Chemical energetics (A Level)Cambridge International AS & A Level Chemistry 9701 · A Level topic 23
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Cambridge International AS & A Level Chemistry 9701 · A Level topic 23

Chemical energetics

What this chapter covers23.1–23.4

Sodium burns in chlorine with a brilliant yellow flame and leaves a white crust of salt. Magnesium ribbon flares white in air and crumbles to magnesium oxide. Both reactions are strongly exothermic, and both produce ionic solids. Yet every step that turns a metal atom into a positive ion costs energy, and removing the second electron from magnesium costs almost twice as much as removing the first. Something in the formation of an ionic solid must repay those costs with interest. This chapter identifies that something — the lattice energy — and shows how it is measured, even though it can never be measured directly.

The chapter then asks two further questions that ordinary enthalpy changes cannot answer. Why do some salts, such as ammonium nitrate or potassium chloride, dissolve readily even though dissolving them makes the solution colder? And why does calcium carbonate refuse to decompose at room temperature but decompose steadily in a lime kiln, even though the enthalpy change hardly alters between the two temperatures? The answers need a second quantity, entropy, and a way of combining it with enthalpy, the Gibbs free energy change.

What topic 23 asks you to do

23.1 Lattice energy and Born–Haber cycles — define and use the enthalpy change of atomisation and the lattice energy; define and use first electron affinity, explain what affects it and the trends in Groups 16 and 17; construct and calculate with Born–Haber cycles for solids containing +1 and +2 cations and −1 and −2 anions; explain qualitatively how ionic charge and ionic radius affect the size of a lattice energy.

23.2 Enthalpies of solution and hydration — define and use ΔHhyd and ΔHsol; construct and calculate with the cycle linking them to the lattice energy; explain how ionic charge and radius affect ΔHhyd.

23.3 Entropy change, ΔS — define entropy as the number of possible arrangements of the particles and their energy; predict and explain the sign of ΔS for changes of state, temperature changes and reactions that change the number of gas molecules; calculate ΔS° from standard entropies.

23.4 Gibbs free energy change, ΔG — state, use and calculate with ΔG° = ΔH° − TΔS°; judge feasibility from the sign of ΔG; predict how temperature changes feasibility.

What you are assumed to know already

  • Enthalpy change, exothermic and endothermic, standard conditions (298 K and 101 kPa) and standard states.
  • Enthalpy changes of formation and combustion, bond energies, and Hess's law, including energy cycles and energy-level diagrams.
  • Ionic bonding and the giant ionic lattice; first and successive ionisation energies and the factors that control them (nuclear charge, distance, shielding).
  • Ionic radius trends: cations are smaller than their atoms, anions larger; ions get larger down a group.

The one idea that organises the first half of the chapter

Every quantity in 23.1 and 23.2 is an enthalpy change for a precisely defined process, and every calculation is Hess's law. If you can write the equation that a term refers to — with the right amounts and the right state symbols — the arithmetic almost always takes care of itself. Nearly every mark lost in this topic is lost by writing the wrong process: the wrong number of moles, gaseous ions where there should be gaseous atoms, or an ion where there should be an atom.

Enthalpy change of atomisation23.1.1(a)

The first step in building an ionic solid from its elements is to turn each element into separate gaseous atoms. For a metal this means pulling the atoms out of the metallic lattice; for a non-metal such as chlorine it means breaking the covalent bonds in the diatomic molecules.

Definition

The standard enthalpy change of atomisation, ΔHat⊖, is the enthalpy change when one mole of gaseous atoms is formed from the element in its standard state under standard conditions.

Na(s) → Na(g)   ΔHat⊖ = +107 kJ mol−1     ½Cl2(g) → Cl(g)   ΔHat⊖ = +121 kJ mol−1

Two features of the definition are worth fixing now. First, the quantity is defined per mole of atoms produced, not per mole of element used. For chlorine, one mole of Cl atoms comes from half a mole of Cl2 molecules, so ΔHat for chlorine is half the Cl–Cl bond energy: 242 ÷ 2 = 121 kJ mol−1. For oxygen, atomisation is half the O=O bond energy, ½ × 496 = +248 kJ mol−1. Second, atomisation is always endothermic. Whatever holds the atoms together — metallic bonding, covalent bonds, or the intermolecular forces in solid iodine or liquid bromine — has to be overcome, and that always requires energy.

Exam alert — bromine and iodine

The standard state of bromine is a liquid and of iodine a solid. Atomising them therefore involves two processes: turning Br2(l) or I2(s) into gaseous molecules, then breaking the bond. When a question gives the enthalpy change of sublimation of iodine and the I–I bond energy separately, both belong in the cycle. Work out how many moles of I2 the formula needs: for ZnI2 that is one mole, so the full sublimation enthalpy and the full I–I bond energy are used; for NaI it would be half of each. In one examination cycle for a metal iodide, the commonest wrong answer came from leaving out the sublimation step.

Lattice energy23.1.1(b)

An ionic solid is a regular three-dimensional array of oppositely charged ions. Each ion is attracted by all the oppositely charged neighbours around it and repelled by the similarly charged ions a little further away; the net effect is a large attraction that holds the lattice together. The lattice energy measures how much energy is released when that lattice assembles from free ions.

Definition

The lattice energy, ΔHlatt⊖, is the enthalpy change when one mole of an ionic compound is formed from its gaseous ions under standard conditions.

Na+(g) + Cl−(g) → NaCl(s)   ΔHlatt⊖ = −787 kJ mol−1
Mg2+(g) + 2Cl−(g) → MgCl2(s)   ΔHlatt⊖ = −2493 kJ mol−1

Lattice energy defined this way is always exothermic: oppositely charged ions attract, and energy is released as they come together. The more negative the value, the more strongly the ions are held.

Look carefully at the equation for MgCl2. One mole of compound is formed from one mole of Mg2+ ions and two moles of Cl− ions. It is therefore wrong to say that lattice energy is "formed from one mole of gaseous ions"; the one mole refers to the compound. Examiners have reported both errors — omitting "one mole" altogether, and attaching it to the ions instead of the compound.

Common trap — the direction of the process

Some books define lattice energy (or "lattice enthalpy") the other way round, as the endothermic change when one mole of solid is separated into gaseous ions. That quantity has the same size and the opposite sign. In this syllabus the lattice energy always refers to formation of the solid from gaseous ions, and so is always negative. If you meet a value of +787 kJ mol−1 labelled "lattice dissociation", reverse its sign before putting it into a formation cycle.

Lattice energy cannot be measured directly, because there is no practical way of assembling a mole of gaseous ions into a crystal and catching the heat released. It is found indirectly, by Hess's law, from quantities that can be measured — which is what a Born–Haber cycle does.

First electron affinity23.1.2(a)

Forming the anions in an ionic solid means adding electrons to gaseous non-metal atoms. The energy change for this is the electron affinity.

Definition

The first electron affinity, EA1, is the enthalpy change when one mole of electrons is added to one mole of gaseous atoms to form one mole of gaseous 1− ions.

Cl(g) + e− → Cl−(g)   EA1 = −349 kJ mol−1
O(g) + e− → O−(g)   EA1 = −141 kJ mol−1

The definition mirrors that of ionisation energy, and examiners regularly report candidates confusing the two. The distinction is simply the direction: ionisation energy removes an electron from a gaseous atom and is always endothermic; electron affinity adds an electron to a gaseous atom. Both are defined per mole of gaseous atoms, and both require the gaseous state.

For most non-metals the first electron affinity is exothermic. The incoming electron is attracted by the nucleus of the neutral atom, because the atom's own electrons do not completely shield the nuclear charge from an electron arriving at the outer shell. Energy is released as it is captured.

Second electron affinity

Oxide and sulfide ions carry a 2− charge, so forming them needs a second electron to be added:

O−(g) + e− → O2−(g)    EA2 = +798 kJ mol−1

The second electron affinity is endothermic, and large. The electron is now being added to a species that is already negatively charged, so it is repelled; energy must be supplied to force it on. This is why, in a Born–Haber cycle for an oxide, the total energy needed to make O2−(g) from O(g) is strongly positive (−141 + 798 = +657 kJ mol−1). The oxide ion exists in solids only because the very large lattice energy of a 2+/2− lattice more than repays that cost.

O(g)e−neutral atom attracts the electron:EA1 = −141 kJ mol−1 (exothermic)O−(g)e−repulsionnegative ion repels the electron:EA2 = +798 kJ mol−1 (endothermic)
Figure 23.1 The first electron affinity of oxygen is exothermic because the neutral atom attracts the incoming electron; the second is endothermic because the O− ion repels it.
AnimationWhat a Born–Haber cycle is
Follow the formation of sodium chloride broken into steps: atomising each element, ionising sodium, adding an electron to chlorine, and finally assembling the lattice. Notice which arrows point up and which point down.
Follow the formation of sodium chloride broken into steps: atomising each element, ionising sodium, adding an electron to chlorine, and finally assembling the lattice. Notice which arrows point up and which point down.

