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Hexaferrum, physicists reproduce the material in the center of the Earth

A research team has synthesized hexaferrum, a key material to help better understand the Earth's core.

August 19 2023
Gianluca RiccioGianluca Riccio
⚪ 3 minutes
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Agnes Dewaele and his team of researchers fromUniversity of Paris-Saclay they used a diamond anvil to synthesize hexaferrum, a form of iron believed to exist in the Earth's core. This discovery not only sheds light on the characteristics of our planet but also opens up new avenues for future research.

Viaggio al centro della Terra

The Earth's core has always been a mystery. How can we study something that lies thousands of kilometers under our feet? The answer may surprise you: with a diamond.

Agnes Dewaele and his team used a diamond anvil to compress the iron into a shape called hexaferrum or epsilon iron (ϵ-Fe). This form of iron is stable only at very high pressures, similar to those found in the Earth's core. But why is it so important? Because the hexaferrum could hold the key to understanding directional variations in the Earth's core, a phenomenon known as anisotropy.

The research was published in the journal Physical Review Letters, and I link it here.

Hexaferrum, the challenge of synthesis

Creating the hexaferrum was no easy task. The atmospheric pressure we are used to is very different from that in the earth's core. But, as the saying goes, want is power. Using the diamond anvil and heat, the team managed to create high-pressure conditions, if only for a short amount of time.

The article continues after the related links

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The real obstacle was transforming iron, in its form called ferrite or alpha iron, into hexaferrum. In the past, similar attempts had resulted in the formation of small crystals, making detailed analysis difficult. But Dewaele and his colleagues did not give up. They took a stepwise approach, increasing pressure and temperature in a controlled way, until they achieved the coveted hexaferrum shape.

Hexaferrum
An illustration showing the synthesis of hexaferrum.

A step forward

Thanks to this research we now know much more about the Earth's core. For example, we know that the elasticity of the hexaferrum is direction dependent, meaning that waves propagate faster along a specific axis. This discovery could explain how seismic waves travel across the planet.

But that's not all: French research could also help us better understand the extreme conditions at the center of the Earth. As if to say: we may never have the opportunity to get there directly (sorry, Jules Verne), but we can certainly explore its mysteries through the research and dedication of passionate scientists.

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