Ice: A strongly correlated proton system

被引:50
作者
Castro Neto, A. H.
Pujol, P.
Fradkin, Eduardo
机构
[1] Boston Univ, Dept Phys, Boston, MA 02215 USA
[2] Ecole Normale Super Lyon, Phys Lab, F-69364 Lyon 07, France
[3] Univ Illinois, Dept Phys, Urbana, IL 61801 USA
基金
美国国家科学基金会;
关键词
t;
D O I
10.1103/PhysRevB.74.024302
中图分类号
T [工业技术];
学科分类号
08 ;
摘要
We discuss the problem of proton motion in hydrogen bond materials with special focus on ice. We show that phenomenological models proposed in the past for the study of ice can be recast in terms of microscopic models in close relationship to the ones used to study the physics of Mott-Hubbard insulators. We discuss the physics of the paramagnetic phase of ice at 1/4 filling (neutral ice) and its mapping to a transverse field Ising model and also to a gauge theory in two and three dimensions. We show that H3+O and HO- ions can be either in a confined or deconfined phase. We obtain the phase diagram of the problem as a function of temperature T and proton hopping energy t and find that there are two phases: an ordered insulating phase which results from an order-by-disorder mechanism induced by quantum fluctuations, and a disordered incoherent metallic phase (or plasma). We also discuss the problem of decoherence in the proton motion introduced by the lattice vibrations (phonons) and its effect on the phase diagram. Finally, we suggest that the transition from ice Ih to ice XI observed experimentally in doped ice is the confining-deconfining transition of our phase diagram.
引用
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页数:12
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