Magnetic mystery of Earth's early core explained

Magnetic mystery of Earth's early core explained

Magnetic mystery of Earth's early core explained

Geophysicists call it the “new core paradox.” They can’t quite explain how ancient Earth could have sustained a magnetic field billions of years ago, as it was cooling from its fiery birth.

Now, two scientists have independently proposed different ways to solve the paradox. Each relies on minerals crystallising out of the molten Earth, a process that would have generated a magnetic field by churning the young planet’s iron core. The difference between the two explanations is in which mineral does the crystallising.

Silicon dioxide is the choice of Kei Hirose, a geophysicist at the Tokyo Institute of Technology who runs high-pressure experiments to simulate conditions deep within the Earth.

“I’m very confident in this,” he reported on December 17 at a meeting of the American Geophysical Union in San Francisco, California. But David Stevenson, a geophysicist at the California Institute of Technology in Pasadena, says that magnesium oxide — not silicon dioxide — is the key to solving the problem.

In an unpublished work, David proposes that magnesium oxide, settling out of the molten early Earth, could have set up the buoyancy differences that would drive an ancient geodynamics. And new laboratory experiments appear to bear him out.

Battle of the oxides

The core paradox arose in 2012, when several research teams reported that Earth’s core loses heat at a faster rate than once thought. More heat conducting away from the core means less heat available to churn the core’s liquid.

That’s important because some studies suggest that Earth could have had a magnetic field more than four  billion years ago — less than half a billion years after it coalesced from fiery debris swirling around the newborn Sun. “We need a dynamo more or less continuously,” said Peter Driscoll, a geophysicist at the Carnegie Institution for Science in Washington DC, at the meeting.

In his Tokyo laboratory, Kei put different combinations of iron, silicon and oxygen into a diamond anvil cell and squeezed them to produce extraordinarily high pressures and temperatures — sometimes above 4,000 degrees Celsius — to simulate the hellish conditions of Earth’s interior. He found that silicon and oxygen crystallised out together as silicon dioxide whenever both were present.

When silicon dioxide precipitated deep inside the early Earth, it would have made the remaining molten material buoyant enough to continue rising, thus setting up the churning motion needed to sustain the dynamo, Kei reported. “As far as I know, this is the most feasible mechanism to drive the geodynamics,” he said.

David, by contrast, plumps for magnesium, saying that it “makes much more sense” than silicon dioxide because magnesium oxide would precipitate out of a molten Earth first.” “Kei,” he says, “is telling you something that can happen, not what did happen.”

And now there are laboratory experiments supporting the magnesium oxide idea. James Badro, a geophysicist at the Institut de Physique du Globe in Paris, has led high-pressure, high-temperature studies that involve adding magnesium into a mix of chemicals to simulate the early Earth.

At the meeting, he reported that magnesium oxide crystallises out — and in doing so produces a large amount of gravitational energy, more than enough to generate a strong magnetic field very early in the planet’s history. “Dave Stevenson was right!!” read James’ concluding slide.

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