Physical and chemical equilibrium
Leave a glass of water uncovered and it slowly disappears — evaporation wins, no contest. Seal that same water in a stoppered flask, though, and after a while the water level stops falling. Nothing has stopped moving at the molecular level; water molecules still leave the surface as vapour and vapour molecules still strike the surface and rejoin the liquid. What has happened is that the two opposing processes have settled into a tie: evaporation and condensation now occur at exactly the same rate, so the net, measurable change is zero even though the underlying traffic never halts. That tied state is equilibrium, and it is the idea the entire ISC Class 11 unit on Equilibrium is built around. Chemistry splits it into two flavours: physical equilibrium, where matter only changes state or location (melting, evaporating, dissolving), and chemical equilibrium, where a reversible reaction settles into a balance between forward and reverse rates. This article builds the vocabulary, the general characteristics every equilibrium shares, and the reasoning for why it must be dynamic — the platform the next articles (equilibrium constants, Le Chatelier's principle, ionic equilibrium) stand on.
Equilibrium is a dynamic state in which two opposing processes — physical (melting/evaporation/dissolution) or chemical (a reversible reaction) — occur at equal, non-zero rates in a closed system, so measurable properties stay constant even though molecules keep converting back and forth.
The core idea
Physical equilibria — no new substance forms. Five patterns recur throughout the syllabus and everyday life:
- Solid Liquid: ice water at , 1 atm, rate of melting equal to rate of freezing.
- Liquid Vapour: water water vapour in a closed vessel, giving a constant vapour pressure.
- Solid Vapour: sublimation, e.g. solid iodine iodine vapour.
- Dissolution of a solid in a liquid: a saturated sugar solution with undissolved sugar at the bottom, dissolution rate equal to crystallisation rate.
- Dissolution of a gas in a liquid: a sealed carbonated drink, gas dissolving at the same rate it escapes.
Chemical equilibrium — a reversible reaction settles. Take in a closed vessel. As accumulates, its decomposition rate rises while the formation rate (fixed by the starting concentrations, then falling) drops; the two curves cross and, past that point, both proceed at the same rate. Nothing about the amounts needs to be equal at that instant — only the rates must match.
General characteristics apply to any equilibrium, physical or chemical, at constant temperature:
where: rate is the rate of the process going one way (melting, evaporation, dissolution, or the forward reaction) and rate is the rate of the exactly opposite process, both measured under the same fixed temperature. Because neither rate is zero, equilibrium is dynamic, not static. It follows that: (1) it is reached only in a closed system, where nothing escapes or enters; (2) macroscopic properties — mass of each phase, concentration, colour, pressure — stop changing with time; (3) the same equilibrium state is reached whether you start from pure reactants, pure products, or somewhere in between, under the same conditions; and (4) at a fixed temperature there is one definite value of the relevant constant (vapour pressure, solubility, or an equilibrium constant) — it changes only if temperature changes.
Why it works
This section has no numerical equilibrium constant to derive yet — that quantitative step is the next article's job. What needs justifying here is a purely conceptual claim: why must equilibrium be dynamic, and why does it require a closed system? Both follow directly from tracking rates rather than amounts. Consider evaporation in a sealed flask from the very start. Initially there is no vapour above the liquid, so only evaporation happens: liquid molecules with enough kinetic energy escape into the empty space above, and the vapour pressure climbs from zero. As vapour accumulates, some of those molecules now strike the liquid surface and rejoin it — condensation begins. Evaporation's rate stays roughly constant, because it depends only on temperature and the exposed liquid surface, neither of which is changing. Condensation's rate, however, keeps rising as more vapour molecules become available to strike the surface. Eventually the two rates must cross and become equal — at that instant, and from then on, the vapour pressure stops changing. This is why equilibrium is inevitable in a closed system: one rate is roughly fixed while the other climbs to meet it, and once they meet, nothing forces them apart again at constant temperature. Now see why an open system can never reach this state. If the flask were open, escaping vapour never accumulates — condensation's rate stays near zero forever, evaporation keeps winning, and the liquid eventually vanishes. There is no plateau to reach because one side of the balance is permanently starved. This is exactly why the definition insists on a closed system: equilibrium is not about a process running out of steam, it is about two rates converging because both reactants (or both phases) are trapped together and forced to keep meeting each other. The same logic, unchanged, carries over to a reversible chemical reaction: as product concentration builds, the reverse reaction's rate rises from zero while the forward rate falls from its initial maximum, and the crossing point is chemical equilibrium.