What affects electron affinity: Groups 16 and 1723.1.2(b), (c)

The size of a first electron affinity depends on how strongly the nucleus attracts an electron arriving at the outer shell. The same three factors that govern ionisation energy are at work, and they act in the same directions:

Down Group 17

From chlorine to bromine to iodine, the first electron affinity becomes less exothermic (−349, then about −325, then about −295 kJ mol−1). Nuclear charge rises, but each step adds a complete inner shell. The incoming electron enters a shell further from the nucleus and is better shielded, so it is attracted less strongly and less energy is released when it is captured.

+e−distanceCl+e−distanceBr+e−distanceImore inner shells, larger atom → incoming electron further from the nucleus and better shieldedweaker attraction → less energy released → first electron affinity less exothermic down the group
Figure 23.2 Down Group 17 the incoming electron enters a shell further from the nucleus and is shielded by more inner shells, so it is attracted less and the first electron affinity becomes less exothermic.

Down Group 16

Sulfur, selenium and tellurium follow the same pattern for exactly the same reason: from S to Te the first electron affinity becomes less exothermic as the atoms get larger and the incoming electron is further from, and better shielded from, the nucleus.

The exceptions at the top of each group

Fluorine's first electron affinity (−328 kJ mol−1) is less exothermic than chlorine's, and oxygen's (−141 kJ mol−1) is less exothermic than sulfur's. Fluorine and oxygen atoms are very small, so their outer shells are crowded. An electron added to such a small shell is close to the electrons already there and is strongly repelled by them; that repulsion offsets part of the attraction of the nucleus. From the second member of each group onwards, the larger outer shell relieves this crowding, and the ordinary trend takes over.

Across a period

Comparing elements in the same period isolates the effect of nuclear charge. Carbon's first electron affinity is only −120 kJ mol−1, fluorine's −328 kJ mol−1. The electron is added to the same shell in each case, with the same shielding, but fluorine has three more protons, so the attraction for the incoming electron is much greater. Examiners report that candidates often try to explain this difference in terms of electronegativity; the answer that earns the mark is the greater nuclear charge of fluorine and its greater attraction for the added electron.

Exam language — describe trends in energy terms

Say "becomes less exothermic" or "less negative", not "decreases". A value that goes from −349 to −295 has increased numerically, so "decreases" is ambiguous and examiners have specifically reported it as a way candidates lost marks on this trend.

Quick check 23.1

  1. Write the equation, with state symbols, for the first electron affinity of sulfur.
    answer
    S(g) + e− → S−(g)
  2. Write the equation for the lattice energy of calcium fluoride.
    answer
    Ca2+(g) + 2F−(g) → CaF2(s)
  3. Why is ΔHat of chlorine equal to half the Cl–Cl bond energy?
    answer
    Atomisation forms one mole of Cl atoms, which needs only half a mole of Cl2 bonds to be broken.
  4. State one reason why the second electron affinity of sulfur is endothermic.
    answer
    The electron is added to a negative ion (S−), which repels it, so energy must be supplied.

Constructing a Born–Haber cycle23.1.3

A Born–Haber cycle is a Hess's law cycle, usually drawn as an energy-level diagram, that links the enthalpy change of formation of an ionic solid to the lattice energy through a series of steps, each of which can be measured. The formation of the solid from its elements can happen by two routes that start and finish in the same place:

By Hess's law the two routes have the same total enthalpy change. For a compound Ma+Xb−:

ΔHf = ΔHat(metal) + ΔHat(non-metal) + ΣIE(metal) + ΣEA(non-metal) + ΔHlatt

with each term multiplied by the number of moles the formula requires.

Drawing the energy-level diagram

The diagram is built from the bottom-left. A horizontal line represents the elements in their standard states, at zero. Every endothermic step is drawn as an arrow pointing up to a new, higher line; every exothermic step as an arrow pointing down. On every line you write the species present at that stage, with state symbols, so that the atoms and electrons balance on every level. The last arrow, the lattice energy, runs a long way down from the gaseous ions to the ionic solid, and the formation arrow joins the elements directly to the solid.

ΔHat(K) +90ΔHat(F) +79IE1(K) +418EA1(F) −348ΔHlatt −802ΔHf −563K+(g) + e− + F(g)K+(g) + F−(g)K(g) + F(g)K(g) + ½F2(g)K(s) + ½F2(g)KF(s)vertical scale approximate
Figure 23.3 Born–Haber cycle for potassium fluoride. Endothermic steps (red) point up, exothermic steps (blue) point down. The species on each level balance: every electron removed from potassium appears on the line until fluorine accepts it. Values in kJ mol−1.

What earns the marks when you complete a cycle

  • Every species on the correct level, with its state symbol. Published marking awarded one mark for every few correct species and required all of them for full credit.
  • Electrons shown on the line after each ionisation, and removed only when the electron affinity step uses them. Omitting an electron from the level after an ionisation step is a reported error.
  • Atoms, not molecules, after atomisation. Writing S2(g) on the level after atomising sulfur is another reported error: atomisation gives S(g).
  • Arrows in the right direction and labelled with the process, not just a number.
AnimationBuilding a Born–Haber cycle step by step
Construct the cycle for sodium chloride one level at a time. Before each step appears, decide whether its arrow will point up or down and which species will be on the new level.
Construct the cycle for sodium chloride one level at a time. Before each step appears, decide whether its arrow will point up or down and which species will be on the new level.

Cycles with doubly charged ions

For compounds of a Group 2 metal the metal must lose two electrons, so both the first and second ionisation energies appear. For an oxide or sulfide the non-metal must gain two electrons, so both electron affinities appear — the first exothermic, the second endothermic. The magnesium oxide cycle below shows both features. Notice how far above the elements the gaseous ions sit: 3239 kJ mol−1 must be put in to make Mg2+(g) and O2−(g) from the elements. The lattice energy repays all of that and a further 602 kJ mol−1, which is why MgO is stable.

ΔHat(Mg) +148IE1(Mg) +736IE2(Mg) +1450ΔHat(O) +248EA1(O) −141EA2(O) +798ΔHlatt = ?ΔHf −602Mg2+(g) + O2−(g)Mg2+(g) + 2e− + O(g)Mg2+(g) + e− + O−(g)Mg2+(g) + 2e− + ½O2(g)Mg+(g) + e− + ½O2(g)Mg(g) + ½O2(g)Mg(s) + ½O2(g)MgO(s)vertical scale approximate
Figure 23.4 Born–Haber cycle for magnesium oxide, showing both ionisation energies of magnesium and both electron affinities of oxygen; EA2 points up because it is endothermic. Values in kJ mol−1; the lattice energy is calculated in Worked example 23.2.

Calculations with Born–Haber cycles23.1.4

Because the cycle is closed, any one unknown term can be calculated from the others. The method is always the same: write the Hess's law sum along the two routes, substitute every value with its own sign, multiply by the number of moles each step involves, and solve for the unknown.

Worked example 23.1 · Lattice energy of potassium fluoride

Question. Use the data to calculate the lattice energy of KF: ΔHf(KF) = −563; ΔHat(K) = +90; ΔHat(F) = +79; IE1(K) = +418; EA1(F) = −348 (all in kJ mol−1).

GivenΔHf and every step to K+(g) + F−(g); one mole of each ion per KF.
FindΔHlatt(KF): K+(g) + F−(g) → KF(s)
RelationshipΔHf = ΔHat(K) + ΔHat(F) + IE1(K) + EA1(F) + ΔHlatt
Substitution−563 = (+90) + (+79) + (+418) + (−348) + ΔHlatt
CalculationΔHlatt = −563 − 239 = −802
AnswerΔHlatt(KF) = −802 kJ mol−1
CheckNegative, as a lattice energy must be; larger in magnitude than ΔHf, because the lattice energy has to repay the +239 kJ mol−1 needed to make the gaseous ions as well as supply the −563 released overall.

Worked example 23.2 · Lattice energy of magnesium oxide (two electrons transferred)

Question. ΔHf(MgO) = −602; ΔHat(Mg) = +148; IE1(Mg) = +736; IE2(Mg) = +1450; O=O bond energy = +496; EA1(O) = −141; EA2(O) = +798 (kJ mol−1). Calculate ΔHlatt(MgO).

GivenA bond energy, not an atomisation enthalpy, for oxygen. MgO contains one O atom, so only half a mole of O=O bonds is broken.
FindΔHlatt: Mg2+(g) + O2−(g) → MgO(s)
RelationshipΔHf = ΔHat(Mg) + IE1 + IE2 + ½E(O=O) + EA1 + EA2 + ΔHlatt
Substitution−602 = 148 + 736 + 1450 + 248 + (−141) + 798 + ΔHlatt
Calculationsum of steps = +3239; ΔHlatt = −602 − 3239 = −3841
AnswerΔHlatt(MgO) = −3841 kJ mol−1
CheckAbout five times the KF value, which is what doubled charges on both ions should roughly give (see the section on what controls the size of a lattice energy). Using the full 496 for oxygen, or leaving out EA2, would each give a wrong answer that still looks plausible — so write down which values you used and why.

The same cycle can be run backwards to find a quantity that is hard to measure. Electron affinities, in particular, are often obtained this way from a lattice energy that has been calculated independently.

