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KRISS Team Identifies Ice XXI, a New Room-Temperature High-Pressure Phase of Water

A dynamic diamond anvil paired with microsecond X‑ray probing captured previously unseen crystallization pathways that revealed the phase.

Overview

  • Experiments pushed water above 2 gigapascals at room temperature, producing a supercompressed liquid before it crystallized.
  • The KRISS-built dynamic diamond anvil cell shortened pressure ramps to about 10 milliseconds, reducing nucleation artifacts seen in conventional cells.
  • Microsecond-resolution measurements at the European XFEL recorded multiple freezing–melting routes that culminated in Ice XXI.
  • Structural analysis found an unusually large unit cell with a flattened rectangular geometry, distinguishing Ice XXI from known ice phases.
  • The peer-reviewed work, led by KRISS with 33 collaborators and support from European XFEL and DESY, was published in Nature Materials in October and suggests relevance to high-pressure ice layers inside icy moons.