Intense pressurised conditions of Earth’s outer core are recreated in a LAB by firing two lasers at a sample of iron the width of a human hair
- Iron normally has a cubic form, but becomes closer packed with more pressure
- Experts from SLAC wanted to see how iron would behave in extreme conditions
- They found it assumes another form to allow it to cope with the pressure
- This process — called ‘twinning’ — can be seen in other minerals, like quartz
- Iron is much stronger after twinning that had been expected, the team said
At the extreme pressures found at the bottom of the Earth’s outer core, iron assumes a stronger form to cope with the stress in a process called ‘twinning’.
This is the conclusion of a study by researchers from the SLAC National Accelerator Laboratory who recreated the pressures of the core in the laboratory.
They did this by shining two lasers at a sample of iron the width of a human hair. The first created a shock wave that fleetingly heated and compressed the metal.
The second laser — part of SLAC’s Linac Coherent Light Source — enabled the team to probe the effect on the atomic structure of the iron within a billionth of a second.
At the extreme pressures found at the bottom of the Earth’s outer core (shown in the above artistic cutaway), iron assumes a stronger form to cope with the stress in a process called ‘twinning’. This is the conclusion of a study by researchers from the SLAC National Accelerator Laboratory who recreated the pressures of the core in the laboratory
Much of the iron you might encounter out and about — whether for example in buildings, machinery, Victorian lampposts, etc. — has a structure that crystallographers would refer to as ‘body-centred cubic’.
This means that the crystal lattice is arranged into a pattern of nanoscopic cubes, with iron atoms at each cube’s centre, as well as each of the eight corners.
When iron is subjected to higher pressures, however, this structure changes — taking, above 10 gigapascals, a hexagonal form that allows the atoms to pack together more closely.
In their study, paper author and geologist Arianna Gleason of SLAC and her colleagues wanted to see what would happen to the hexagonal close-packed form of iron if you continued to pile on the pressure up to that found in the Earth core.
‘We didn’t quite make inner core conditions, but we achieved the conditions of the outer core of the planet — which is really remarkable,’ said Professor Gleason.
The team were unsure how iron would respond to such extreme conditions — equivalent to some 360 million times the pressure at the Earth’s surface and as hot as surface of the Sun — as no-one has previously been able to observe such.
It turns out that iron undergoes another structural transition, much like the one from a cubic to a hexagonal form it experiences at much lower pressures.
‘As we continue to push it, the iron doesn’t know what to do with this extra stress,’ Professor Gleason explained.
She continued: ‘It needs to relieve that stress, so it tries to find the most efficient mechanism to do that.’
The coping mechanism that iron resorts to — twinning — sees the arrangement of atoms shunted to the side, rotating all the hexagonal prisms by nearly 90 degrees.
Twinning is a common pressure response in various minerals and metals, including calcite, quartz, titanium and zirconium.
‘Twinning allows iron to be incredibly strong — stronger than we first thought — before it starts to flow plastically on much longer time scales [than it would have otherwise,’ Professor Gleason said.
‘As we continue to push it, the iron doesn’t know what to do with this extra stress,’ Professor Gleason explained. ‘It needs to relieve that stress, so it tries to find the most efficient mechanism to do that.’ The coping mechanism that iron resorts to — twinning — sees the arrangement of atoms shunted to the side, rotating the hexagonal prisms by nearly 90°
‘Now we can give a thumbs up, thumbs down on some of the physics models for really fundamental deformation mechanisms,’ said Professor Gleason.
‘That helps to build up some of the predictive capability we’re lacking for modelling how materials respond at extreme conditions.’
Alongside this, the team explained, the same methods could be applied to better understand how other materials behave under extreme conditions.
Prior to their experiments, the researchers were unsure if iron would respond too fast for them to measure or too slow for them to ever see.
‘The fact that the twinning happens on the time scale that we can measure it as an important result in itself,’ explained paper author and geophysicist Sébastien Merkel of the University of Lille, France.
Twinning is a common pressure response in various minerals and metals, including calcite, quartz, titanium and zirconium. Pictured: a twinned crystal of quartz
‘The future is bright now that we’ve developed a way to make these measurements,’ added Professor Gleason, noting as well that recent upgrades to the Linac Coherent Light Source will allow materials to be studied at higher X-ray energies.
This, she explained, will enable studied of ‘thicker alloys and materials that have lower symmetry and more complex X-ray fingerprints’ — while also allowing larger samples to be observed, permitting a more comprehensive look at iron’s behaviour.
Furthermore, Gleason said, ‘we’re going to get more powerful optical lasers with the approval to proceed with a new flagship petawatt laser facility.
‘That’ll make future work even more exciting because we’ll be able to get to the Earth’s inner core conditions without any problem,’ she concluded.
The full findings of the study were published in the journal Physical Review Letters.
EARTH’S LIQUID IRON CORE CREATES THE MAGNETIC FIELD
Our planet’s magnetic field is believed to be generated deep down in the Earth’s core.
Nobody has ever journeyed to the centre of the Earth, but by studying shockwaves from earthquakes, physicists have been able to work out its likely structure.
At the heart of the Earth is a solid inner core, two thirds of the size of the moon, made mainly of iron.
At 5,700°C, this iron is as hot as the Sun’s surface, but the crushing pressure caused by gravity prevents it from becoming liquid.
Surrounding this is the outer core there is a 1,242 mile (2,000 km) thick layer of iron, nickel, and small quantities of other metals.
The metal here is fluid, because of the lower pressure than the inner core.
Differences in temperature, pressure and composition in the outer core cause convection currents in the molten metal as cool, dense matter sinks and warm matter rises.
The ‘Coriolis’ force, caused by the Earth’s spin, also causes swirling whirlpools.
This flow of liquid iron generates electric currents, which in turn create magnetic fields.
Charged metals passing through these fields go on to create electric currents of their own, and so the cycle continues.
This self-sustaining loop is known as the geodynamo.
The spiralling caused by the Coriolis force means the separate magnetic fields are roughly aligned in the same direction, their combined effect adding up to produce one vast magnetic field engulfing the planet.
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