New High-Pressure Phase of<mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" display="inline"><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant="normal">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub></mml:mrow></mml:math>O: Ice X
Physical Review LettersPublished 9 April 1984
A. Polian, M. Grimsditch
Citations161
SJR quartileQ1
SJR score2.86
SNIP2.41
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Abstract
${\mathrm{H}}_{2}$O at 300 K has been studied up to 67 GPa by Brillouin scattering. A transition to a new form of ice occurs at 44 GPa. This is the tenth known solid form of ${\mathrm{H}}_{2}$O and may be the expected "symmetric-ice" structure.
Keywords
ChemistryEarth and Planetary SciencesPhysics and Astronomy
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