New research suggests helium can bond with iron under extreme pressures and temperatures, challenging previous assumptions about noble gas reactivity.
Scientists used a laser-heated diamond anvil cell to demonstrate helium integration into iron's crystal structure at pressures up to 55 gigapascals.
The findings indicate that helium, instead of remaining separate, can become part of iron's atomic lattice, forming stable compounds like FeHex.
This discovery sheds light on helium's potential storage in Earth's core, contrary to the belief that it was mainly trapped in the mantle.
The high helium concentrations found in iron core samples suggest a significant reservoir of primordial helium, altering our understanding of Earth's internal composition.
The experimental approach, combining high-temperature synthesis and cryogenic analyses, allowed for the detection of higher helium concentrations in iron.
The presence of helium in Earth's core offers insights into the planet's early development, challenging traditional models of gas loss during Earth's formation.
This research also hints at the possibility of helium interacting with other volatile elements and contributing to the origin of Earth's water and atmosphere.
Future studies will explore if helium-iron compounds exist in deeper planetary interiors, impacting our understanding of planetary composition and material science.
The discovery of helium bonding with iron not only expands our knowledge of Earth's core but also has implications for the development of advanced materials.