Worked example 1
Predict the sign of ΔS for CaCO₃(s) → CaO(s) + CO₂(g).
Try it first: Count the moles of gas on each side.
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What you'll be able to do: Predict the sign of an entropy change and calculate ΔS from standard molar entropies.
Best after: Energy, Heat and the First Law
Enthalpy alone cannot explain why ice melts on a warm day or why gases mix without being pushed. The missing ingredient is entropy, a measure of how many ways the energy and particles can be arranged.
These are recommended, not required. You can start this lesson at any time.
Entropy is a measure of how many microscopic arrangements of position and energy give the same overall state. More available arrangements means higher entropy.
Describing it as disorder is a rough shorthand that fails for cases such as protein folding, so counting arrangements is the safer picture.
For the same substance, melting, vaporization and heating at fixed phase and ordinary constraints generally increase entropy. Dissolution and increases in gas moles often suggest an increase, but competing effects require a closer comparison. A large gas-mole change is often the leading qualitative clue, but tabulated entropies settle cases with competing effects.
Qualitative comparisons work best when other features are controlled. Vaporization of the same substance gives many more accessible configurations; compression of a gas at fixed temperature reduces them. Dissolving a salt releases lattice ions into the solvent, but ordering of surrounding water can offset that gain, so dissolution entropy is not always positive. When gas moles are unchanged, molecular complexity, phase and mixing can still matter. A memorized particle-count rule is not a replacement for the standard-entropy calculation.
Tabulated as S in J/mol K, these are absolute values rather than changes, because the third law sets the entropy of a perfect crystal at 0 K to exactly zero. Every substance above absolute zero therefore has a positive S, elements included.
Distinguish S for a whole sample, in J/K, from molar entropy Sₘ, in J/(mol·K). Standard molar values are scaled by stoichiometric amounts before subtracting. For N₂ + 3 H₂ → 2 NH₃, 2(192.8) − [191.6 + 3(130.7)] = −198.1 J/K for the stoichiometric batch, or −198.1 J/(mol reaction·K). Unlike formation enthalpies, elemental molar entropies at 298 K are not zero. A perfect ordered crystal at 0 K supplies the third-law reference, not an arbitrary zero assigned separately to each element.
ΔS(rxn) = S n S(products) - S n S(reactants)
A process is spontaneous when the total entropy of the universe increases. The system alone is allowed to become more ordered, as when water freezes, provided the surroundings gain more entropy than the system loses.
ΔS(universe) = ΔS(system) + ΔS(surroundings) > 0 for a spontaneous change
Heat released by an exothermic reaction spreads into the surroundings and raises their entropy, and it does so more effectively at low temperature. This is why exothermic reactions are so often spontaneous, and it is the idea the Gibbs equation packages up.
For a large thermal reservoir at T, ΔSsurr = qsurr/T. With constant-pressure reaction heat and only pressure-volume work, this becomes −ΔHsys/T. If ΔHsys = −10.0 kJ per reaction amount, ΔSsys = −20.0 J/K and T = 298 K, ΔSsurr = +10000/298 = +33.6 J/K, so ΔSuniv = −20.0 + 33.6 = +13.6 J/K. The system loses entropy but the total increases. Use reservoir temperature in kelvin and match joules with joules. At equilibrium the total entropy has no first-order increase for a permitted infinitesimal change; molecular exchange need not stop.
ΔS(surroundings) = -ΔH(system) / T
Two different ideal gases mixed at the same temperature occupy more accessible arrangements than when separated. Their mixing entropy is positive even if neither gas reacts and there is no net change in gas moles.
Entropy is not merely a count of gaseous particles; the number of ways to distribute distinct particles also matters.
Entropy for a sample has units J/K; standard molar entropy has units J/(mol·K). It reflects accessible microscopic states and energy distributions.
An increase in gas moles often suggests positive reaction entropy; calculate from data when other effects compete.
A perfect crystal at 0 K has zero entropy, which makes absolute entropies measurable.
For a spontaneous change the entropy of the universe increases.
Unlike ΔHf, standard molar entropies of elements are positive.
ΔS(rxn) = Σ n S(products) - Σ n S(reactants)
ΔS(surroundings) = -ΔH(system)/T
Predict the sign of ΔS for CaCO₃(s) → CaO(s) + CO₂(g).
Try it first: Count the moles of gas on each side.
0 of 2 steps revealed.
Calculate ΔS for N₂(g) + 3 H₂(g) → 2 NH₃(g) given S: N₂ = 191.6, H₂ = 130.7, NH₃ = 192.8 J/mol K.
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Water freezes at -10 C, yet the system becomes more ordered. Explain how this is consistent with the second law.
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A partition between equal amounts of N₂ and O₂ is removed in an insulated container. Predict the sign of ΔSmix.
Try it first: Think about the accessible positions of each type of molecule.
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| Mistake | Why it's wrong | Check instead |
|---|---|---|
| Assuming any process that orders the system violates the second law. | The law applies to the universe, not the system alone. | Include the surroundings term before judging spontaneity. |
| Combining S in J/mol K with ΔH in kJ/mol without converting. | The entropy term ends up 1000 times too large. | Convert entropy to kJ/mol K, or enthalpy to J/mol, before combining. |
| Giving elements a standard entropy of zero. | Only a perfect crystal at 0 K has zero entropy. | Look up the tabulated positive value for the element. |
| Predicting ΔS from the total number of particles rather than gas particles. | Gases carry far more entropy per mole than solids or liquids. | Count gas moles as an initial clue, then consider phases, mixing and tabulated entropy data. |
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After the lesson · Question bank
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Entropy describes the multiplicity of microscopic states and energy distributions. Phase, temperature, mixing and gas-mole changes guide qualitative predictions, while standard molar entropy data give a quantitative products-minus-reactants sum. Elemental entropies at ordinary temperatures are not assigned zero. Spontaneity requires positive total entropy change of system plus surroundings; the system alone may lose entropy.
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