous materials that had been left behind by the planetary system after its host star died.
They found that over time this debris gradually moves closer to the stellar remnant, until it is consumed within the surface of the star.
This happened billions of years after the formation of the planetary system, as it takes that long for a start to work through its elements, push off its outer layers and become a white dwarf – which is just the core of the sun-like origin star.
Most stars, and planetary systems, will end up like G 29-38, turning into a white dwarf, with over 300,000 discovered in the Milky Way alone.
Many are thought to be accreting the debris from planets and other objects that once orbited around them.
Astronomers have been using a process known as spectroscopy for the past few decades, looking at optical and ultraviolet wavelengths, to study white dwarfs.
This allowed them to measure the abundances of elements on the surface of the star, and work out from that the composition of the objects it came from.
These observations, made using the NASA Chandra X-ray Observatory, confirm decades of indirect evidence that debris from disintegrating planets are sent hurtling into these stellar remnants
For example, this could allow them to see the chemical remnants of rock and gas not native to the dead star – but not how it got there.
Astronomers have indirect evidence that they come from dead planets, but this is the first time the process has been witnessed directly.
The indirect evidence came from the fact 25-50 per cent of all white dwarfs contain heavy elements – such as iron, calcium and magnesium – in the atmosphere.
Dr Cunningham of the University of Warwick Department of Physics said this is the first time they’ve seen material entering the atmosphere of a white dwarf.
‘It is the first time we’ve been able to derive an accretion rate that doesn’t depend on detailed models of the white dwarf atmosphere. What’s quite remarkable is that it agrees extremely well with what’s been done before,’ he explained.
‘Previously, measurements of accretion rates have used spectroscopy and have been dependent on white dwarf models. These are numerical models that calculate how quickly an element sinks out of the atmosphere into the star, and that tells you how much is falling into the atmosphere as an accretion rate.
‘You can then work backwards and work out how much of an element was in the parent body, whether a planet, moon or asteroid.’
The material from planetary bodies are scattered through the system after the star ends its Red Giant phase – where outer layers are shed, leaving clouds of dust and gas in the system.
As these blocks of gas and dust, that remain from once fully formed planets, moons and asteroids, are pulled towards the star – they form a disc.
‘Once a planetary body gets close enough to the white dwarf to be destroyed (tidally-disrupted), in most instances this material will form a disk around the white dwarf that slowly “drip feeds” material on to the star,’ Dr Cunningham told MailOnline.
‘Current estimates put the average lifetime of these disks at around 100,000 – 1,000,000 years, but this would vary a lot depending on the mass of the planetary body which is destroyed.’
As material from planetary bodies is pulled into the star – at a high enough rate – it slams into the surface and forms something known as a ‘shock-heated plasma’.
This plasma has temperatures up to 1.8 million degrees Fahrenheit and it settles on the surface of the star – as it cools it emits X-rays that can be seen from Earth.
This high energy wavelength of light are created by very fast-moving electrons and are a key fingerprint of material raining down on black holes and neutron stars.
Detecting them is a challenging problem, as the small amount that reach the Earth can be lost among other bright sources of X-ray in the night sky.
Chandra, the space-based NASA x-ray observatory, is normally used to look at black holes, but can also pick up on less obvious sources of emissions.
With Chandra’s improved angular resolution over other telescopes the team could isolate the target star, G 29-38, from other X-ray sources.
Most stars, and planetary systems, will end up like G 29-38, turning into a white dwarf, with over 300,000 discovered in the Milky Way alone
This allowed them to view X-rays from an isolated white dwarf for the first time, and see the material entering the atmosphere of the star.
Dr Cunningham adds: ‘What’s really exciting about this result is that we’re working at a different wavelength, X-rays, and that allows us to probe a completely different type of physics.
‘This detection provides the first direct evidence that white dwarfs are currently accreting the remnants of old planetary systems.
‘Probing accretion in this way provides a new technique by which we can study these systems, offering a glimpse into the likely fate of the thousands of known exoplanetary systems, including our own Solar system.’
The findings have been published in the journal Nature.