New insights into the glaciation cycles that occurred on Earth long before humans began affecting the temperature of the atmosphere and oceans are now possible using the technique of
measuring noble gas quantities.
Not exact matches
For example, they want to
measure the planet's inventory of stable
noble gases, such as xenon and krypton, which change little in abundance over billions of years and hold clues to planetary origins.
Only with this experimental set - up is it possible to
measure the tiny forces between microscope tip and
noble gas atom, as a pure metal surface would allow the
noble gas atoms to slide around.
By
measuring the abundance of an isotope of the
noble gas argon in the rock or its crystals, Gazel and his colleague Michael Kunk of the U.S. Geological Survey found that the magma was much younger than the last known volcanic event on the East Coast — which occurred when the supercontinent of Pangaea slowly pulled apart into North America, Africa and South America some 200 million years ago, forming the Atlantic Ocean in the process.
Greg Holland, a postdoctoral researcher in isotope geochemistry at the University of Manchester in England, and his colleagues
measured the amounts of various isotopes of
noble gases in the Bravo Dome
gas field in New Mexico, where magmatic
gases — primarily carbon dioxide — that allow the mantle to be sampled are buried hundreds of meters below.
Using mass spectroscopy, they
measured the full suite of
noble gases, with an emphasis on helium, neon and argon.
Researchers at the University of California, San Diego decided on a different model — they
measured the ratio of
noble gases in the atmosphere, which are in direct relation to the ocean's temperature.
Severinghaus
measured values of the
noble gases argon, krypton, and xenon in air bubbles captured inside ice cores in Antarctica.