
Nitrogen Is In Liquid Metal Form Inside Earth's Core (eurekalert.org) 70
hackingbear writes: A team of scientists from China, the U.S., and U.K. successfully turned nitrogen, the dominant gas in Earth's atmosphere, into a metallic fluid by subjecting it to the extreme pressure and temperature conditions found deep inside the Earth and other planets. Their findings have been published in the journal Nature Communications .
"Our findings could inform the efforts to create forms of energetic nitrogen polymers as well as superconducting, metallic states of a sister diatomic molecule, hydrogen or H2, which could revolutionize the energy sector if reliably synthesized," according to team member Nicholas Holtgrewe. The project was funded by by the (U.S.) National Science Foundation, the (U.S.) Army Research Office, the National Natural Science Foundation of China, the Chinese Academy of Science, the British Council Researcher Links Program, and other sources. According to EurekAlert, "The researchers found that the temperature at which nitrogen transitions from insulating to metallic decreases as the pressure increases -- starting at about 1,180,000 times normal atmospheric pressure (120 gigapascals) and 2,720 degrees Celsius (3,000 kelvin)." "This means that, theoretically, nitrogen would remain in its diatomic state in the Earth's mantle but would disassociate into a fluid metal in or just above the core, which potentially has implications for our understanding of the planet's deep nitrogen cycle," said team member Sergey Lobanov.
"Our findings could inform the efforts to create forms of energetic nitrogen polymers as well as superconducting, metallic states of a sister diatomic molecule, hydrogen or H2, which could revolutionize the energy sector if reliably synthesized," according to team member Nicholas Holtgrewe. The project was funded by by the (U.S.) National Science Foundation, the (U.S.) Army Research Office, the National Natural Science Foundation of China, the Chinese Academy of Science, the British Council Researcher Links Program, and other sources. According to EurekAlert, "The researchers found that the temperature at which nitrogen transitions from insulating to metallic decreases as the pressure increases -- starting at about 1,180,000 times normal atmospheric pressure (120 gigapascals) and 2,720 degrees Celsius (3,000 kelvin)." "This means that, theoretically, nitrogen would remain in its diatomic state in the Earth's mantle but would disassociate into a fluid metal in or just above the core, which potentially has implications for our understanding of the planet's deep nitrogen cycle," said team member Sergey Lobanov.