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One striking anomaly of water ice has been largely neglected and never explained. Replacing hydrogen (H) by deuterium (H) causes ice to expand, whereas the “normal” isotope effect is volume contraction with increased mass. Furthermore, the anomaly increases with temperature , even though a normal isotope shift should decrease with and vanish when is high enough to use classical nuclear motions. In this study, we show that these effects are very well described by {\it ab initio} density functional theory. Our theoretical modeling explains these anomalies, and allows us to predict and to experimentally confirm a counter effect, namely that replacement of O by O causes a normal lattice contraction.

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