Hydrogen bond symmetrization in the C2 and C3 hydrogen hydrate phases occurs as a continuous crossover at lower pressures than in pure ice, driven by quantum fluctuations and guest-host coupling.
Hydrogen bond sym- metrisation in D2O ice observed by neutron diffraction,
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Hydrogen bond symmetrization in high-pressure ice clathrates
Hydrogen bond symmetrization in the C2 and C3 hydrogen hydrate phases occurs as a continuous crossover at lower pressures than in pure ice, driven by quantum fluctuations and guest-host coupling.