Worked example 23.3 · An electron affinity from a cycle

Question. For lithium fluoride: ΔHf = −594.1; atomisation of lithium = +155.2; ½ × F–F bond energy = +75.3; IE1(Li) = +520; ΔHlatt = −1017 kJ mol−1. Calculate EA1 of fluorine.

RelationshipΔHf = ΔHat(Li) + ΔHat(F) + IE1(Li) + EA1(F) + ΔHlatt
Substitution−594.1 = 155.2 + 75.3 + 520 + EA1 + (−1017)
CalculationEA1 = −594.1 − 155.2 − 75.3 − 520 + 1017 = −327.6
AnswerEA1(F) ≈ −328 kJ mol−1
CheckExothermic, and slightly less exothermic than chlorine's −349 kJ mol−1, as expected for the crowded outer shell of fluorine.

The four errors that account for most lost marks

1 · Missing multipliers. In CaCl2, two moles of Cl atoms are formed and two moles of electrons added: both ΔHat(Cl) and EA(Cl) are multiplied by 2. Reports on several sessions list answers that doubled only one of the pair.

2 · Bond energy versus atomisation. One mole of Cl atoms needs ½ × E(Cl–Cl). For CaCl2 you need 2 × ΔHat(Cl) = 1 × E(Cl–Cl). Decide from the formula how many atoms you need, then how many bonds that means.

3 · Signs. Substitute each value with its own sign and keep brackets around negatives. Reported answers include the right number with the wrong sign, obtained by writing +208 for a formation enthalpy of −208.

4 · Irrelevant data. Questions deliberately include values you do not need — the first ionisation energy of iodine, or the O–O single-bond energy alongside O=O. Selecting the right data is part of what is being tested; examiners describe many candidates as finding this selection difficult.

AnimationComplete a Born–Haber cycle, then use it
Fill in the levels of a cycle, then use the data to calculate an enthalpy of formation. Work each one on paper before checking.
Fill in the levels of a cycle, then use the data to calculate an enthalpy of formation. Work each one on paper before checking.
AnimationBorn–Haber cycle questions
A set of ten calculations: lattice energies, formation enthalpies and electron affinities from cycles. Write the Hess's law sum before substituting each time.
A set of ten calculations: lattice energies, formation enthalpies and electron affinities from cycles. Write the Hess's law sum before substituting each time.
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What controls the size of a lattice energy23.1.5

Lattice energy comes from electrostatic attraction between oppositely charged ions. The force between two charges is proportional to the product of the charges and falls off with the distance between their centres. Two properties of the ions therefore control the size of a lattice energy:

The two effects are often combined in the phrase charge density: a small, highly charged ion has a high charge density and forms strong ionic bonds.

0 1000 2000 3000 4000 m a g n i t u d e   o f   l a t t i c e   e n e r g y   /   k J   m o l   ( a l l   v a l u e s   n e g a t i v e ) − 1 LiF KF NaCl KCl Z n C l 2 M g C l 2 C a C l 2 ZnO CaO SrO −1 022 −802 −787 −701 −2 734 −2 493 −2 237 −3 971 −3 513 −3 310 charges 1+ / 1− charges 2+ / 1− charges 2+ / 2−
Figure 23.5 Lattice energies grouped by the charges on the ions. Charge dominates: every 2+/2− compound has a far more exothermic value than every 1+/1− compound. Within a group of the same charges, smaller ions give the more exothermic value — LiF > KF, and KF > KCl. Values in kJ mol−1, as quoted in examination questions and in this chapter.

Reading the data

Compare NaCl (−787) with MgO. Both have the same arrangement of ions, and Mg2+ and O2− are similar in size to Na+ and Cl−, but the charge product rises from 1 to 4 and the lattice energy rises nearly five-fold. Within compounds of the same charges the differences are smaller and come from size: LiF is more exothermic than KF because Li+ is smaller than K+; KF is more exothermic than KCl because F− is smaller than Cl−; CaO is more exothermic than SrO because Ca2+ is smaller than Sr2+.

What a full-credit comparison contains

Three things, in a chain: (1) the property of the ions that differs — "Mg2+ is smaller than K+ and has a greater charge"; (2) the consequence — "so there is greater attraction between the ions" or "stronger ionic bonds"; (3) the conclusion — "so the lattice energy of MgCl2 is more exothermic". Examiners repeatedly report answers that give (1) and (3) but never mention the attraction between the ions. Talking about "stronger nuclear attraction" is a different, and wrong, idea: lattice energy is about ion–ion attraction, not the nucleus of one atom attracting its own electrons.

Name the ion, and avoid "it"

In a comparison of BaSO4 and Cs2SO4, an examiner commented that it was often impossible to tell whether "it" referred to BaSO4, Cs2SO4, the Ba2+ ion or the Cs+ ion. Name the species every time.

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Why the formula is MgCl2 and not MgCl

Removing the second electron from magnesium costs 1450 kJ mol−1, so on ionisation energies alone "MgCl", containing Mg+, would be cheaper to make. But the lattice of MgCl2, built from a 2+ ion, is so much more exothermic (−2493 kJ mol−1) than any lattice built from Mg+ that the extra ionisation energy is more than repaid, and the overall enthalpy change of formation is far more negative. The formula of an ionic compound is the one that gives the most exothermic overall result — and the lattice energy is usually the deciding term. The same reasoning explains why sodium does not form NaCl2: the second ionisation energy of sodium removes an electron from a full inner shell and is enormous, far more than any extra lattice energy could repay.

Past-paper practice · Set 23A · Lattice energy, electron affinity and Born–Haber cycles

Examination questions on this part of the unit. Try each one on paper before opening the answer.

Question 23A.1[4]
question 23A.1
Answer and marking guidance
(a)(i) Energy released when one mole of an ionic compound is formed ✔ from its gaseous ions (under standard conditions) ✔. (ii) Ca2+ and O2− have higher charges / higher charge density than Li+ and F− ✔ — the answer must refer to the charges of both ions. (iii) MgO −3600 or more negative AND BaO −3200 or less negative ✔ (both needed). Examiner insight: the definition was generally well answered; the errors were omitting "1 mole" of compound and writing "1 mole of gaseous ions". Part (ii) was found difficult because answers did not address the charges of both ions.
Question 23A.2[9]
question 23A.2
Answer and marking guidance
(a)(i) Enthalpy (energy) change ✔ when one mole of electrons ✔ is gained by one mole of gaseous atoms ✔ — two points for one mark, all three for two marks. (ii) Energy is needed to overcome the repulsion between the electron and the negative ion ✔. (iii) Becomes less negative (less exothermic) down the group ✔; the added electron is further from the nucleus / atomic radius larger / more shielding, so less attraction between the nucleus and the incoming electron ✔. (b) −208 = 131 + 906 + 1733 + 62 + 151 + 2x − 2605 ✔ (the seven correct values); 2x = −586 ✔ (EA used twice); x = −293 kJ mol−1 ✔. (c) First box: less negative ✔, because Cd2+ is larger / has lower charge density, so the attraction between the ions is weaker. Examiner insight: common errors in (b) were −586 (no division by 2), −262 (sublimation enthalpy of iodine omitted), and sign errors such as +293 or −85 (using +208). In (c) most chose the right box but gave no reasoning about the larger Cd2+ attracting I− less strongly; in (a)(iii) many did not state that the attraction between the nucleus and the incoming electron decreases.
Question 23A.3[8]
question 23A.3
Answer and marking guidance
(a) Bond energy: always positive; atomisation: always positive; formation: can be either ✔. (b) Enthalpy change when one mole of gaseous atoms is formed ✔ from the element in its standard state under standard conditions ✔. (c) −31 = 2(285) + 2(731) + (−141) + 798 + ½(496) + x ✔ (the six correct values, with 2 × for silver and ½ × for O=O) ✔; x = −2968 kJ mol−1 ✔. Ag's second ionisation energy, the O–O bond energy and the first ionisation energy of oxygen are not used. (d) least exothermic Ag2Se, then Ag2S, most exothermic Ag2O ✔; the anion radius increases (charge density decreases) from O2− to Se2−, so attraction between the ions decreases ✔. Examiner insight: a common error in (a) was claiming that the enthalpy change of formation is always negative. In (b) errors included "one mole of gaseous ions" and omitting "one mole". In (d) many identified that O2− is smallest but did not say this gives greater attraction between the ions in Ag2O.
Question 23A.4[7]
question 23A.4
Answer and marking guidance
(ii) Each species on the correct line, with state symbols: Zn(s) + S(s) on the level from which ΔHf starts; Zn(g) + S(s) after ΔHat(Zn); Zn(g) + S(g) after ΔHat(S); Zn+(g) + S(g) + e− after IE1. That is eight species plus the electron: any three for one mark, any six for two, all nine for three. (iii) First EA becomes less negative (less exothermic) from S to Te ✔; atomic radius increases / more shielding ✔; so less attraction for the incoming electron ✔ — two points one mark, three points two marks. (iv) O2− has the same charge as S2− but is smaller ✔, so there is greater attraction between Zn2+ and O2− / stronger ionic bonds ✔. Examiner insight: in (ii) common errors were writing S2(g) and omitting an electron after IE1; in (iii) some used the ambiguous word "decreases"; in (iv) some wrongly referred to stronger nuclear attraction instead of attraction between the ions.
Question 23A.5[6]
question 23A.5
Answer and marking guidance
(c) Use of 2 × (−348) for EA(F) and +158 for the F–F bond energy ✔; use of +147, +736 and +1450 for magnesium ✔; ΔHlatt = −1102 − (147 + 158 + 736 + 1450 − 696) = −2897 kJ mol−1 ✔. Note that two F atoms need one F–F bond broken, so 158 is used once. (d)(i) Energy change when one electron is added ✔ to each atom in one mole ✔ of gaseous atoms. (ii) F has the greater nuclear charge (more protons) AND so a greater attraction between the nucleus and the added electron ✔. Examiner insight: errors in (c) came from wrong multipliers: −3245 (1 × 348), −3166 (1 × 348 and ½ × 158), −3055 (2 × 158). In (d)(ii) a common wrong answer was an explanation in terms of electronegativity.

