Move over, Lucy: Researchers say Saturn, Jupiter, Neptune and Uranus may also be in the sky, with diamonds.
The atmospheres of these gas-ball planets have the perfect temperature and pressure conditions to host carbon in the form of diamond, say Mona Delitsky of California Specialty Engineering in Pasadena, California, and Kevin Baines of the University of Wisconsin-Madison.
Their research was presented Wednesday at the American Astronomical Society Division for Planetary Sciences conference in Denver.
Previous research had implicated Neptune and Uranus in the hypothetical space diamond business, but Delitsky and Baines performed calculations suggesting that Saturn and Jupiter may host sparkly treasure, too.
“They would be diamonds like we have here, except they would probably be a little more dense,” Delitsky said. “They would probably be the same translucent gem that we’re all familiar with.”
This is all based on theory and modeling, of course. No spacecraft has actually detected diamonds, photographed them or collected them.
But the theory didn’t come entirely out of thin air.
The phases of carbon
You may remember from chemistry class that substances enter different physical states depending on temperature and pressure. For instance, water becomes ice at 32 degrees Fahrenheit and vapor at 212 F, at typical pressures on the surface of Earth.
Carbon has more than one form that it takes as a solid. At low temperatures and pressures, carbon is stable as graphite, that soft substance in your pencils. Much more extreme conditions are needed to turn carbon into diamonds, chemically identical to graphite but exquisitely strong, with atoms tightly bound to one another.
Scientists know that carbon in the form of methane is found in the atmospheres of Saturn, Jupiter, Neptune and Uranus — especially in the latter two. A methane molecule consists of one carbon atom surrounded by four hydrogen atoms.
Marvin Ross pointed out in a 1981 Nature study that Uranus and Neptune have deep interiors rich in methane, which would be converted into elemental carbon at high temperatures. The extreme temperature and pressure conditions would allow carbon to form diamond.
More recently, shock-wave experiments, simulating extreme conditions on other planets, have more clearly shown the temperature and pressure boundaries between the various forms of carbon. Delitsky and Baines combined these latest insights with what is known about the temperatures and pressures in the interiors of the outer planets.
From lightning to diamonds
Studying the storm systems on Saturn, Baines noticed that there were patches in the atmosphere, where storm clouds had been, that were darker than regular clouds. He wanted to find out what material would have that effect.
The substance that fit the scenario the best was carbon in the form of soot, like the kind you see when you burn wood — likely as a result of lightning. The researchers published a study on this in 2009.
But what happens when these carbon particles sink into the deep interior of Saturn?
Planetary researcher Nadine Nettleman at the University of California, Santa Cruz, developed graphs of how temperature and pressure changes with altitude for Jupiter, Saturn, Uranus and Neptune. Delitsky and Baines used this data — much of which is unpublished — and compared it with the recent insights about conditions for forming diamond.