Solubility
Pour salt into water and it vanishes into solution; pour it into oil and it just sits at the bottom. That single contrast is solubility — the maximum amount of a solute a solvent can hold, at a given temperature, before the solution is saturated. For solids and liquids dissolving in liquids, "like dissolves like" and a rough rule of thumb about temperature get you most of the way. But the CBSE Class 12 syllabus asks for something sharper: how gases dissolve in liquids, captured in one clean proportionality called Henry's law. It explains why a soda bottle fizzes the instant you twist the cap, why a scuba diver who surfaces too fast can get the bends, and why mountaineers gasp for breath on a summit. This article builds Henry's law from the ground up, derives it as a proportionality you can invert either way, and drills the numericals examiners actually ask — partial pressure to mole fraction, and back again — while flagging the traps that cost marks.
At constant temperature, the partial pressure of a gas above a solution is directly proportional to the mole fraction of that gas dissolved in the liquid, , and a larger Henry's law constant means the gas is less soluble.
The core idea
Solids and liquids in liquid solvents follow a qualitative rule you already know from making tea or trying (and failing) to mix oil and water: polar solutes dissolve in polar solvents, non-polar solutes dissolve in non-polar solvents, because dissolution needs solute–solvent attractions strong enough to out-compete the solute's own internal bonding and the solvent's own internal bonding. Sugar and salt (polar/ionic) dissolve readily in water (polar); naphthalene (non-polar) dissolves in benzene (non-polar) but barely at all in water. For most solids dissolving in liquids the process absorbs heat, so raising the temperature usually pushes solubility up — though there are well-known exceptions, and the syllabus does not ask you to predict them quantitatively.
Gases in liquids are where the syllabus wants numbers, not just intuition. Shake a closed bottle of soda and gas keeps dissolving until the rate of gas molecules entering the liquid equals the rate leaving it — a dynamic equilibrium. At that equilibrium, English chemist William Henry found a strikingly simple relationship between how much gas is squeezed above the liquid and how much ends up dissolved in it:
where: is the partial pressure of the gas in the vapour phase above the solution, is the mole fraction of that gas dissolved in the liquid, and is the Henry's law constant — a number specific to one gas–solvent pair at one temperature, with units of pressure (since is a dimensionless ratio). Henry's law is a straight line through the origin on a plot of against : double the pressure, double the dissolved mole fraction. It only applies to gases that dissolve without reacting chemically with the solvent — HCl and NH₃ ionise in water instead of simply dissolving, so Henry's law does not describe them. The figure below shows why is the whole story: it is literally the slope of the -versus- line, so a steep line (large ) means you need a lot of pressure to force even a little gas into solution — low solubility — while a shallow line (small ) means the gas dissolves easily at modest pressure.
Temperature dependence: increases with rising temperature for most gases in water. That matches everyday experience — warm soda goes flat faster, and a lake's dissolved oxygen drops as it warms, stressing fish. A larger at the same fixed pressure forces smaller, so the gas becomes less soluble.
Applications worth remembering: carbonated drinks are bottled under high CO₂ pressure so more gas dissolves; opening the cap drops the pressure, so by Henry's law the equilibrium mole fraction of dissolved CO₂ falls and the excess escapes as bubbles. Scuba divers who ascend too quickly can suffer the "bends," because dissolved nitrogen in the blood, which stayed in solution under high pressure at depth, suddenly bubbles out as pressure drops. At high altitude the partial pressure of atmospheric O₂ is lower, so less oxygen dissolves in blood, causing altitude sickness.
The goal is to show, starting only from the proportionality that defines Henry's law, how to rearrange it into the form actually needed for numericals — solving for the dissolved mole fraction when the partial pressure and the constant are given — and to confirm that the rearrangement is dimensionally consistent so the result is a pure, unitless mole fraction as it must be.
Step 1. Start from Henry's law as stated: . Here carries units of pressure (say pascals), and also carries units of pressure, because itself is a ratio of moles to moles and therefore has no units.
Step 2. Divide both sides by to isolate : , so .