Enthalpy change of solution and enthalpy change of hydration23.2.1

Drop anhydrous calcium chloride into water and the beaker becomes noticeably warm; dissolve ammonium nitrate and it becomes cold enough to feel through the glass. In both cases an ionic lattice is being taken apart, which on its own would absorb a very large amount of energy — the reverse of the lattice energy. The ions do not end up as free gaseous ions, however. Each one becomes surrounded by water molecules, and that process releases energy. Whether dissolving is exothermic or endothermic depends on which of these two large quantities is bigger.

Water molecules are polar. The oxygen atom carries a partial negative charge and lone pairs; the hydrogen atoms carry partial positive charges. Around a cation the water molecules orient with their oxygen atoms inwards; around an anion they orient with hydrogen atoms inwards. These ion–dipole attractions are what release energy when an ion is hydrated.

Definitions

The enthalpy change of hydration, ΔHhyd⊖, is the enthalpy change when one mole of a specified gaseous ion dissolves in sufficient water to form an infinitely dilute solution.

Na+(g) → Na+(aq)   ΔHhyd⊖ = −405 kJ mol−1    Cl−(g) → Cl−(aq)   ΔHhyd⊖ = −364 kJ mol−1

The enthalpy change of solution, ΔHsol⊖, is the enthalpy change when one mole of an ionic solid dissolves in sufficient water to form an infinitely dilute solution.

NaCl(s) → Na+(aq) + Cl−(aq)   ΔHsol⊖ = +18 kJ mol−1

"Infinitely dilute" means that so much water is used that adding more produces no further enthalpy change: every ion is fully surrounded by water and the ions are too far apart to interact with one another. Both definitions involve dissolving in water; published marking required that idea in both, and examiners noted that answers which left it out of either definition lost the mark.

Common trap — which enthalpy is "always" what

When a question asks you to classify lattice energy, enthalpy change of hydration and enthalpy change of solution as always positive, always negative or either, the answers are: lattice energy always negative, hydration always negative, solution either. Examiners report that candidates placed lattice energy and solution correctly but found hydration more difficult. If you remember that hydration only makes attractions, its sign follows.

The solution energy cycle23.2.2, 23.2.3

Dissolving an ionic solid can be imagined as taking place in two stages, which together start and finish in the same place as the direct process:

  1. The lattice is separated into gaseous ions. This is the reverse of the lattice energy, so its enthalpy change is −ΔHlatt, a large positive number.
  2. The gaseous ions are hydrated. The enthalpy change is the sum of the hydration enthalpies of all the ions in the formula — negative.

By Hess's law:

ΔHsol = −ΔHlatt + ΣΔHhyd(ions)

which is often written in the equivalent form ΔHlatt + ΔHsol = ΣΔHhyd, obtained by going round the cycle the other way: gaseous ions → solid → solution gives the same total as gaseous ions → solution directly.

Na+(g) + Cl−(g)NaCl(s)Na+(aq) + Cl−(aq)−ΔHlatt = +787ΔHhyd(Na+) + ΔHhyd(Cl−)= (−405) + (−364) = −769ΔHsol = +787 − 769 = +18
Figure 23.6 Energy cycle for dissolving sodium chloride. Breaking up the lattice needs +787 kJ mol−1; hydrating the two ions releases 769 kJ mol−1. The small difference, +18 kJ mol−1, is the enthalpy change of solution. Values from the text.

The NaCl cycle makes a point that recurs: ΔHsol is usually the small difference between two very large numbers. A modest change in either the lattice energy or the hydration enthalpies can switch dissolving from exothermic to endothermic. That is why the sign of ΔHsol cannot be predicted by inspection, and why it alone does not decide whether a salt dissolves (the entropy change, discussed later in this chapter, matters as well).

Worked example 23.4 · Enthalpy change of solution of sodium chloride

GivenΔHlatt(NaCl) = −787; ΔHhyd(Na+) = −405; ΔHhyd(Cl−) = −364 kJ mol−1
FindΔHsol: NaCl(s) → Na+(aq) + Cl−(aq)
RelationshipΔHsol = −ΔHlatt + ΔHhyd(Na+) + ΔHhyd(Cl−)
SubstitutionΔHsol = −(−787) + (−405) + (−364)
AnswerΔHsol = +18 kJ mol−1
CheckSlightly endothermic: a solution of salt cools very slightly as it forms. The answer is small compared with the terms, which is typical.

Worked example 23.5 · A hydration enthalpy from the cycle, for a 1:2 salt

Question. For a salt MX2: ΔHlatt = −2500; ΔHsol = −100; ΔHhyd(M2+) = −1900 kJ mol−1. Calculate ΔHhyd(X−). (Illustrative values.)

RelationshipΔHsol = −ΔHlatt + ΔHhyd(M2+) + 2ΔHhyd(X−)
Substitution−100 = +2500 + (−1900) + 2x
Calculation2x = −100 − 2500 + 1900 = −700; x = −350
AnswerΔHhyd(X−) = −350 kJ mol−1
CheckThe cycle gives the hydration enthalpy of two moles of X−; the definition is per mole of ion, so divide by 2. Reports on two recent sessions name the missing division as the commonest error (for example −670 instead of −335 in a calcium chloride question).
AnimationCalculating an enthalpy of solution
Sodium chloride dissolves by an indirect route: first the lattice is broken into gaseous ions, then the ions are hydrated. Note that the first stage is labelled as lattice dissociation with a positive value — the reverse of the lattice energy as defined in this syllabus.
Sodium chloride dissolves by an indirect route: first the lattice is broken into gaseous ions, then the ions are hydrated. Note that the first stage is labelled as lattice dissociation with a positive value — the reverse of the lattice energy as defined in this syllabus.
AnimationEnthalpy of solution calculations
Four salts to try. For the calcium salts remember that one mole of the salt releases two moles of anions into solution.
Four salts to try. For the calcium salts remember that one mole of the salt releases two moles of anions into solution.
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What controls the enthalpy change of hydration23.2.4

Hydration releases energy because water molecules are attracted to the ion. The stronger that ion–dipole attraction, the more exothermic the hydration enthalpy. The same two properties that control lattice energy control it:

Table 23.1 Enthalpy changes of hydration quoted in this chapter and its examination questions, kJ mol−1.
ionΔHhydcomparison
K+−322same charge; Na+ is smaller, so more exothermic
Na+−405
Ca2+about −16002+ ions: roughly four times the 1+ values; Mg2+ smaller than Ca2+
Mg2+about −1900
Cl−−364Cl− smaller than Br−, so more exothermic
Br−about −347

A two-step explanation

To explain why the hydration enthalpy of Br− is more exothermic than that of I−, a published mark scheme gave one mark for "Br− has a smaller ionic radius" and a second for "Br− has stronger attractive forces with water molecules". The examiner reported that the size comparison was usually right but the attraction to water molecules was given much less often. As with lattice energy, the explanation is incomplete until it names what is being attracted to what.

Why ions of higher charge density dominate solubility trends

Both lattice energy and hydration enthalpy become less exothermic as ions get larger, so when you move down a group the two changes pull ΔHsol in opposite directions. Which one wins depends on the particular compounds. For the Group 2 hydroxides and sulfates this balance explains their opposite solubility trends — the full argument belongs to Group 2 at A Level and is developed there. The skill here is the cycle itself: once ΔHlatt and ΔHhyd are known, ΔHsol follows.

Quick check 23.2

  1. Write the equation for the enthalpy change of hydration of the magnesium ion.
    answer
    Mg2+(g) + aq → Mg2+(aq), or Mg2+(g) → Mg2+(aq)
  2. ΔHlatt(KCl) = −701, ΔHhyd(K+) = −322 and ΔHhyd(Cl−) = −364 kJ mol−1. Calculate ΔHsol(KCl).
    answer
    +701 − 322 − 364 = +15 kJ mol−1
  3. Explain why ΔHhyd(Mg2+) is more exothermic than ΔHhyd(Na+).
    answer
    Mg2+ is smaller and more highly charged (higher charge density), so it attracts the water molecules more strongly.
  4. Why can ΔHsol have either sign when ΔHlatt and ΔHhyd each have a fixed sign?
    answer
    It is the difference between a large endothermic term (−ΔHlatt) and a large exothermic term (ΣΔHhyd); whichever is larger decides the sign.
Past-paper practice · Set 23B · Enthalpies of solution and hydration

Examination questions on this part of the unit. Try each one on paper before opening the answer.

