Entropy and second law
Why does ice melt on a warm table but a puddle never spontaneously freezes into an ice cube while the room stays the same temperature? Both processes conserve energy, so the first law of thermodynamics is silent on the question — it cannot tell spontaneous from impossible. Something else decides the direction time's arrow runs in chemistry. That something is entropy , a state function measuring how disordered a system's arrangement of particles is, and the second law of thermodynamics, which says the total entropy of the universe never decreases in any real process. This article builds the qualitative feel for entropy — what makes it rise or fall — then turns the second law into a genuine calculation, using to judge spontaneity even when a reaction makes its own system more ordered.
A process is spontaneous only if it increases the total entropy of system plus surroundings, , so even an entropy-losing system can proceed spontaneously if it releases enough heat to raise the surroundings' entropy by more.
The core idea
Spontaneous processes need a second criterion beyond . A spontaneous process happens on its own, without continuous outside push, once it starts — spontaneity says nothing about how fast it happens, only that it can. Many spontaneous processes are exothermic (rusting, combustion), which tempted early chemists to think "exothermic means spontaneous." But ice melting above and many salts dissolving are spontaneous and endothermic. Enthalpy alone cannot be the whole story; a second quantity, entropy, is needed.
Entropy measures disorder, and it is a state function. depends only on the current state of the system, not on how it got there, so for any process
where: and are the entropies of the final and initial states. Because is a state function, for a reaction can be tracked just like , without worrying about path. Entropy rises whenever particles gain freedom to spread into more arrangements (more "microstates"):
- melting (solid to liquid) or vaporisation (liquid to gas) — molecules gain freedom of motion;
- a solid or liquid dissolving into solution — an ordered lattice disperses among solvent molecules;
- the number of moles of gas increasing in a reaction — more independent gas particles, more ways to arrange them;
- heating a substance — more thermal motion, more microstates become accessible.
The reverse of any of these — condensation, crystallisation, decreasing gas moles, cooling — tends to lower entropy.
The second law: total entropy of the universe increases for any spontaneous process.
where: is the entropy change of the reacting substances, is the entropy change of everything outside the system (the rest of the universe, in practice the immediate thermal environment), and is their sum. Equality holds only for an idealised reversible process at equilibrium; every real, spontaneous process makes strictly positive. This is the rigorous test for spontaneity — not alone. A system's own entropy can fall in a spontaneous process (water freezing below : the system becomes more ordered) provided the surroundings gain enough entropy to compensate (freezing releases heat, warming and disordering the surroundings by more than the system ordered itself).
Linking to heat flow. At constant pressure and temperature , the entropy the surroundings gain is tied directly to the heat the system releases:
where: is the enthalpy change of the system (negative for exothermic reactions) and is the absolute temperature in kelvin at which heat transfer occurs. An exothermic reaction () dumps heat into the surroundings, making positive; an endothermic reaction pulls heat from the surroundings, cooling and ordering them, so is negative. This one equation is what turns "entropy" from a qualitative disorder story into a number you can add to and compare against zero — the whole engine behind Worked example 2 below, and the qualitative seed of the later Gibbs free energy topic, which packages and of the system into a single criterion without needing explicitly.
The goal is to show, starting only from the second law and the heat-flow relation , that spontaneity at a given temperature can be judged entirely from the system's own and , without ever measuring the surroundings directly — the calculation used in every "is this reaction spontaneous" question in this unit.
Step 1. Start from the second law as the master criterion: a process is spontaneous when (and at equilibrium, ). This is the only rigorous test — it is defined in terms of the whole universe, system plus surroundings, not the system alone.
Step 2. Replace using the constant-pressure heat relation. Since heat leaving the system at constant equals , and that heat enters the surroundings at temperature , substitute into the second-law inequality: .
Step 3. Read off the two competing effects. The term is the system's own disorder change — favourable (positive) when moles of gas increase or a phase becomes less ordered. The term is favourable (positive) whenever the reaction is exothermic (). Spontaneity requires their sum to be positive: a strongly exothermic can outweigh an unfavourable (negative) , and vice versa a strongly positive can outweigh a mildly endothermic reaction.
Step 4. State the practical recipe. To test spontaneity at temperature : compute from the given (or measured) ; add it to the given ; if the sum is positive the process is spontaneous at that , if zero it is at equilibrium, and if negative it is non-spontaneous as written (the reverse process is spontaneous instead). This is exactly the check performed in Worked example 2 below.
Worked example
For a reaction at , and . Is it spontaneous at ?
Step 1. Convert to joules so units match : .
Step 2. Find using : .
Step 3. Add to get .
Step 4. Since , the reaction is spontaneous at , even though — the system itself becomes more ordered, but the large exothermic heat release drives up the surroundings' entropy by far more, and the total still increases. Answer: spontaneous, with .
Competitive stretch
At instead, , so — the borderline of equilibrium. Raising shrinks the favourable contribution, so a reaction comfortably spontaneous at can approach non-spontaneity at high if is negative — the temperature sensitivity the later Gibbs free energy criterion, , tracks directly.
Common traps
- Judging spontaneity from alone instead of — a system can lose entropy in a spontaneous process if the surroundings gain more.
- Confusing "spontaneous" with "fast." Spontaneity only says a process can occur on its own eventually; rate is a separate question belonging to chemical kinetics.
- Assuming all exothermic reactions are spontaneous or all endothermic ones are not — both and of the system, weighed together through , decide it.
- Dropping or flipping the sign in — an exothermic system () must give a positive , not negative.
- Forgetting to convert kJ to J (or vice versa) before adding (in J K⁻¹mol⁻¹) to — mismatched units silently corrupt the sum.
Ask the tutor: Want to work through more calculations, or check your sign conventions on a tricky exothermic-versus-endothermic problem?
If entropy always increases in the universe, why do ordered things like crystals or living cells ever form?
The second law only requires the total entropy of system plus surroundings to increase — it says nothing about the system alone. A crystal forming from solution, or a cell building complex molecules, is the system's entropy decreasing, which is allowed precisely because that process releases heat or otherwise pushes disorder into the surroundings by a larger amount. Add the two and the total still rises. Locally ordered pockets are common; globally, disorder always wins.
Why does ΔS surroundings use ΔH of the system and not some separate measurement of the surroundings?
At constant pressure, whatever heat the system releases or absorbs is exactly the heat the surroundings absorbs or releases, just with the opposite sign — energy is conserved between them. So the heat entering the surroundings is at constant . Dividing that heat by the (essentially constant) temperature of the surroundings gives their entropy change, without needing any separate calorimetry on the surroundings themselves.
Is it possible for a reaction to be spontaneous at one temperature and non-spontaneous at another?
Yes, and it is common whenever and favour opposite outcomes. Since shrinks as rises, an exothermic reaction with negative (favourable , unfavourable ) can be spontaneous at low but stop being spontaneous once grows large enough that the shrinking term can no longer outweigh the negative . This is exactly why melting and boiling points exist: below them one phase is favoured, above them the other is, with the crossover set by where .