H2O and D2O ice differ considerably in their quantum behavior
The quantum properties of normal and heavy ice show surprising differences.
Scientific Explanation
In ice, hydrogen atoms sit in double-well potentials between neighboring oxygen atoms. They can switch between two equilibrium positions, and this switching determines the proton ordering in the ice lattice. The quantum properties of this system differ fundamentally between H2O ice and D2O ice.
The light hydrogen atom (proton) has a large zero-point energy due to its low mass — it is strongly delocalized quantum mechanically and can efficiently tunnel through the energy barrier between the two positions. The tunnel splitting, a measure of tunneling probability, is significantly larger for protons than for deuterons.
The consequences are manifold: H2O ice has a larger lattice constant than D2O ice (even though the proton is lighter), because the greater zero-point motion effectively expands the lattice. The heat capacity at low temperatures differs because the excitation spectra are different. The residual entropy — the question of whether ice becomes fully proton-ordered at the lowest temperatures — is also influenced by tunneling processes.
Everyday Relevance
These quantum differences may seem esoteric but have practical consequences. In neutron scattering, D2O ice crystals are preferred because deuterium scatters neutrons less strongly than hydrogen — but the altered crystal structure must be taken into account. In cryobiology, where cells are frozen at extremely low temperatures, the proton ordering affects the mechanical properties of ice and thus the survival chances of the cells. And in fundamental physics, comparing H2O and D2O ice provides direct access to studying quantum effects in condensed matter systems.