Early in the thread the idea of mining rare earth minerals and such was brought up as a future aspect of space travel, which makes some sense.
Mercury Could Have A Layer of Diamonds 11 Miles Thick Beneath the Surface
Someone is bound to find a way to do it at some point.
Mercury Could Have A Layer of Diamonds 11 Miles Thick Beneath the Surface
A bi-disciplinary scientific study has revealed the likely presence of a layer of diamonds 11 miles thick at the boundary layer of Mercury’s core and mantle.
It was a remarkable finding, and came from what is the least understood planet in the solar system, despite being one of the closest to Earth.
Diamonds are forever—a girl’s best friend—but more importantly for science, they are pure carbon. Carbon is an awfully common chemical to find in the solar system, and many sources can become diamonds under the correct pressures and temperatures.
When viewed by the MESSENGER spacecraft from 2011 to 2015, Mercury appears exceptionally grey due to the high content of graphite on the planet. This mineral, responsible for our pencil tips among other things, is another form of pure carbon, and was a clue for the researchers that diamonds might be richly present beneath the surface.
“We know there’s a lot of carbon in the form of graphite on the surface of Mercury, but there are very few studies about the inside of the planet,” said Yanhao Lin, a staff scientist at the Center for High Pressure Science and Technology Advanced Research in Beijing and co-author of the study, which appeared in June in the journal Nature Communications.
In their study, the researchers placed graphite in a special pressure machine along with a smattering of elements believed to be rich in Mercury’s mantle layer, including silicon, titanium, magnesium, and aluminum.
They subjected the mixture to 70,000 times the pressure of Earth at sea level, and 2,000° Celcius (3,630 degrees Fahrenheit). These are the conditions believed to have been present at the core-mantle boundary layer while Mercury was forming 4.5 billion years ago when it coalesced from clouds of gas and dust.
Electron microscopy revealed that the mixture melted and the graphite had turned into diamond crystal.
By examining data from the MESSENGER mission about the mineral composition and depth of Mercury’s crust, mantle, and planetary core under the context of their experiment, the authors estimate the layer of diamonds should be about 11 miles thick.
It was a remarkable finding, and came from what is the least understood planet in the solar system, despite being one of the closest to Earth.
Diamonds are forever—a girl’s best friend—but more importantly for science, they are pure carbon. Carbon is an awfully common chemical to find in the solar system, and many sources can become diamonds under the correct pressures and temperatures.
When viewed by the MESSENGER spacecraft from 2011 to 2015, Mercury appears exceptionally grey due to the high content of graphite on the planet. This mineral, responsible for our pencil tips among other things, is another form of pure carbon, and was a clue for the researchers that diamonds might be richly present beneath the surface.
“We know there’s a lot of carbon in the form of graphite on the surface of Mercury, but there are very few studies about the inside of the planet,” said Yanhao Lin, a staff scientist at the Center for High Pressure Science and Technology Advanced Research in Beijing and co-author of the study, which appeared in June in the journal Nature Communications.
In their study, the researchers placed graphite in a special pressure machine along with a smattering of elements believed to be rich in Mercury’s mantle layer, including silicon, titanium, magnesium, and aluminum.
They subjected the mixture to 70,000 times the pressure of Earth at sea level, and 2,000° Celcius (3,630 degrees Fahrenheit). These are the conditions believed to have been present at the core-mantle boundary layer while Mercury was forming 4.5 billion years ago when it coalesced from clouds of gas and dust.
Electron microscopy revealed that the mixture melted and the graphite had turned into diamond crystal.
By examining data from the MESSENGER mission about the mineral composition and depth of Mercury’s crust, mantle, and planetary core under the context of their experiment, the authors estimate the layer of diamonds should be about 11 miles thick.
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