Washington, D.C.—In Earth’s interior, water (H2O) plays an important role in rock physics, but geoscientists rarely treat water in its constituent forms, that is as hydrogen plus oxygen. New work from a team led by Carnegie’s Dave Mao has identified that hydrogen can escape from the water under conditions found in Earth’s lower mantle leading to a new paradigm in lower-mantle chemistry. Their results were published in Proceedings of the National Academy of Sciences, U.S.A.
In the atmosphere, hydrogen is a colorless, transparent gas. It bonds with oxygen to form water, which fuels the biosphere on the Earth’s surface. Deep in the rocky world beneath our feet, so-called