Question 23B.1[9]
question 23B.1
Answer and marking guidance
(a) Lattice energy always negative; hydration always negative; solution either ✔ (all three for the mark). (b) The energy (enthalpy) change when one mole of gaseous ions is dissolved in water ✔. (c)(i) Correct six values only: −682.8, 178.2, 590, 1145, 111.9, −324.6 ✔; 2 × used with bromine (2 × 111.9 and 2 × −324.6) ✔; −682.8 = 178.2 + 590 + 1145 + 2(111.9) + 2(−324.6) + ΔHlatt, so ΔHlatt = −2170.6 kJ mol−1 ✔. The Br–Br bond energy, the ionisation energy of bromine and the solution/hydration data are not used here. (ii) Correct three numbers: −2170.6, −103.1, −1579 ✔; ΔHhyd(Br−) = (−2170.6 − 103.1 + 1579) ÷ 2 = −347 kJ mol−1 ✔. (iii) Br− has a smaller ionic radius ✔ so it has stronger attractive forces with water molecules ✔. Examiner insight: hydration was the tick most often misplaced in (a). In (c)(ii) many did not realise the calculation first gives the hydration enthalpy of two moles of Br−. In (iii) the attraction to water molecules was awarded much less often than the size comparison. Show working: credit is available for the method.
Question 23B.2[6]
question 23B.2
Answer and marking guidance
(a) K+(g) + Cl−(g) on the upper box AND K+(aq) + Cl−(aq) on the other ✔; three correct arrows: ΔHlatt from gaseous ions to KCl(s), ΔHsol from KCl(s) to the aqueous ions, ΣΔHhyd from gaseous to aqueous ions ✔. (b) Use of −155, −2493 and 2 × (−364) ✔; ΔHhyd(Mg2+) = −155 + (−2493) − 2(−364) = −1920 kJ mol−1 ✔ (minimum 3 s.f.). (c) Mg2+ is smaller than K+; Mg2+ has a greater charge; so greater attraction between Mg2+ and Cl− (stronger ionic bonds) — two points one mark, all three two marks. Examiner insight: completing the cycle was found harder than identifying the species. In (c) many gave the charge and size but did not state that this leads to greater attraction between the ions in MgCl2.
Question 23B.3[9]
question 23B.3
Answer and marking guidance
(a) Energy change when one mole of ionic solid is formed from gaseous ions ✔. (b) ΔHf = −2237 + 193 + 590 + 1150 + 2(121) + 2(−364) ✔ = −790 kJ mol−1 ✔. (c) −342 kJ mol−1, because the Br atom has a larger radius than Cl, so less attraction for the added electron ✔. (d)(i) Solution: energy change when one mole of solid dissolves in water ✔; hydration: energy change when one mole of gaseous ions dissolves in water ✔. (ii) ΔHhyd(Cl−) = (−2237 − 83 + 1650) ÷ 2 ✔ = −335 kJ mol−1 ✔. Examiner insight: in (a), marks were lost by omitting "one mole" or "gaseous ions". In (b) many did not multiply 121 and/or −364 by two. In (c) answers had to state clearly that the Br atom is larger. In (d)(i) both definitions must say the substance dissolves in water; in (d)(ii) some used their answer to (b) instead of the lattice energy, and others forgot to divide by two and gave −670.

What entropy measures23.3.1

A spontaneous change is one that tends to happen of its own accord, without being driven by a continuous input of energy from outside. Many spontaneous reactions are exothermic, and it is tempting to conclude that releasing energy is what makes a change spontaneous. The evidence says otherwise. Ice melts at room temperature, an endothermic change. Solid hydrated barium hydroxide mixed with solid ammonium chloride reacts readily on mixing and the mixture becomes very cold. Potassium chloride dissolves readily in water even though ΔHsol is positive. Enthalpy alone cannot be the whole story.

What these changes have in common is that the particles, and the energy they carry, end up spread out in more ways than before. Ice becomes a liquid whose molecules are free to move past one another; an ionic lattice becomes ions dispersed through the water; solids react to give ammonia gas, whose molecules fill the whole available volume. The quantity that measures this is entropy.

Definition

Entropy, S, is the number of possible arrangements of the particles and their energy in a given system. The more ways the particles and their energy can be arranged, the greater the entropy. Units: J K−1 mol−1.

Why more arrangements means "more likely"

Imagine four gas particles free to move between the two halves of a container. There is only one way for all four to be in the left-hand half, but there are six ways of having two in each half (particles 1 and 2 on the left, or 1 and 3, or 1 and 4, and so on). If every individual arrangement is equally likely, the evenly spread state turns up six times as often as the all-on-one-side state. With four particles the preference is modest; with a mole of particles it is overwhelming, and the particles are essentially certain to be found spread through the whole container. The same argument applies to the energy: there are far more ways to share a quantity of energy among many particles than among a few.

4 left 0 right 3 left 1 right 2 left 2 right 1 left 3 right 0 left 4 right 0 2 4 6 number of arrangements, W 1 4 6 4 1
Figure 23.7 Four particles distributed between two halves of a container. The number of distinct arrangements W is largest for the even spread (6) and smallest for all four on one side (1). With a mole of particles the even spread is overwhelmingly the most probable state.

This gives a statistical picture of why spontaneous changes happen: a system tends to move towards the state that can be achieved in the most ways — the state of higher entropy — simply because that state is overwhelmingly more probable. The description of entropy as "disorder" is a loose shorthand for this; the syllabus definition in terms of arrangements of particles and energy is the one that earns credit, and examiners have commented that stronger answers used it.

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Enrichment — Boltzmann's equation

The link between entropy and the number of arrangements W can be made exact: S = k ln W, where k is the Boltzmann constant (1.38 × 10−23 J K−1). It is not required by the syllabus, but it explains two things you do need: entropy is a property of a state, so ΔS depends only on the start and finish; and a perfectly ordered crystal at 0 K, which can be arranged in only one way (W = 1), has zero entropy. Every real substance above 0 K therefore has a positive entropy.

Predicting the sign of an entropy change23.3.2

The syllabus asks for the sign of ΔS in three kinds of change. In each, the reasoning comes back to counting arrangements.

(a) Changes of state

In a solid the particles vibrate about fixed positions; in a liquid they move past one another while remaining in contact; in a gas they move independently through the whole volume. Each step from solid to liquid to gas gives the particles more possible positions and more ways of distributing their energy, so

S(solid) < S(liquid) << S(gas)

Melting and boiling therefore have positive ΔS; freezing and condensing negative ΔS. The jump on boiling is far larger than on melting, because separating the particles completely increases the number of possible arrangements enormously. Dissolving an ionic solid in water also has a positive ΔS: the ordered lattice becomes ions dispersed through the solvent.

0 100 200 300 400 temperature / K 0 50 100 150 200 e n t r o p y ,   S   /   J   K   m o l − 1 − 1 melting: particles gain freedom to move boiling: far larger jump — particles spread through the whole volume solid liquid gas schematic — anchored at S(ice) ≈ 48, S(liquid) ≈ 70, S(steam) ≈ 189
Figure 23.8 How the entropy of water changes as it is heated from near 0 K (schematic). Entropy rises steadily with temperature within each state, jumps at the melting point, and jumps much further at the boiling point. Standard molar entropies: ice ≈ 48, liquid water ≈ 70, steam ≈ 189 J K−1 mol−1.

(b) Temperature changes

Heating a substance gives its particles more energy. There are more ways to share a larger amount of energy among the particles, and the particles also occupy a wider range of energy levels, so the entropy of a substance increases with temperature even without a change of state.

(c) Reactions that change the number of gaseous molecules

Because gases have by far the largest entropies, the sign of ΔS for a reaction is almost always decided by the change in the number of moles of gas:

What the explanation must contain

"ΔS is negative because the number of moles decreases" is not enough, and examiners have reported many imprecise answers of this kind. The mark goes to the statement that the number of moles (or molecules) of gas decreases — for example "gas molecules are used up" or "fewer moles of gaseous products than gaseous reactants". Name the state; that is what makes the reasoning chemical rather than arithmetical.

Common trap — melting is not dissolving

Asked to explain the positive entropy change when potassium chloride dissolves, a common error reported by examiners was an explanation in terms of melting. The change is solid lattice → aqueous ions: KCl(s) → K+(aq) + Cl−(aq).

