High-pressure alloying of potassium and iron: Radioactivity in the Earth's core?

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

3

Mineral Physics: High-Pressure Behavior, Tectonophysics: Earth'S Interior-Composition And State (1212), Tectonophysics: Heat Generation And Transport

Scientific paper

High-resolution x-ray diffraction provides evidence that potassium (K) alloys with iron (Fe) when the two pure elements are heated together at pressures above ~26 gigapascals (GPa). Increases of 2-3% in volume of the ɛ (hexagonal close packed: hcp) high-pressure phase of Fe can be attributed to the incorporation of ~1 atomic% (~7000 ppm by weight) K into Fe. Our results provide experimental support for predictions, derived from quantum mechanical calculations, that pressure can induce the alloying of K with Fe due to a change in the chemical-bonding character of K from alkaline- to transition-metal. Radioactive decay through the incorporation of 40K into the core could therefore be an important source of energy deep inside the Earth, helping to power the geodynamo and mantle dynamics.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

High-pressure alloying of potassium and iron: Radioactivity in the Earth's core? does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with High-pressure alloying of potassium and iron: Radioactivity in the Earth's core?, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and High-pressure alloying of potassium and iron: Radioactivity in the Earth's core? will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-879571

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.