How the Experiments Worked
Researchers at The University of New Mexico recreated extreme conditions from Earth's formation by exposing silicate rock samples to temperatures ranging from 1,200 to 1,400 degrees Celsius. They used flowing hydrogen gas and repeated the tests with helium for comparison. Each experiment ran for between 15 minutes and three hours.
When the rocks were heated in hydrogen, almost 80% of their iron oxide was transformed into metallic iron, with water vapor produced during the reaction. The researchers did not observe the same reaction when helium was used instead of hydrogen.
"We had suspected and hoped that we would produce iron metal and water in our reduction experiments, but we really had no way of knowing how fast and how much. We were quite surprised to find that extrapolation of our work suggests that hundreds of oceans' worth of water were likely produced in this way," said Zachary Sharp, professor and director of Earth and Planetary Sciences.