AnimationWhat makes a change spontaneous?
Four changes that happen of their own accord, including some that are endothermic. Decide before each one is explained whether enthalpy alone could account for it.
Four changes that happen of their own accord, including some that are endothermic. Decide before each one is explained whether enthalpy alone could account for it.
AnimationEntropy of solid, liquid and gas
How the entropy of water changes as it is heated through its melting and boiling points, and how to predict the sign of ΔS for a reaction from its states.
How the entropy of water changes as it is heated through its melting and boiling points, and how to predict the sign of ΔS for a reaction from its states.
AnimationPositive or negative?
Eight reactions: predict the sign of ΔS for each, then check the reasoning about moles of gas.
Eight reactions: predict the sign of ΔS for each, then check the reasoning about moles of gas.
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Calculating the entropy change of a reaction23.3.3

Unlike enthalpy, entropy has an absolute zero — a perfect crystal at 0 K — so every substance has a measurable standard molar entropy, S⊖, at 298 K. Elements have non-zero standard entropies (compare ΔHf, which is zero for an element in its standard state). The entropy change of a reaction is then simply the difference between the total entropy of the products and that of the reactants:

ΔS⊖ = ΣS⊖(products) − ΣS⊖(reactants)

Each S⊖ is multiplied by the number of moles in the balanced equation. The result is in J K−1 mol−1, per mole of the reaction as written.

Table 23.2 Standard molar entropies and enthalpy changes of formation at 298 K used in this chapter's worked examples and models. Reference values from the chapter's own data, not the official data booklet; examination questions always supply the values needed.
substanceS⊖ / J K−1 mol−1ΔHf⊖ / kJ mol−1substanceS⊖ / J K−1 mol−1ΔHf⊖ / kJ mol−1
N2(g)1920CaCO3(s)93−1207
H2(g)1310CaO(s)40−635
O2(g)2050CO2(g)214−393.5
NH3(g)193−46CO(g)198−110.5
H2O(l)70−286C(s, graphite)60
H2O(g)189−242CH4(g)186−75
Mg(s)330MgO(s)27−602
Na(s)510NaCl(s)72−411
Cl2(g)2230NO(g)211+90
NO2(g)240+34N2O4(g)304+10

Notice the pattern in the table: the gases all lie between about 130 and 310 J K−1 mol−1, while the solids are mostly below 100. Within the solids, the hard, strongly bonded ones (graphite, MgO) have the smallest entropies, because their particles are held most rigidly and the energy can be arranged in the fewest ways.

Worked example 23.6 · Entropy change for the synthesis of ammonia

GivenN2(g) + 3H2(g) → 2NH3(g); S⊖: N2 192, H2 131, NH3 193 J K−1 mol−1
Prediction4 mol of gas → 2 mol of gas, so ΔS⊖ should be negative.
RelationshipΔS⊖ = ΣS⊖(products) − ΣS⊖(reactants)
SubstitutionΔS⊖ = 2(193) − [192 + 3(131)] = 386 − 585
AnswerΔS⊖ = −199 J K−1 mol−1
CheckNegative, as predicted. The stoichiometric coefficients were applied to the entropies, and the elements' entropies were included (they are not zero).

Two errors to avoid

Leaving out elements. Standard entropies of elements are not zero. Only ΔHf of an element is zero; S⊖ of O2(g) is 205 J K−1 mol−1 and must be included.

Forgetting the coefficients. 2NH3 contributes 2 × 193. A reaction such as Ba(OH)2•8H2O(s) + 2NH4Cl(s) → 2NH3(g) + BaCl2•2H2O(s) + 8H2O(l) has coefficients of 2 and 8 that change the answer completely if missed.

AnimationCalculating entropy changes
A worked calculation laid out in three stages: write the equation for ΔS, look up the data, substitute with the coefficients.
A worked calculation laid out in three stages: write the equation for ΔS, look up the data, substitute with the coefficients.
AnimationEntropy change calculations
Five reactions to calculate. Type the sign as well as the number — the sign is where the chemistry is.
Five reactions to calculate. Type the sign as well as the number — the sign is where the chemistry is.

Beyond the syllabus — entropy of the surroundings

The full statement of the second law involves the entropy change of the surroundings as well as of the system: an exothermic reaction releases heat that increases the entropy of the surroundings. The syllabus states explicitly that use of ΔStotal = ΔSsystem + ΔSsurroundings is not required. Its effect is built into the Gibbs equation that follows, which is all you need.

The Gibbs equation23.4.1

A change is driven in two ways: by releasing energy to the surroundings (negative ΔH) and by increasing the number of possible arrangements (positive ΔS). The Gibbs free energy change combines the two into a single quantity:

ΔG⊖ = ΔH⊖ − TΔS⊖
ΔG⊖standard Gibbs free energy change of the reaction, kJ mol−1
ΔH⊖standard enthalpy change of the reaction, kJ mol−1
Ttemperature in kelvin
ΔS⊖standard entropy change of the system, J K−1 mol−1 — divide by 1000 to convert to kJ K−1 mol−1 before substituting

The TΔS term has units of energy, because entropy is measured per kelvin. It represents the part of the energy change associated with rearranging the particles and their energy. A negative ΔH makes ΔG more negative; so does a positive ΔS, through the −TΔS term. The temperature sets how much weight the entropy term carries: at low temperature ΔG is dominated by ΔH, at high temperature by TΔS.

Calculating ΔG23.4.2

Worked example 23.7 · Is the synthesis of ammonia feasible at 298 K?

GivenN2(g) + 3H2(g) → 2NH3(g); ΔH⊖ = 2 × (−46) = −92 kJ mol−1; ΔS⊖ = −199 J K−1 mol−1 (Worked example 23.6)
UnitsΔS⊖ = −199 ÷ 1000 = −0.199 kJ K−1 mol−1; T = 298 K
SubstitutionΔG⊖ = −92 − 298 × (−0.199) = −92 + 59.3
AnswerΔG⊖ = −32.7 kJ mol−1: feasible at 298 K
CheckThe entropy term opposes the reaction (it is positive), but at 298 K it is smaller than the enthalpy term. As T rises that will change — see Worked example 23.9.

Worked example 23.8 · ΔG from formation and entropy data together

Question. Calculate ΔG⊖ at 298 K for CaCO3(s) → CaO(s) + CO2(g), using the data table.

ΔH⊖ΣΔHf(products) − ΣΔHf(reactants) = (−635 − 393.5) − (−1207) = +178.5 kJ mol−1
ΔS⊖(40 + 214) − 93 = +161 J K−1 mol−1 = +0.161 kJ K−1 mol−1
ΔG⊖178.5 − 298 × 0.161 = 178.5 − 48.0 = +130.5 kJ mol−1
MeaningPositive: calcium carbonate does not decompose at room temperature, even though the entropy change favours it.
Method noteWrite down ΔH and ΔS as separate answers before combining them. An examiner noted that candidates who did so were much more likely to gain partial credit when the final value was wrong.
AnimationHow to calculate ΔG
A calculation laid out step by step: ΔH from formation data, ΔS from entropies, then the Gibbs equation. Watch the moment the entropy is converted from J to kJ.
A calculation laid out step by step: ΔH from formation data, ΔS from entropies, then the Gibbs equation. Watch the moment the entropy is converted from J to kJ.
AnimationCalculating ΔG
Practice calculations. Before substituting, check that T is in kelvin and ΔS is in kJ K⁻¹ mol⁻¹.
Practice calculations. Before substituting, check that T is in kelvin and ΔS is in kJ K⁻¹ mol⁻¹.

Feasibility and the sign of ΔG23.4.3

The feasibility rule

A reaction is feasible (can take place spontaneously) under the stated conditions when ΔG is negative. When ΔG is positive, the reaction is not feasible; the reverse reaction is feasible instead. When ΔG = 0, the system is at the boundary between the two.

"Feasible" is a statement about whether a reaction can happen, not about how fast it happens. The Gibbs equation contains no information about activation energy. Carbon burns in oxygen with a very negative ΔG, yet a diamond left in air is not seen to change: the activation energy is high, and the rate at room temperature is immeasurably slow. A feasible reaction may need heating, a catalyst or a spark to get it going at a useful rate. A thermodynamic prediction and a kinetic one answer different questions, and a complete answer about whether a reaction is observed needs both.

Common trap — "feasible" does not mean "fast"

ΔG < 0 tells you that the products are thermodynamically favoured. It does not say the reaction will be observed. If a question tells you a feasible reaction does not appear to occur, the expected explanation is a high activation energy, so a very slow rate.

How temperature affects feasibility23.4.4

For most reactions ΔH⊖ and ΔS⊖ change only slightly with temperature, and at this level they are treated as constant. The Gibbs equation then has the form of a straight line:

ΔG = ΔH − ΔS × T    compare   y = c + mx

A graph of ΔG against T is a straight line with intercept ΔH (at T = 0) and gradient −ΔS. The sign of ΔS decides whether ΔG rises or falls as the temperature increases, and there are four cases.