Step 3. Check the units cancel correctly. Both and are measured in the same pressure unit (pascals, or atmospheres, as long as you are consistent), so has units of — a pure number, exactly what a mole fraction must be. This confirms the rearrangement is valid and gives a direct recipe: read off and from the problem, divide, and the answer is the dissolved mole fraction with no further unit conversion needed.
Worked example
Problem: The Henry's law constant for CO₂ dissolved in water is Pa. A soft drink is bottled under a CO₂ partial pressure of Pa. Find the mole fraction of dissolved CO₂, and then find the new equilibrium mole fraction once the bottle is opened and the CO₂ partial pressure above the liquid falls to atmospheric, about Pa (CO₂'s share of ordinary air).
Step 1 — Apply Henry's law for the sealed bottle. , so about 1.5 CO₂ molecules per thousand molecules of solution while sealed.
Step 2 — Apply Henry's law again for the open bottle. , roughly ten thousand times smaller than the sealed-bottle value.
Step 3 — Interpret the drop. The equilibrium mole fraction the liquid can hold collapses once the cap is off and the CO₂ partial pressure crashes toward atmospheric levels. The drink is now far supersaturated relative to the new, tiny equilibrium value, so the excess dissolved CO₂ escapes as bubbles until the liquid re-equilibrates — this is the fizz. The mole fraction of dissolved CO₂ falls from about (sealed, under pressure) to about (open, at atmospheric CO₂ pressure).
Competitive stretch
Problem: At 298 K, oxygen's Henry's law constant in water is Pa. Air exerts an O₂ partial pressure of Pa. Find the dissolved mole fraction, then estimate how many O₂ molecules that represents per litre of water (1 L water 55.5 mol).
Step 1 — Partial pressure of O₂. Pa.
Step 2 — Apply Henry's law. .
Step 3 — Convert to moles per litre. Since for a dilute solution, per litre. About mol (roughly g) of O₂ dissolves per litre of water in equilibrium with air at 298 K — a small but life-sustaining amount for aquatic organisms, and one that shrinks further as rises with warming water.
Common traps
- Reading "higher " as "higher solubility." It is the opposite: , so a larger Henry's constant makes smaller at fixed pressure — less gas dissolves.
- Using total pressure instead of the gas's own partial pressure when the gas above the solution is part of a mixture, such as O₂ within air rather than pure O₂.
- Applying Henry's law to gases that react with the solvent, like NH₃ or HCl in water — these ionise or react rather than simply dissolving, so the simple proportionality fails.
- Treating as universal for a gas. It is specific to one gas, one solvent, and one temperature — always check whether the given value matches the conditions in the problem.
Ask the tutor: want to try Henry's law numericals with mixed units, or see why Raoult's law turns out to be a special case of Henry's law?
Why does K_H increase with temperature instead of decrease, like I would expect for a solid dissolving faster when heated?
Gas dissolution is generally exothermic — the gas molecule loses more energy settling into the liquid than it takes to make room for it — so, by Le Chatelier's reasoning, adding heat pushes the equilibrium back toward the gas phase, reducing solubility. That shows up as a rising , since falls when rises at fixed pressure. This is the opposite trend from most solids dissolving in liquids, where dissolution usually absorbs heat, so heating helps solubility. The two processes have different thermodynamics, so do not assume gases and solids behave the same way with temperature.
Is Henry's law the same thing as Raoult's law?
Not the same, but closely related — Henry's law is actually a more general statement. Raoult's law, covered in the next topic, says the partial pressure of a volatile solvent component is its mole fraction times its pure vapour pressure. It turns out Raoult's law is the special case of Henry's law that applies to the solvent itself (or to a solute present in very high concentration), where the "Henry's law constant" for that component happens to equal its pure vapour pressure. For a dilute gas solute, Henry's law with an experimentally measured is the right tool.
If I am given K_H in different pressure units than the partial pressure in the problem, what do I do?
Convert one of the two quantities so both and share the same pressure unit before dividing — Henry's law only works dimensionally when and match, since their ratio must come out as a pure, unitless mole fraction. A common slip is mixing pascals with atmospheres or bar without converting, which throws the answer off by several orders of magnitude even though the method is right. Always check units first, exactly as in the derivation above.