Chemical Equilibrium
Senior 6 · Chemistry
Chemical Equilibrium
Lesson 1 of 5
25 min
Quicklime, calcium oxide, is made by heating limestone in a kiln:
Heat limestone to about 900 °C in a sealed steel box and something surprising happens: the decomposition runs only until the carbon dioxide in the box reaches a pressure of 1 atm, and then it stops. Part of the limestone stays unchanged however long you wait. At 1000 °C the limit is higher, 3.8 atm, but there is still a limit. In a kiln the carbon dioxide is carried away with the hot furnace gases, its pressure never builds up, and every lump of limestone is converted.
So the same reaction is "complete" in one container and "incomplete" in another. The reason is that carbon dioxide and calcium oxide also react with each other, re-forming calcium carbonate. This lesson explains what happens when a reaction can run both ways, and why, in a closed container, it settles into a state called dynamic equilibrium.

Definition
Reversible reaction: a reaction in which the products can react to re-form the reactants, so it can go in either direction. It is written with the sign . Example: .
Irreversible reaction: a reaction that, in practice, goes only forwards, either because a product escapes or because so little of the reactants can re-form that none can be detected. Example: .
Closed system: a system that no matter can enter or leave, although energy (heat) can. Example: a stoppered flask or a sealed steel vessel.
Dynamic equilibrium: the state of a reversible reaction in a closed system in which the forward and backward reactions go on at equal rates, so the concentrations of all the reactants and products stay constant.
Position of equilibrium: the proportions of reactants and products present at equilibrium. "The equilibrium lies to the right" means the mixture is mainly products.
Homogeneous equilibrium: one in which every species is in the same phase, e.g. . Heterogeneous equilibrium: one involving more than one phase, e.g. .
Table 1.1 lists reactions you have met before. Notice what decides whether a reaction "comes back".
| Reaction | What you observe | Type |
|---|---|---|
| Blue crystals turn white on heating; adding water to the white powder turns it blue again, and it gets hot. | reversible | |
| Heated in a test tube, the white solid disappears from the hot bottom and re-forms on the cool upper wall. | reversible | |
| A blood-red colour forms; adding more of either ion makes it deeper, adding a reagent that removes makes it fade. | reversible, homogeneous | |
| In an open beaker the hydrogen bubbles away; the magnesium is used up completely. | irreversible (open system) | |
| A white flame and white ash; the oxide does not decompose back on cooling. | irreversible (equilibrium lies very far to the right) |
Every reaction is reversible in principle. We call a reaction irreversible when a product leaves the system, or when the equilibrium lies so far to one side that the reverse reaction cannot be detected. The limestone example shows that one reaction can be either: reversible in a sealed box, irreversible in an open kiln.
Hydrogen and iodine vapour react at 430 °C to form hydrogen iodide, a colourless gas: . Two sealed flasks are kept at 430 °C.
Analysis of the two flasks gives the same final mixture: and . Both flasks contain the same numbers of hydrogen and iodine atoms per cubic decimetre, so whichever side you start from, the system ends in the same equilibrium state (Figure 1.1).
Figure 1.1: Concentration against time for at 430 °C, started from each side. The final concentrations are the same.
Why does the change stop? At the start of flask A only the forward reaction can happen, and it is fast because and are high. As they fall, the forward rate falls. Meanwhile HI builds up, so the backward reaction, , speeds up. When the two rates become equal, HI is made exactly as fast as it is used up, and no concentration changes any more (Figure 1.2). Both reactions are still running: that is why the equilibrium is called dynamic.
Figure 1.2: Rates of the forward and backward reactions against time. They become equal at equilibrium; neither falls to zero.
Constant concentrations alone could mean that the reaction had simply stopped. Radioactive tracers show that it has not. Add a trace of iodine labelled with radioactive iodine-131 to an equilibrium mixture of , and HI: the radioactivity soon appears in the hydrogen iodide as well, although the concentrations stay practically the same. Iodine atoms are still passing into HI and back out again.
Equilibria are not only chemical. Water in a sealed bottle reaches , with evaporation and condensation at equal rates. A saturated salt solution in contact with undissolved crystals reaches : a crystal with a chipped corner slowly changes shape while its mass stays the same. The partition of a solute between two immiscible solvents (Unit 6) is another physical equilibrium.
Worked example
Problem. Dinitrogen tetroxide, a colourless gas, dissociates into brown nitrogen dioxide: . A sealed flask at 60 °C initially contains only. These are illustrative readings:
| time / s | 0 | 20 | 40 | 60 | 80 | 100 |
|---|---|---|---|---|---|---|
| / | 0.0400 | 0.0300 | 0.0240 | 0.0220 | 0.0220 | 0.0220 |
(a) When is equilibrium reached? (b) Calculate at equilibrium. (c) What is happening to the molecules after 60 s?
Solution.
(a) The concentration stops changing at 60 s, so equilibrium is reached by 60 s (it may have been reached a little earlier; the readings cannot show exactly when).
(b) used up . Each gives two :
(c) molecules are still dissociating and molecules are still combining, at equal rates, so the brown colour stays constant.
Answer: equilibrium by 60 s; . Note that at equilibrium: constant does not mean equal.
Worked example
Problem. 50.0 g of calcium carbonate is sealed in an evacuated 10.0 dm³ steel vessel and heated to 1000 °C, where the equilibrium pressure of carbon dioxide over and CaO is 3.8 atm. (a) What mass of decomposes? (b) What would happen with 20.0 g instead? Ignore the volume of the solids; , 1 atm = 101 325 Pa, .
Solution.
(a) Amount of needed to reach 3.8 atm, from :
One mole of gives one mole of , so mass decomposed (2 s.f., because 3.8 atm has 2 s.f.). About 14 g of limestone remains, in equilibrium with CaO and the gas.
(b) 20.0 g is only . Even if all of it decomposed, the pressure would be
This is below 3.8 atm, so the equilibrium pressure is never reached.
Answer: (a) 36 g decomposes. (b) All 20.0 g decomposes: a heterogeneous equilibrium exists only while some of every phase, here solid , is present.
Warning
Three common mistakes
Tip
When a question asks you to describe dynamic equilibrium, an examiner looks for three points: closed system; rate of forward reaction = rate of backward reaction; concentrations constant. Learn them as one sentence: "In a closed system, the forward and backward rates are equal, so the concentrations stay constant."
University of Surrey: Dynamic Equilibrium. The animation shows water molecules evaporating and condensing in a closed container. Watch how the two rates become equal, so that the amount of vapour stays constant while molecules keep moving both ways.
Practice
Sources and credits