Mystery solved: Mercury has a solid heart
Mercury, the smallest planet in our solar system and closest to the sun, doesn’t resemble Earth much on the outside, but deep inside is a different story. It has been known for a long time now that Mercury has a liquid metallic outer core, as Earth does, but planetary scientists didn’t know if Mercury was also like Earth in having a solid inner core. Thanks to new analysis of data from the MESSENGER mission, it turns out that Mercury’s core is solid. It’s also about the same size as Earth’s inner core, even though Mercury itself is much smaller than Earth.
According to Antonio Genova at Sapienza University of Rome:
Mercury’s interior is still active, due to the molten core that powers the planet’s weak magnetic field, relative to Earth’s. Mercury’s interior has cooled more rapidly than our planet’s. Mercury may help us predict how Earth’s magnetic field will change as the core cools.
Genova led the research project while at NASA’s Goddard Space Flight Center in Greenbelt, Maryland.
Mercury has been considered a bit of an oddball compared to the other rocky planets in the solar system, since its core fills nearly 85 percent of the volume of the entire planet – much more than the cores of any of the other rocky planets, including Earth. Just why that is, is still unknown.
But now it seems that another question – whether Mercury’s inner core is solid or liquid – has finally been answered. So how did Genova and his team do it?
They used data from several observations of Mercury from the MESSENGER spacecraft, which orbited the planet from 2011 to 2015. The planet’s spin and gravity provided the clues needed to figure out the mystery of the planet’s inner core. The researchers searched for gravity anomalies – regions where there is an increase or decrease in mass – using radio data from MESSENGER. Similar gravity anomalies have been found on our own moon, as an example.
Mercury rotates much more slowly than Earth does – one day on Mercury is equal to about 58 Earth days – and previously observed variations were enough to determine that the planet had a molten outer core. But this was not enough to figure out the nature of the inner core. That’s where the gravitational analysis came in. By looking at how the spacecraft accelerated under the influence of Mercury’s gravity, especially during the lowest-altitude orbits, scientists could take more accurate measurements of the innermost part of the core.
The results showed that Mercury must have a large, solid inner iron core, estimated to be about 1,260 miles (2,000 km) wide. This means it makes up about half of Mercury’s entire core, which is about 2,440 miles (4,000 km) wide. Earth’s solid inner core is about 1,500 miles (2,400 km) across, taking up a little more than a third of this planet’s entire core.
It took many different kinds of data to achieve this result, as Erwan Mazarico, a planetary scientist at Goddard and co-author of the new study, explained:
As Genova also noted:
Such an advanced solidification of the core demonstrates how the deepest part of Mercury is similar to that of the Earth: understanding the nature and evolution of the internal structure of other planets is essential to enhance our knowledge of Earth’s future. Every new bit of information about our solar system helps us understand the larger universe.
These new findings about Mercury are not only of great scientific interest, but also highlight how essential robotic missions are in the exploration of the solar system. The kind of data taken by MESSENGER would not have been possible from Earth – only by getting close to the planet’s surface were scientists able to find out what Mercury is like in its innermost core, and discover that it has a solid heart.
Bottom line: Learning about Mercury’s inner core will help scientists gain more knowledge about not only how Mercury formed and evolved, but about other rocky planets in our solar system as well – and even rocky exoplanets orbiting distant stars.