4.8 Article

Ferroelectric hexagonal and rhombic monolayer ice phases

Journal

CHEMICAL SCIENCE
Volume 5, Issue 5, Pages 1757-1764

Publisher

ROYAL SOC CHEMISTRY
DOI: 10.1039/c3sc53368a

Keywords

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Funding

  1. MOST [2011CB921400]
  2. NSFC [20603032, 20733004, 91021004, 20933006, 21121003, 2123307]
  3. Fundamental Research Funds for the Central Universities [WK2340000006, WK2060140005, WK2060030012]
  4. CAS [XDB01020300]
  5. USTCSCC
  6. UNL Research Council
  7. NSF [CBET-1066947, CHE-1306326]
  8. ARL [W911NF1020099]
  9. Nebraska Research Initiative
  10. USTC
  11. Division Of Chemistry [1306326] Funding Source: National Science Foundation

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Two new phases of water, the mid-density hexagonal monolayer ice and the high-density flat rhombic monolayer ice, are observed in our molecular dynamics simulations of monolayer water confined between two smooth hydrophobic walls. These are in addition to the two monolayer ices reported previously, namely, the low-density 4.8(2) monolayer ice and the high-density puckered rhombic monolayer ice (HD-pRMI). Stabilities of the structures are confirmed by ab initio computation. Importantly, both new phases and the HD-pRMI are predicted to be ferroelectric. An in-plane external electric field can further stabilize these ferroelectric monolayer ices.

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