Earth’s inner core holds the secrets to the planet’s past. But how can scientists analyse something that's impossible to see from the surface?
More than 5,000 kilometres beneath the surface is Earth’s inner core, a solid metallic ball that sits at the centre of our planet. Think of it as a time capsule – a fossilised record that takes us back into the deep past and tells us more about the planet’s evolution.
Not only can the inner core enlighten us about events that happened on Earth hundreds of millions to billions of years ago, it’s an ‘engine room’ integral to sustaining the planet’s magnetic field, which is what makes all life possible.
Developing new ways to study Earth’s innermost region can even help us learn more about other planets in our solar system.
Earth is like a thick, multi-layered cake and the inner core is the bottom layer. It’s the hardest layer to study because it’s located in the centremost region of Earth, under thousands of kilometres of dense rock. Much of what we know about Earth’s deep interior comes from data captured by an extensive network of seismometers – instruments used to record the motion of the ground – placed in all corners of the globe.
To learn more about the inner core, seismologists analyse seismic waves triggered by earthquakes. These waves, which originate from the energy created by earthquakes, penetrate and pass through the inner core. Seismic waves reveal many properties about the Earth’s interior. Different types of seismic waves give us different clues.
P-waves, which are more frequently observed by researchers, and J-waves, which are harder to detect, are types of seismic waves that pass through the inner core. Seismologists are particularly interested in detecting and analysing J-waves as they hold the key to understanding the state and composition of the inner core, which has been continually growing over millions of years.
Seismic waves speed up or slow down depending on the composition and texture of the material they travel through. By observing J-waves and analysing their speed, scientists can unlock clues about the inner core’s material, including whether it is liquid or crystallised, and how rigid it is.
However, detecting J-waves is difficult because of their weak signals–they are seemingly invisible when employing traditional seismometer observation methods. That’s why ANU researchers have developed an innovative new technique that measures them. They did this by using data from thousands of digital records from seismometers deployed across Earth’s surface.
The team then created a simulation using the southern hemisphere’s biggest supercomputer, located on the ANU campus, to determine the speeds at which the J-waves travel through Earth’s centre.
“Detecting J-waves is like finding a needle in a haystack,” Professor Hrvoje Tkalčić says.
“Although we detected J-waves in 2018, our new technique provides a much better estimate of their speed. It’s almost like looking at the same thing but through a much sharper lens.”
According to ANU seismologist Dr Thanh-Son Phạm, the ANU-developed technique to study J-waves is similar to how astrophysicists processed their geomagnetic records to produce the first-ever image of a black hole a few years ago.
By developing a new way to examine J-waves as they pierce the inner core, ANU researchers have confirmed that while the core is solid (a hypothesis first outlined in 1940), it is also softer than previously thought.
PhD student Thuany Costa de Lima, who works with Tkalčić and Phạm, says the best way to describe the inner core’s texture is “squishy”.
“Although it is difficult to answer why the inner core is squishy but solid, it could be because it experienced a complex solidification process at some point during Earth’s evolutionary timeline,” she says.
“Understanding how the material in the inner core is affected by high pressures and temperatures in the labs, combined with seismological measurements of J-wave speed, could prove game-changing in understanding the inner core’s structure and evolution.”
ANU seismologists, based at the Research School of Earth Sciences, are at the forefront of major discoveries shaping our understanding of Earth and how the world around us came to be.
Not long ago it was thought Earth’s structure comprised four distinct layers: the crust, the mantle, the outer core and the inner core. Thanks to a team of ANU researchers, including Tkalčić, Phạm and de Lima, we now know there’s a fifth layer referred to as the innermost inner core.
“The existence of an internal metallic ball within the inner core, known as the innermost inner core, was hypothesised about 20 years ago,” Phạm says.
“Earlier this year we provided another line of evidence to prove the hypothesis.”
While the work of ANU seismologists is helping other scientists study the evolution of Earth, their research is also helping us learn more about life beyond our world.
This includes developing new ways to study the deep interior of planets such as Mars.
“Our work opens up new avenues for further investigation of our planet’s deep interior and evolution, as well as the evolution of other planets in the solar system such as Mars, and the many moons,” Tkalčić says.
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