Table 23.3 How the signs of ΔH and ΔS decide the effect of temperature on feasibility.
ΔHΔS−TΔSΔG = ΔH − TΔSfeasible?example
negativepositivenegativealways negativeat all temperatures2H2O2(l) → 2H2O(l) + O2(g)
positivenegativepositivealways positiveat no temperature3O2(g) → 2O3(g)
negativenegativepositivenegative at low T, positive at high Tbelow T = ΔH/ΔSN2 + 3H2 → 2NH3; freezing
positivepositivenegativepositive at low T, negative at high Tabove T = ΔH/ΔSCaCO3 → CaO + CO2; melting; boiling
0 200 400 600 800 1000 temperature, T / K −300 −200 −100 0 100 200 300 Δ G   /   k J   m o l − 1 ΔG < 0: feasible ΔG > 0: not feasible gradient = −ΔS intercept at T = 0 is ΔH ΔH < 0, ΔS > 0: feasible at all T ΔH > 0, ΔS < 0: never feasible ΔH < 0, ΔS < 0: feasible below T = ΔH/ΔS ΔH > 0, ΔS > 0: feasible above T = ΔH/ΔS
Figure 23.9 ΔG against temperature for the four sign combinations (illustrative values of ΔH = ±100 kJ mol−1 and ΔS = ±100 or ±200 J K−1 mol−1). The intercept at T = 0 is ΔH; the gradient is −ΔS. Where a line crosses ΔG = 0, feasibility changes.

The temperature at which feasibility changes

For the two cases where the signs of ΔH and ΔS are the same, there is a temperature at which ΔG = 0. Setting ΔG = 0 in the Gibbs equation:

0 = ΔH − TΔS   ⟹   T = ΔH ÷ ΔS    (ΔH in kJ mol−1, ΔS in kJ K−1 mol−1)

For an endothermic reaction with positive ΔS this is the minimum temperature for feasibility; for an exothermic reaction with negative ΔS it is the maximum.

Worked example 23.9 · The minimum temperature for decomposing calcium carbonate

GivenΔH⊖ = +178.5 kJ mol−1; ΔS⊖ = +161 J K−1 mol−1 (Worked example 23.8)
Relationshipfeasible when ΔG < 0; boundary when ΔG = 0, so T = ΔH/ΔS
SubstitutionT = 178.5 ÷ 0.161
AnswerT = 1109 K (836 °C): decomposition is feasible above about 1109 K.
CheckCalcium carbonate is decomposed industrially only at high temperatures, consistent with the prediction. Leaving ΔS in J K−1 mol−1 gives 1.1 K, obviously absurd — a check worth making every time.

Worked example 23.10 · Predicting a boiling point

Question. Use ΔHf and S⊖ for water to estimate the temperature at which H2O(l) → H2O(g) becomes feasible at standard pressure.

ΔH⊖−242 − (−286) = +44 kJ mol−1
ΔS⊖189 − 70 = +119 J K−1 mol−1 = +0.119 kJ K−1 mol−1
T44 ÷ 0.119 = 370 K
EvidenceWater boils at 373 K at standard pressure. The estimate is within 1%, which is strong evidence that the model — ΔH and ΔS treated as constant — is a good approximation, and that boiling happens where ΔG = 0. The small difference comes from ΔH and ΔS changing slightly between 298 K and 373 K.

What examiners look for in a "how does feasibility change with temperature" answer

A published mark scheme for a question on dissolving a salt with positive ΔHsol credited three points: feasibility increases as temperature increases; because ΔS is positive, so TΔS becomes more positive (−TΔS more negative) as T rises; so ΔG becomes negative. Examiners reported that most candidates recognised the trend but few gave the explanation in terms of ΔS and ΔG. In a question about a reaction with negative ΔS, the expected reasoning was that TΔS becomes more negative (−TΔS more positive) as T rises, so the reaction becomes less feasible as ΔG becomes positive. Always name the term that changes and the direction it changes ΔG.

The unit and temperature traps

ΔS in J, ΔH in kJ. Divide ΔS by 1000 before substituting. A report on one calculation lists 2.33 × 105 as a common wrong answer produced by omitting this conversion; another reports graph gradients left unconverted to J K−1 mol−1 or with the wrong sign.

T in kelvin. A reaction "at 800 °C" is at 1073 K. Using T = 800 was the other common error on the same question. When the question asks for a temperature in °C, calculate in kelvin and convert at the end, as one mark scheme required when the answer came out at 214.3 K = −58.7 °C.

AnimationWhen is a reaction feasible?
Find the temperature at which ΔG = 0 for several reactions. In each, decide first whether it is a minimum or a maximum temperature.
Find the temperature at which ΔG = 0 for several reactions. In each, decide first whether it is a minimum or a maximum temperature.
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Quick check 23.3–23.4

  1. Predict the sign of ΔS for 2H2(g) + O2(g) → 2H2O(l), and explain.
    answer
    Negative: three moles of gas become a liquid, so there are far fewer ways to arrange the particles and their energy.
  2. Calculate ΔS⊖ for C(s) + CO2(g) → 2CO(g) from the data table.
    answer
    2(198) − (6 + 214) = +176 J K−1 mol−1
  3. A reaction has ΔH = −50 kJ mol−1 and ΔS = −125 J K−1 mol−1. State the temperature range in which it is feasible.
    answer
    Below T = 50 ÷ 0.125 = 400 K.
  4. A graph of ΔG against T has a gradient of −0.160 kJ K−1 mol−1. What is ΔS?
    answer
    Gradient = −ΔS, so ΔS = +0.160 kJ K−1 mol−1 = +160 J K−1 mol−1.
  5. Why might a reaction with ΔG = −200 kJ mol−1 not be observed at room temperature?
    answer
    Its activation energy may be so high that the rate is negligible; ΔG says nothing about rate.
Past-paper practice · Set 23C · Entropy and Gibbs free energy

Examination questions on this part of the unit. Try each one on paper before opening the answer.

Question 23C.1[3]
question 23C.1
Answer and marking guidance
(i) Negative AND the number of gas molecules is reduced (gaseous F2 is used up to form a solid) ✔. (ii) TΔS becomes more negative as T increases ✔; so the synthesis becomes less feasible AND ΔG becomes (less negative, eventually) positive ✔. Examiner insight: many imprecise answers to (i) omitted the key fact that gas molecules are used up. Part (ii) was found very difficult; strong answers used the Gibbs equation as the basis of a logical explanation, stating that TΔS becomes more negative, or −TΔS more positive, as temperature increases.
Question 23C.2[4]
question 23C.2
Answer and marking guidance
(i) All five points plotted correctly ✔; best-fit straight line with a negative gradient ✔. (ii) Gradient ≈ (−10.3 − 9.9) ÷ (1176 − 1050) = −0.160 kJ K−1 mol−1 ✔ (working seen); gradient = −ΔS⊖, so ΔS⊖ = +0.160 kJ K−1 mol−1 = +160 J K−1 mol−1 (± 10) ✔. Examiner insight: most could calculate the gradient, but many could not turn it into ΔS in J K−1 mol−1: the common errors were not multiplying by 1000 and not converting the negative gradient into a positive ΔS.
Question 23C.3[5]
question 23C.3
Answer and marking guidance
(i) ΔG⊖ = 0, so T = ΔH⊖ ÷ ΔS⊖ ✔; T = 132 ÷ 0.616 = 214.3 K = −58.7 °C ✔ (the answer was asked for in °C). (ii) ΔS⊖ = [203 + 8(70) + 2(192)] − [427 + 2(95)] = 1147 − 617 = +530 J K−1 mol−1 ✔; ΔG⊖ = ΔH⊖ − TΔS⊖ ✔; ΔG⊖ = 133 − 298 × 0.530 = −24.9 kJ mol−1 ✔ (ecf). The reaction is feasible at room temperature, consistent with the observation that it happens on mixing.
Question 23C.4[5]
question 23C.4
Answer and marking guidance
(i) The number of possible arrangements of the particles and the energy in a system (or a measure of the disorder of a system) ✔. (ii) ΔS⊖ = 192.8 + 213.8 − 238.2 − 188.8 = −20.4 J K−1 mol−1 ✔; ΔH⊖ = (−45.9) + (−393.5) − (−101.7) − (−241.8) = −95.9 kJ mol−1 ✔; ΔG⊖ = ΔH⊖ − TΔS⊖ ✔; ΔG⊖ = −95.9 − 298 × (−0.0204) = −89.8 kJ mol−1 ✔. Examiner insight: better answers to (i) stated "the number of possible arrangements of particles and energy in a system". Part (ii) was usually well answered; candidates who wrote down their calculated ΔH and ΔS were much more likely to gain partial credit when the final answer was wrong.
Question 23C.5[4]
question 23C.5
Answer and marking guidance
(i) ΔS negative AND more moles of gaseous reactants than gaseous products (3 mol O2 → 2 mol SO2) ✔. (ii) ΔS⊖ = 50.8 + 197.7 − 43.7 − 5.7 = +199.1 J K−1 mol−1 ✔. (iii) ΔG = ΔH − TΔS ✔; ΔG = +733 − (800 + 273) × 0.218 = +499 kJ mol−1 ✔ (min 3 s.f.): positive, so not feasible at 800 °C. Examiner insight: in (i) a common error was to omit any reference to the gaseous state. In (iii) the common wrong answers were +558.6 (using T = 800 instead of 1073 K) and 2.33 × 105 (ΔS not divided by 1000).
Question 23C.6[2]
question 23C.6
Answer and marking guidance
Feasibility increases as temperature increases; ΔS is positive (dissolving; ΔH is positive); so TΔS becomes more positive / −TΔS more negative as T rises, and ΔG becomes negative — two points one mark, all three two marks. Examiner insight: most recognised that feasibility increases with temperature, but few explained it in terms of ΔS (TΔS becoming more positive) and ΔG becoming more negative.
Question 23C.7[3]
question 23C.7
Answer and marking guidance
(i) The number of possible arrangements of particles and energy in a system ✔. (ii) ΔS is positive AND the ionic lattice (solid) forms aqueous ions, KCl(s) → K+(aq) + Cl−(aq); or ΔS positive AND so ΔG is negative, TΔS being greater than ΔHsol ✔. (iii) More soluble at 80 °C AND ΔG is more negative at higher T (TΔS more positive) ✔. Examiner insight: the definition in (i) was well known. Part (ii) was found difficult: many stated that ΔS was positive without adequate explanation, and a common error was to explain it in terms of melting rather than dissolving.

