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How does water freeze?
Quick answer
Water freezes when its molecules slow down enough for hydrogen bonds to lock them into a hexagonal crystal lattice. This typically happens at 0°C under normal pressure, but dissolved substances like salt can lower the freezing point. The open lattice makes ice less dense than liquid water, so ice floats.
Water freezes when its molecules slow enough to lock into a rigid, repeating lattice held together by hydrogen bonds. This happens at 0°C under normal pressure, but impurities and dissolved substances can lower that temperature.
Step by step
- Water molecules are attracted to each other through hydrogen bonds between partial positive and negative ends.
- As the temperature drops, molecules lose kinetic energy and move more slowly, allowing bonds to persist longer.
- At the freezing point, molecules arrange into a hexagonal pattern, forming a tiny ice crystal nucleus.
- The crystal grows outward as more molecules join the lattice, releasing heat in the process.
- Impurities or dissolved substances disrupt the lattice, requiring lower temperatures to freeze.
Key things to understand
- Water molecules are polar, with partial negative oxygen and partial positive hydrogen ends that attract each other.
- As water cools, its molecules lose kinetic energy and move more slowly, allowing hydrogen bonds to hold them in place.
- At 0°C, the molecules arrange into a hexagonal crystal lattice, which is why ice is less dense than liquid water.
- Freezing requires nucleation, a starting point like a dust particle or a tiny ice crystal, to begin the crystal structure.
- Dissolved salts or sugars interfere with the lattice, lowering the freezing point, which is why seawater freezes below 0°C.
Labelled diagram
- Liquid water
Molecules move freely, constantly breaking and reforming hydrogen bonds.
- Cooling
Molecules slow down as kinetic energy decreases, so bonds last longer.
- Nucleation
A tiny cluster of molecules forms a stable hexagonal arrangement.
- Crystal growth
More molecules join the lattice, expanding the ice crystal.
- Ice
Rigid hexagonal lattice with open spaces makes ice less dense than water.
Real-world examples
- Ice cubes in a freezer freeze from the outside in because the surface cools first and nucleation starts there.
- Seawater freezes at about -2°C because dissolved salt interferes with the ice crystal lattice.
- Frost forms on grass on a cold night when water vapor deposits directly as ice crystals without becoming liquid.
- Snowflakes are hexagonal ice crystals that grow in clouds when water vapor freezes around dust particles.
Common mistake
✗ Myth: Water always freezes at exactly 0°C.
✓ Fact: Pure water freezes at 0°C under normal pressure, but dissolved substances like salt lower the freezing point. Also, very pure water can be supercooled below 0°C without freezing until nucleation occurs.
People also ask
What causes water to freeze?
Why does ice float on water?
Can water freeze at room temperature?
Can water freeze at temperatures above 0°C?
How does salt melt ice on roads?
Does water freeze faster if it starts hot?
Part of the guide: Everyday Science: Light, Heat & Matter →

