Hydrogen bonds make ice float, and they hold the two strands of your DNA together.
Ice floats
In liquid water, hydrogen bonds break and form all the time as the molecules tumble past each other, and the molecules pack close together. When water freezes, each molecule locks into four hydrogen bonds with its neighbours, in a regular pattern of six-sided rings. The rings have space in the middle, so the molecules end up further apart than in the liquid.
The same amount of water takes up about 9% more space as ice, so ice is less dense than water and floats. For most substances, the solid is denser than the liquid and sinks.
This matters for life on Earth. A pond freezes from the top down, and the layer of ice on top helps keep the water below from freezing, so fish live through the winter. Water that expands as it freezes also bursts pipes and splits rocks apart. The six-sided rings even show in snowflakes, which grow as six-sided crystals.
DNA's base pairs
You have already met DNA's base pairs: A pairs with T, held by 2 hydrogen bonds, and G pairs with C, held by 3. These are the same hydrogen bonds as in water. A δ+ hydrogen on an N–H group of one base reaches a lone pair on a δ− oxygen or nitrogen atom of the base opposite.
Each hydrogen bond is weak, so a cell can unzip the two strands to read or copy them. Millions of them along a DNA molecule hold the strands together firmly. Hydrogen bonds between -OH groups also hold cellulose chains side by side in plant fibres, as you have seen, and they help hold each protein's chain folded the right way.
Quick check
That's the end of lesson 12
In this lesson you found out:
- The pulls between molecules, and how they set boiling points
- What a hydrogen bond is, and why water boils at 100 °C
- Why oil and water separate, and what dissolves in what
- Why ice floats, and how hydrogen bonds hold DNA's base pairs together