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The solubility of oxygen in water is temperature-dependent, and about twice as much (14.6 mg·L−1) dissolves at 0 °C than at 20 °C. To illustrate, recall bubbles forming in a pot of water right before it begins to boil; these bubbles are oxygen that was dissolved at room temperature, but is being ejected as the temperature rises. Oxygen can slip into the crevasses or “holes” that exist in the loose hydrogen-bonded network of water molecules without forcing them apart. A very physical perspective on solubility of oxygen in water is that when the water is colder, the water molecules move less, and the oxygen remains trapped in the aqueous solution.

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Q: Why does cold water hold more oxygen?
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