A second type of liquid water with fewer hydrogen bonds could explain why ice floats

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Water is weird. It breaks many of the usual rules that liquids are expected to follow. In 1992 a team of researchers suggested why that is. They proposed that there are two types of liquid water, which only become distinct at temperatures well below freezing point. Researchers have sought evidence for this bold conjecture ever since – and now an international team claims to have found it.

Water is weird. It breaks many of the usual rules that liquids are expected to follow. In 1992 a team of researchers suggested why that is (bit.ly/3RLcoaM). They proposed that there are two types of liquid water, which only become distinct at temperatures well below freezing point. Researchers have sought evidence for this bold conjecture ever since – and now an international team claims to have found it.

The team led by Anders Nilsson of Stockholm University used ultrafast laser pulses to rapidly melt ice and then studied the resulting supercooled liquid water.

Close up on a splash of water

Source: © Snide12/Shutterstock

Solid, liquid … or something inbetween? Water may have more than one liquid state

In ordinary water, H2O molecules form intermolecular hydrogen bonds between the lone pairs on their oxygen atoms and the positively charged hydrogen atoms of nearby water molecules. Each water molecule forms four hydrogen bonds resulting in an extensive network of molecules all being held at arm’s length from each other.

This model of hydrogen bonding remains the key explanation used in the curriculum to describe why water behaves unusually, including why ice floats. The team’s findings may add further detail rather than replace that explanation.

Fewer hydrogen bonds

The scientists observed a second liquid phase for water containing fewer hydrogen bonds than we would expect to see in liquid water. The lack of bonds holding the molecules apart means that this second phase is more dense than ordinary water.

It is thought that liquid water typically exists as mixtures of these two states. The presence of this second form of liquid water may explain some of its more unusual properties, such as why it is most dense at 4°C above freezing.

As a rule, liquids shrink when cooled, causing their density to increase. Ice should therefore sink in liquid water. But as we know, it floats. The findings of these new experiments suggest that liquid water’s higher density comes from its second, denser liquid phase.

This article is adapted from Philip Ball’s in Chemistry World

Nina Notman

Reference

S You et al, Science, 2026, 391, 1387 (doi.org/10.1126/science.aec0018)

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