Compounds are classified as high-pressure ices based on specific crystal structures and hydrogen bonding networks.
Compounds such as water ice form diverse high-pressure crystalline phases whose classifications and transitions are dictated by their underlying crystal structures and hydrogen bonding networks.
The retrieved literature consistently supports the premise that high-pressure ice phases and polymorphs are characterized and classified based on their crystal structures and hydrogen-bonding behaviors (e.g., proton ordering, symmetrization, and network topologies).
Kenneth S. Schweizer, Frank H. Stillinger. High pressure phase transitions and hydrogen-bond symmetry in ice polymorphs. 1984. https://doi.org/10.1063/1.446800
Paper [0] discusses how high-pressure ice polymorphs undergo phase transitions driven by proton ordering and hydrogen-bond symmetrization.
See more details
F. Della Pia, Andrea Zen, D. Alfé, A. Michaelides. DMC-ICE13: Ambient and high pressure polymorphs of ice from diffusion Monte Carlo and density functional theory.. 2022. https://doi.org/10.1063/5.0102645
Paper [1] notes that the structural diversity of high-pressure ice polymorphs arises from hydrogen bonding and dispersion forces.
Maharjan R, Williamson C, Fennell CJ. Assessing Order in Liquid, Supercooled, and Crystalline Water.. 2026. https://doi.org/10.1021/acs.jpcb.5c08791
Paper [11] explains that different crystalline ice polymorphs possess unique degrees of order and hydrogen-bonding network distributions.
The paper trail · every fact has a biography
Challenge the receipt
Citation formatting by citeproc-js (Frank Bennett) and the Citation Style Language project. Source and licenses.
Terms · Privacy · How verdicts work · Dispute this receipt