To add on a little, this due to how water molecules arrange themselves when frozen. They form a sort of crystalline lattice that ends up having a lot of space in between, which is why ice is less dense. However that does happen until a very specific point right before it freezes. I don’t remember exactly where this is, it’s like, four Celsius or something, but water does actually contract like you’d expect, right up until that point.
Water is a very interesting chemical. When liquid the molecules of H2O can move around freely whereas, when solid, the molecules are held in place by intermolecular forces. As a liquid the molecules are able to be close together but when it decreases in temperature those intermolecular forces hold the molecules apart. Water is most dense at about 4 degrees Celsius. Any hotter and the water expands, any colder and the forces hold molecules apart.
Water is an exception to the rule; when water freezes into ice it gets less dense (which is why ice floats in water, that wouldn’t work with say, a steel bar in a vat of liquid steel). It does this because it’s a very polar molecule, so when you take energy out by freezing it and slowing molecules down, the magnetic repulsion of individual molecules is enough to force them to spread out more than.
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