Science

Scientists Confirm the Existence of an Ocean Deep Inside the Earth

By | Jun 14, 2014 09:05 AM EDT
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Sample of a ringwoodite crystal thought to hold much of the Earth's sub-surface water

Sample of a ringwoodite crystal thought to hold much of the Earth's sub-surface water

The world's largest ocean lies 400 to 600 kilometers beneath our feet. But all that water's trapped inside a special type of rock called "ringwoodite."

Scientists have long suspected that a so-called "transition zone" in the Earth's mantle could contain water trapped in rare minerals. That transition zone lies between the upper and lower mantle layers which are 410 kilometers to 660 kilometers below the surface.

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Direct evidence for this water has now been confirmed for the first time.

Scientists in the US conducted experiments on ringwoodite, a water-rich mineral, by analyzing seismic waves travelling through the mantle beneath the US. They discovered that downward-flowing mantle material was melting as it crossed the boundary between the transition zone and the lower mantle layer. 

This led researchers to conclude there has to be this water in the transition zone because of this melting. Melting is a way of getting rid of water, which is unstable under conditions in the Earth's lower mantle, said the researchers.

A new study published a few days ago in the journal Science said the transition zone "... can hold a lot of water, and could potentially have the same amount of H2O (water) as all the world's oceans."

Most of this water in this sub-surface "ocean" is trapped inside ringwoodite. This is a rare type of mineral that forms from a mineral called olivine under very high pressures and temperatures such as those present in the mantle's transition zone.

Olivine, also called peridot or chrysolite, is a magnesium iron silicate mineral common in the Earth's sub-surface.

Sceintific studies have shown that ringwoodite can contain water. This water isn't present as liquid, ice or vapor, however.

Instead, the water is trapped in the ringwoodite's molecular structure as hydroxide ions or bonded oxygen and hydrogen atoms.

Scientists have previously used many approaches to look for evidence of Earth's interior water reservoir. This is the first time scientists have searched for clues of the reservoir by focusing on the potential water-induced melting at the bottom of the transition zone.

The new findings will help scientists better understand Earth's water cycle. Scientists know that the surface water we now have comes from degassing of molten rock. It came from the original rock ingredients in the Earth. The question now facing scientists is how much water is still inside the Earth today relative to the surface.

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