Misconceptions and the examiner's view23.1–23.4

Misconceptions to correct

"Lattice energy is formed from one mole of gaseous ions." Why it is wrong: one mole of MgCl2 forms from three moles of ions. Correct model: one mole of the compound is formed from its gaseous ions. Consequence: reported as a lost definition mark in several sessions.

"Electron affinity is the energy to remove an electron." Why it is wrong: that is ionisation energy. Correct model: electron affinity adds an electron to each atom in a mole of gaseous atoms. Consequence: examiners report this confusion regularly.

"Lattice energy is bigger because of stronger nuclear attraction." Why it is wrong: lattice energy is about the attraction between oppositely charged ions. Correct model: smaller or more highly charged ions → stronger attraction between the ions. Consequence: the explanation mark is not awarded.

"Hydration enthalpy can be either sign." Why it is wrong: hydration only forms ion–dipole attractions. Correct model: always exothermic; only ΔHsol can be either sign.

"The cycle gives ΔHhyd of the anion directly." Why it is wrong: for MX2 it gives the value for two moles of X−. Correct model: divide by the number of anions per formula.

"Entropy decreases because there are fewer moles." Why it is incomplete: moles of solid barely matter. Correct model: the change in the number of moles of gas decides the sign.

"If ΔG is negative the reaction happens quickly." Why it is wrong: ΔG says nothing about the activation energy. Correct model: feasible means thermodynamically possible; rate is a separate question.

"Substitute ΔS as given, and T as given." Why it is wrong: ΔS is usually in J K−1 mol−1 and ΔH in kJ mol−1; T must be in kelvin. Consequence: answers out by a factor of 1000, or computed at the wrong temperature, are among the most frequently reported errors.

Examiner's overall observation · Chemical energetics

Answered well: recalling the definitions of lattice energy, enthalpy change of hydration and entropy; recognising why a second electron affinity is endothermic; routine ΔS and ΔG calculations laid out with working; and identifying the direction of a trend (for example, that feasibility increases with temperature for a dissolving salt).

Found difficult: selecting the relevant data from a table that deliberately includes extra values; applying multipliers correctly in Born–Haber cycles (the ×2 for two chloride ions or two electrons, halving a bond energy); dividing by two when a cycle yields the hydration enthalpy of two moles of ion; completing an energy cycle with every species and state symbol, including the electrons; and explaining the effect of temperature on feasibility by reference to the TΔS term and the sign of ΔG.

Recurring errors: definitions missing "one mole" or "gaseous"; confusing electron affinity with ionisation energy; explaining an electron-affinity difference by electronegativity; describing energy trends as "increases/decreases" rather than more or less exothermic; stopping at "the ion is smaller" without stating the stronger attraction between ions or to water molecules; ΔS left in J in a ΔG calculation; temperature left in °C; and the ambiguous "it" in comparisons.

What successful answers did: wrote the Hess sum before substituting; kept every sign in brackets; showed calculated ΔH and ΔS separately before combining them; named each ion when comparing; and linked every size or charge argument explicitly to the strength of an attraction.

How the topic is assessed

Table 23.4 Question families seen in the structured papers reviewed for this chapter.
question familytypical demandchemistry needed
Definitions and sign tablesdefine lattice energy, EA, ΔHat, ΔHhyd, ΔHsol, entropy; tick always +, always −, eitherthe exact process, amounts and states
Born–Haber calculationsfind ΔHlatt, ΔHf, an EA or ΔHf of a gaseous ion, selecting dataHess's law with the right multipliers
Completing a cyclelabel the species on each levelatoms after atomisation, electrons after ionisation, state symbols
Comparing lattice or hydration energiesexplain which is more exothermiccharge and radius → attraction between ions or to water
Solution cyclesfind ΔHhyd or ΔHsolΔHsol = −ΔHlatt + ΣΔHhyd, per mole of ion
Entropy and Gibbspredict sign of ΔS; calculate ΔS, ΔG, a boundary temperature; interpret a ΔG–T graph; explain temperature effectsgas moles; unit conversion; ΔG = ΔH − TΔS; gradient = −ΔS

Self-test

Fourteen questions across the whole unit. Each explanation says why the right answer is right and what the wrong ones get wrong.

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Definitions to learn

Table 23.5 The definitions this unit examines. The italicised words are the ones whose omission most often costs the mark.
termdefinitionexample equation
enthalpy change of atomisationenthalpy change when one mole of gaseous atoms is formed from the element in its standard state under standard conditions½Cl2(g) → Cl(g)
lattice energyenthalpy change when one mole of an ionic compound is formed from its gaseous ions under standard conditionsNa+(g) + Cl−(g) → NaCl(s)
first electron affinityenthalpy change when one mole of electrons is added to one mole of gaseous atoms to form one mole of gaseous 1− ionsO(g) + e− → O−(g)
second electron affinityenthalpy change when one mole of electrons is added to one mole of gaseous 1− ions to form one mole of gaseous 2− ionsO−(g) + e− → O2−(g)
enthalpy change of hydrationenthalpy change when one mole of a gaseous ion dissolves in sufficient water to form an infinitely dilute solutionMg2+(g) → Mg2+(aq)
enthalpy change of solutionenthalpy change when one mole of an ionic solid dissolves in sufficient water to form an infinitely dilute solutionKCl(s) → K+(aq) + Cl−(aq)
entropy, Sthe number of possible arrangements of the particles and their energy in a given system—
Gibbs free energy changeΔG⊖ = ΔH⊖ − TΔS⊖; a reaction is feasible when ΔG is negative—

Data used in this chapter

The values used in the text, figures and models come from three places: the data printed in the examination questions reproduced here, the worked examples' own stated data, and a small table of standard entropies and enthalpies of formation given with the entropy section. They are reference values for learning the methods, not the official data booklet. Different sources quote slightly different values for the same quantity — the first electron affinity of chlorine appears as −349 in one question and −364 in another, and the hydration enthalpy of Ca2+ as −1579 and −1650 — so in an examination always use the value the question gives.

The Born–Haber and solution-cycle figures are drawn with heights roughly proportional to the enthalpy changes, but with every step given a minimum height so that small steps remain legible; their vertical scales are approximate. The entropy–temperature graph is schematic, anchored at the standard molar entropies of ice, liquid water and steam.

Summary

23.1 Lattice energy and Born–Haber cycles

23.2 Enthalpies of solution and hydration

23.3 Entropy change

23.4 Gibbs free energy change

Examination checklist

Knowledge organiser

ideakey facts and relationshipsmust-remember distinctions and common errors
AtomisationX(standard state) → one mole X(g); always +; ½ bond energy for X2atoms, not ions; Br2(l) and I2(s) need vaporisation too
Lattice energygaseous ions → one mole solid; always −; more negative for higher charge, smaller ions"one mole of compound", not "one mole of ions"; attraction between ions, not nuclear attraction
Electron affinityEA1: X(g) + e− → X−(g), usually −; EA2: X−(g) + e− → X2−(g), +adds, not removes, an electron; "less exothermic", not "decreases"
Group trends in EAless exothermic down Groups 16 and 17: distance, shieldingF and O smaller than expected: crowded small shell
Born–HaberΔHf = ΣΔHat + ΣIE + ΣEA + ΔHlattmultipliers; signs in brackets; ignore distractor data
HydrationXn±(g) → Xn±(aq); always −; more negative for small, highly charged ionsexplanation needs attraction to water molecules
SolutionΔHsol = −ΔHlatt + ΣΔHhyd; either sign÷ number of ions for one ion's ΔHhyd
Entropyarrangements of particles and energy; J K−1 mol−1; ΔS = ΣS(products) − ΣS(reactants)moles of gas decide the sign; elements' S ≠ 0
GibbsΔG = ΔH − TΔS; feasible if ΔG < 0; Tboundary = ΔH/ΔSΔS ÷ 1000; T in K; feasible ≠ fast
ΔG–T graphstraight line; intercept ΔH; gradient −ΔSgradient in kJ → × 1000 and change sign for ΔS in J
Chemical energetics · Cambridge International AS & A Level Chemistry 9701 · A Level topic 23

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