Henry's law describes the equilibrium reached when a gas dissolves in a liquid: at a fixed temperature, the amount
of gas dissolved is directly proportional to the partial pressure of that gas maintained above the liquid,
where p is the gas's partial pressure, x is its mole fraction actually dissolved in the liquid, and KH is
the Henry's law constant — a proportionality constant characteristic of the particular gas-solvent pair and
temperature. A plot of p against x is a straight line through the origin, and a larger KH corresponds to
lower solubility, since a greater pressure is then needed to dissolve the same mole fraction.
Gas solubility depends on the identity of both the gas and the solvent, and — importantly — falls as temperature
rises, since dissolving a gas is normally exothermic, so by Le Chatelier's principle warming the liquid shifts the
dissolution equilibrium back toward undissolved gas (equivalently, KH increases with temperature). This
explains why warmer water holds less dissolved oxygen, stressing aquatic life, and why gas solubility calculations
in this chapter always specify a fixed temperature.
Henry's law underlies several practical situations: bottling soft drinks under high CO2 pressure to
force a large mole fraction of gas into solution, so that the drink fizzes once the pressure is released; deep-sea
divers dissolving unusually large amounts of nitrogen in their blood under pressure, risking decompression
sickness ("the bends") if they ascend too quickly and the dissolved gas suddenly comes out of solution as
bubbles; and the lower dissolved-oxygen intake experienced at high altitude, where the reduced atmospheric partial
pressure of oxygen means less of it dissolves in blood plasma, causing altitude sickness.