Worked example
Classify three sealed-container scenarios as physical or chemical equilibrium, and name the two opposing processes in each. (a) A stoppered jar of solid camphor, where after some time the space above the solid becomes saturated with camphor vapour. (b) in a closed glass bulb, where the brown colour (from ) stops changing in intensity. (c) A saturated solution in a stoppered bottle with excess undissolved solid at the bottom.
Step 1. Check for a new substance. In (a), camphor vapour is chemically identical to solid camphor — only the state changes, so this is a physical equilibrium (sublimation). The opposing processes are solid camphor subliming to vapour, and vapour depositing back onto the solid.
Step 2. In (b), a chemical bond is broken and formed: two molecules combine into one molecule, and can split back into two molecules. Since a new substance () forms from a different one (), this is a chemical equilibrium. The opposing processes are the forward combination and the reverse dissociation , and the colour stabilising (rather than fading to zero or deepening forever) is the experimental signal that the two rates have become equal.
Step 3. In (c), dissolved and ions are the same chemical species as the solid lattice, just separated — no new substance forms, so this is a physical equilibrium (dissolution). The opposing processes are dissolution of solid into ions, and crystallisation of ions back onto the solid.
Step 4. State the final classification. (a) Physical equilibrium (sublimation); (b) chemical equilibrium (dimerisation of ); (c) physical equilibrium (dissolution) — each one dynamic, each requiring the container to stay closed for the balance to be maintained.
Common traps
- Thinking equilibrium means "nothing is happening." Both forward and reverse processes continue at equal, non-zero rates; only the net, measurable change is zero.
- Believing equilibrium can be reached in an open system. An open system lets one side of the balance escape indefinitely, so the rates never converge — evaporation into open air never reaches true equilibrium.
- Confusing "equal amounts of reactant and product" with equilibrium. Equilibrium only requires equal rates; the actual amounts of the two sides at equilibrium are almost never equal to each other.
- Treating melting or boiling points as fixed numbers rather than equilibrium conditions. A melting or boiling point at a given pressure is precisely the temperature at which two phases coexist in equilibrium; change the pressure and that temperature changes too.
Ask the tutor: Ask the AI tutor to give you more sealed-vs-open scenarios to classify as physical or chemical equilibrium before you move on to the quantitative equilibrium constant.
Is dissolving a gas in a liquid, like carbon dioxide in a soft drink, really the same kind of equilibrium as ice melting?
Yes, both are physical equilibria — no new chemical substance is formed in either case. In the sealed bottle, dissolved carbon dioxide escapes back into the gas space at the same rate that gas dissolves into the liquid, exactly parallel to the melting-freezing balance in ice and water. The moment you open the bottle you break the closed system, gas escapes faster than it redissolves, and the fizz eventually goes flat, just as an open beaker of water never settles into a constant vapour pressure.
If equilibrium is dynamic, why do the concentrations or amounts look completely fixed when I measure them?
Because your measurements track the bulk, average properties of the system, not individual molecules. At equilibrium, roughly the same number of molecules cross from state A to state B as cross back from B to A in any given interval, so the total amount in each state stays constant even though the identities of the specific molecules on each side keep changing. It is the chemistry equivalent of a busy revolving door: the number of people inside a building can stay exactly constant while people keep walking in and out.
How is chemical equilibrium different from a reaction that has simply run out of reactants and stopped
A reaction that has run out of reactants is not at equilibrium at all — it has gone to completion, and there is no reverse process bringing it back. True equilibrium requires the reaction to be reversible, meaning both forward and reverse reactions can occur under the given conditions, and it requires a closed system so products cannot escape and keep participating in the reverse reaction. If products are removed as they form, or if the reaction genuinely cannot run backward, you get one-directional completion, not a dynamic balance.