APPLIED FIZZICS · Field Notes · Edition No. 11
A whimsical look at the universe through a glass of Champagne (or your favorite cocktail).
September 29 · Seattle, Washington
Dear Reader,
Put an ice cube in a glass of water and it floats. Hardly breaking news.
But that familiar little observation is one of water’s most consequential peculiarities. It helps fish survive winter. It explains the tip of an iceberg, and played a role in the wreck of the Titanic. And it lets us fill a glass right to the brim, leave a sizable chunk of ice sticking out of it, and ask a question:
When that ice melts, where does the water go?
Water does things differently
Most substances become denser when they freeze. Water expands instead.
In ordinary ice, water molecules arrange themselves into an open crystal structure that takes up more space than they occupied as a liquid. The same mass occupies a larger volume, so its density decreases.
That’s why ice floats—even perfectly clear ice without a single air bubble.
We see it so often that it hardly seems remarkable. But your ice cube is doing something distinctly unusual in the material world.
Good news for fish
Floating ice also changes what winter looks like beneath a lake’s surface.
Because ice floats, lakes freeze from the top down. The layer of ice at the surface acts as insulation, while water beneath it can remain liquid.
If ice were denser than water, newly formed ice would sink, exposing more water to the freezing air. Lakes in cold climates could freeze solid from the bottom up, profoundly changing the environment in which aquatic life survives.
So this apparently trivial peculiarity of the ice in your cocktail has consequences that extend far beyond the cocktail hour.
And that raises a much bigger question.
What happens when seemingly small properties of the physical world turn out to be essential to the kind of universe we live in?
That question took this week's Field Notes somewhere I wasn't expecting to go.
From an ice cube in a cocktail, we somehow ended up talking about frozen lakes, atomic nuclei, the fundamental constants of physics—and why the universe has properties that allow us to be here asking questions about it in the first place.
All because ice floats.
Watch Field Notes #11 below: What If Ice Sank?
Meanwhile, back at the experiment...
For this week’s demonstration, I made an ice “cube” approximately ten inches tall.
All right, it’s a pillar. But I’m calling it a cube.
I floated it inside a cylinder filled right to the brim with water. A substantial portion of the ice stuck up above the waterline, looking very much like a spill waiting to happen.
So what happened when it melted?
Nothing.
The water stayed at the brim.
Archimedes explained why more than 2,000 years ago. A floating object displaces an amount of water equal in weight to the object itself. When our ice melts, it becomes exactly the amount of water it had already displaced while it was floating.
Or, more intuitively:
The ice simply melts into the hole it had already made in the water.
No overflow required.
Want to see Archimedes' Principle derived from first principles? It takes nothing but simple algebra. Click the link below.
ρgh From First Principles: Why Ice Floats ›
Archimedes’ principle says that a floating object displaces an amount of water equal in weight to the object itself. But we can derive that result from something even more fundamental: water pressure increases with depth.
Imagine a column of water with cross-sectional area A and depth d. If the density of water is ρw, the mass of that column is
Its weight is therefore

Pressure is force divided by area. Using pressure relative to the atmosphere, the pressure at depth d is therefore
Now imagine a vertical column of ice with the same cross-sectional area A, total length L, and density ρi. It floats with a length d below the surface.
The water pressure acting on the bottom of the ice produces an upward force
while the weight of the entire ice column pulling downward is
Because the ice is floating, those two forces must be equal:
The gravitational acceleration g and the area A cancel, leaving
In other words, the fraction of the ice below the waterline is simply the density of ice divided by the density of water.
Ordinary ice near its melting point has a density about 92% that of liquid water, so roughly 92% of a floating piece of ice lies below the surface.
And notice what happened along the way. The upward force was
But ρwAd is simply the mass of the water displaced by the submerged ice. So the buoyant force is equal to the weight of the displaced water.
And there, starting only with the fact that pressure increases with depth, we have arrived at Archimedes’ principle.
Next Field Note: what makes ice so good at its job?
Floating is only the beginning of ice’s contribution to a drink.
Next time, we’ll look at the surprisingly large amount of heat ice absorbs when it melts—and why ice doesn't chill your cocktail simply because it's cold.
For now, here's this week's Quiz.
This Week's Quiz
Question: Suppose our floating ice cube contained a small stone—small enough not to sink the ice cube. When the ice melts and the stone sinks to the bottom, will the water level rise, fall, or stay the same?
Reveal the Answer
The correct answer is: the water level FALLS.
While the stone is trapped inside the floating ice, the ice-and-stone combination must displace an amount of water equal to its total weight. So the stone causes the floating ice to displace an additional amount of water equal in weight to the stone.
When the ice melts, however, the stone sinks to the bottom. A submerged object displaces only its own volume of water.
Because the stone is denser than water, the volume of the stone is smaller than the volume of water that has the same weight as the stone.
So after the stone sinks, it displaces less water than it did while it was being supported by the floating ice.
The water level therefore falls.
The ice itself is a wash: when it melts, its meltwater exactly replaces the water the ice had been displacing. The entire change in water level comes from the stone.
One little rock turns our previous experiment on its head.
Cheers,

Evan Wallace
President, Applied Fizzics Inc.
Makers of The Perlage System®
Want more Champagne science, carbonation experiments, and assorted investigations? Visit the Applied Fizzics Field Notes archive .

