Scientists Think Water Lurks Far Beneath Earth's Surface

According to new research, scientists think that water may lurk far beneath the Earth's surface; 250 miles beneath the surface, to be exact, Yahoo reports.

Studies show that approximately 250 miles below the Earth's surface, the mantle of the Earth meets the crust. Scientists are now convinced that below the "transition zone," decomposed and unstable brucite causes water molecules to run towards the surface of the planet.

What exactly is brucite? According to Web Mineral, brucite is an irregular-shaped, transparent crystal made up of fibers, typically 50 percent water and 50 percent magnesium oxide. They are typically yellow, white, blue, gray, or gray-blue in color.

What the study shows is that when brucite decomposes, it turns into a "stable, 3D structure." What this means for scientists is that water is lurking further beneath the Earth's surface than previously thought.

A lecturer in computational physics at the University of Edinburgh in Scotland and co-author Andreas Hermann was not expecting this result.

"[This finding] was not entirely expected."[That's] because people have studied this material for decades and nobody ever thought of looking whether there would be another phase before it eventually fell apart."
Previously, scientists believed that brucite remains stable down to directly above the mantle, which is approximately 155 miles beneath the Earth's surface. Brucite, if pressured enough, would crumble. Scientists are still unsure how much water the brucite will hold, or the amount of the substance in the mantle, but they were able to determine the elasticity of the brucite while under such pressures as in the mantle.
"We create thousands of structures, optimize them all and do calculations accurate enough that if something stands out as more stable than something else, we can reliably say that it is so."
It has been estimated that the mantle holds as much as all of the oceans on this Earth combined. According to scientists, the material that this deep water beneath the earth holds, is very important for the movement of water-containing minerals to the Earth's surface, which makes it's way to the surface through volcanic activity.

Water contains lubrication, which is needed for the rocks and minerals to move by each other during volcanic activity. Hermann explained that some rocks simply dissolve, which also helps with the rock movement. If our planet didn't have this deep reservoir of water, our Earth's geologic atmosphere would come to a complete halt, which would be catastrophic.

Water lurks deep within the Earth's mantle, according to a recent study.
[Image by Shutterstock]

Hermann is very satisfied with the most recent findings regarding the deep Earth. He said that if they would have settled on the research that they originally had, they wouldn't have ever found out these new, very important details.

In 2014, studies conducted by researchers from the University of New Mexico and Northwestern University used synthesized ringwoodite to test the conditions of the Earth at 400 miles deep, Northwestern Now reports.

University of New Mexico's Northwestern geophysicist, Steve Jacobsen, has been creating synthetic ringwoodite for years to test the Earth's interior composition.

"The ringwoodite is like a sponge, soaking up water. There is something very special about the crystal structure of ringwoodite that allows it to attract hydrogen and trap water. This mineral can contain a lot of water under conditions of the deep mantle."
A 2014 study uses Ringwoodite to test the Earth's Mantle composition.
[Image by Shutterstock]

Jacobsen determined that by exposing the synthesized ringwoodite to the conditions of 400 miles below the Earth's surface, that it forms a partial melt. This was the same result as Brandon Schmandt had when he used seismic waves to observe the deep Earth.

"Seismic data from the USArray are giving us a clearer picture than ever before of the Earth's internal structure beneath North America. The melting we see appears to be driven by subduction -- the downwelling of mantle material from the surface."
The melting detected is known as dehydration melting,
"When a rock with a lot of H2O moves from the transition zone to the lower mantle it needs to get rid of the H2O somehow, so it melts a little bit. This is called dehydration melting."
Every year, we come closer and closer to finding out more intriguing information about our planet. The Earth is truly remarkable.

[Featured Image by Shutterstock]