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Chapter 2 · Part 8 of 10
  1. Chapter overview
  2. 1Inside an atom
  3. 2Electron shells and the periodic table
  4. 3Atomic mass, moles, and isotopes
  5. 4Covalent bonds and molecules
  6. 5Polar bonds and weak attractions
  7. 6Ions and chemical reactions
  8. 7Water as a solvent
  9. 8Water's special properties
  10. 9Acids, bases, and the pH scale
  11. 10Buffers and pH balance

Water's special properties

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The hydrogen bonds between water molecules do more than help water dissolve things. They explain why ice floats, why water is slow to heat up, and how insects can stand on a pond.

Ice, liquid water, and water vapor

H₂O exists in all three states of matter: solid (ice), liquid (water), and gas (water vapor). At the temperatures found over most of Earth, it’s a liquid, in which hydrogen bonds between molecules constantly break and re-form.

In ice, the hydrogen bonds hold the molecules in an orderly, open framework, with more space between molecules than in liquid water. So a block of ice has less mass than the same volume of liquid water. In other words, ice has a lower density (mass packed into a given space), and that’s why it floats. Ice is also less likely than liquid water to take part in chemical reactions.

Two panels. On the left, liquid water: molecules in a close, disordered jumble with a few hydrogen bonds. On the right, ice: the same molecules locked into an open hexagonal lattice by hydrogen bonds, with more space between them.
Figure 2.8 In liquid water, hydrogen bonds constantly form and break. In ice, they hold every molecule in an open lattice, which makes ice less dense than liquid water.

Water holds steady as a liquid

Changing from one state to another takes in or gives off energy, and water’s many hydrogen bonds make these amounts large.

Thanks to its high heats of vaporization and fusion and its high specific heat, water holds steady as a liquid. That’s why large lakes and oceans change temperature slowly and keep nearby land milder. Life has evolved to work best at the temperatures where water stays liquid.

Dissolved solutes widen that liquid range. Pure water freezes at 0 °C and boils at 100 °C, but adding solutes lowers the freezing point and raises the boiling point. Properties like these, which depend only on the number of dissolved solute particles and not on what kind they are, are colligative properties. Antifreeze keeps the water in a car’s radiator from freezing in winter, dissolved salts help keep oceans liquid below 0 °C, and dissolved solutes act as antifreeze in some organisms, too.

Water’s jobs in living things

Water doesn’t just surround reactions; it takes part in them. In a hydrolysis reaction, water is used to break apart another molecule:

R₁–R₂ + H–O–H → R₁–OH + H–R₂

Here R₁ and R₂ stand for two groups of atoms joined by a covalent bond. That bond breaks, and so does one of water’s bonds: the OH from water attaches to one group and the H to the other. (Hydro means water, and lysis means to break apart.) Cells break many large molecules into smaller units this way.

Water’s other jobs follow from its properties:

Check yourselfWhy does ice float on liquid water?

In ice, hydrogen bonds lock the molecules into an orderly, open lattice with more space between them than in liquid water. That makes ice less dense than liquid water, so it floats.

Practice questions

  1. 1 of 2

    In winter, ice forms on the surface of a pond and floats instead of sinking. Why is ice less dense than liquid water?

  2. 2 of 2

    Why does sweat evaporating from your skin cool you down?