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:
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.
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:
- nuclear charge — more protons attract the incoming electron more strongly;
- distance — the further the outer shell is from the nucleus, the weaker the attraction;
- shielding — more complete inner shells between nucleus and outer shell reduce the attraction the incoming electron feels.
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.
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
- Write the equation, with state symbols, for the first electron affinity of sulfur.
answer
S(g) + e− → S−(g) - Write the equation for the lattice energy of calcium fluoride.
answer
Ca2+(g) + 2F−(g) → CaF2(s) - 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. - 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:
- directly: elements in their standard states → ionic solid, with enthalpy change ΔHf;
- indirectly: elements → gaseous atoms → gaseous ions → ionic solid, via atomisation, ionisation energy, electron affinity and finally the lattice energy.
By Hess's law the two routes have the same total enthalpy change. For a compound Ma+Xb−:
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.
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.
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.
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).
| Given | ΔHf and every step to K+(g) + F−(g); one mole of each ion per KF. |
| Find | ΔHlatt(KF): K+(g) + F−(g) → KF(s) |
| Relationship | ΔHf = ΔHat(K) + ΔHat(F) + IE1(K) + EA1(F) + ΔHlatt |
| Substitution | −563 = (+90) + (+79) + (+418) + (−348) + ΔHlatt |
| Calculation | ΔHlatt = −563 − 239 = −802 |
| Answer | ΔHlatt(KF) = −802 kJ mol−1 |
| Check | Negative, 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).
| Given | A bond energy, not an atomisation enthalpy, for oxygen. MgO contains one O atom, so only half a mole of O=O bonds is broken. |
| Find | ΔHlatt: Mg2+(g) + O2−(g) → MgO(s) |
| Relationship | ΔHf = ΔHat(Mg) + IE1 + IE2 + ½E(O=O) + EA1 + EA2 + ΔHlatt |
| Substitution | −602 = 148 + 736 + 1450 + 248 + (−141) + 798 + ΔHlatt |
| Calculation | sum of steps = +3239; ΔHlatt = −602 − 3239 = −3841 |
| Answer | ΔHlatt(MgO) = −3841 kJ mol−1 |
| Check | About 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.
| Relationship | ΔHf = ΔHat(Li) + ΔHat(F) + IE1(Li) + EA1(F) + ΔHlatt |
| Substitution | −594.1 = 155.2 + 75.3 + 520 + EA1 + (−1017) |
| Calculation | EA1 = −594.1 − 155.2 − 75.3 − 520 + 1017 = −327.6 |
| Answer | EA1(F) ≈ −328 kJ mol−1 |
| Check | Exothermic, 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.
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:
- Ionic charge. The larger the charges on the ions, the stronger the attraction between them and the more exothermic the lattice energy. Doubling the charge on both ions quadruples the charge product.
- Ionic radius. The smaller the ions, the closer together their centres can approach and the stronger the attraction. Smaller ions give a more exothermic 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.
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.
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.
Examination questions on this part of the unit. Try each one on paper before opening the answer.
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
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.
- Hydration is always exothermic: ion–dipole attractions form and nothing is broken.
- Solution can be exothermic or endothermic, because it is the balance between breaking up the lattice (endothermic) and hydrating the ions (exothermic).
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:
- 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.
- 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:
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.
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
| Given | ΔHlatt(NaCl) = −787; ΔHhyd(Na+) = −405; ΔHhyd(Cl−) = −364 kJ mol−1 |
| Find | ΔHsol: NaCl(s) → Na+(aq) + Cl−(aq) |
| Relationship | ΔHsol = −ΔHlatt + ΔHhyd(Na+) + ΔHhyd(Cl−) |
| Substitution | ΔHsol = −(−787) + (−405) + (−364) |
| Answer | ΔHsol = +18 kJ mol−1 |
| Check | Slightly 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.)
| Relationship | ΔHsol = −ΔHlatt + ΔHhyd(M2+) + 2ΔHhyd(X−) |
| Substitution | −100 = +2500 + (−1900) + 2x |
| Calculation | 2x = −100 − 2500 + 1900 = −700; x = −350 |
| Answer | ΔHhyd(X−) = −350 kJ mol−1 |
| Check | The 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). |
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:
- Ionic charge. A more highly charged ion attracts the polar water molecules more strongly.
- Ionic radius. A smaller ion lets the water molecules approach its centre more closely, so the attraction is stronger.
| ion | ΔHhyd | comparison |
|---|---|---|
| K+ | −322 | same charge; Na+ is smaller, so more exothermic |
| Na+ | −405 | |
| Ca2+ | about −1600 | 2+ ions: roughly four times the 1+ values; Mg2+ smaller than Ca2+ |
| Mg2+ | about −1900 | |
| Cl− | −364 | Cl− 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
- Write the equation for the enthalpy change of hydration of the magnesium ion.
answer
Mg2+(g) + aq → Mg2+(aq), or Mg2+(g) → Mg2+(aq) - ΔHlatt(KCl) = −701, ΔHhyd(K+) = −322 and ΔHhyd(Cl−) = −364 kJ mol−1. Calculate ΔHsol(KCl).
answer
+701 − 322 − 364 = +15 kJ mol−1 - 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. - 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.
Examination questions on this part of the unit. Try each one on paper before opening the answer.
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
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.
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.
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
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.
(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:
- more moles of gas in the products than the reactants → ΔS positive (CaCO3(s) → CaO(s) + CO2(g));
- fewer moles of gas in the products → ΔS negative (N2(g) + 3H2(g) → 2NH3(g); 2Mg(s) + O2(g) → 2MgO(s)).
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).
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:
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.
| substance | S⊖ / J K−1 mol−1 | ΔHf⊖ / kJ mol−1 | substance | S⊖ / J K−1 mol−1 | ΔHf⊖ / kJ mol−1 |
|---|---|---|---|---|---|
| N2(g) | 192 | 0 | CaCO3(s) | 93 | −1207 |
| H2(g) | 131 | 0 | CaO(s) | 40 | −635 |
| O2(g) | 205 | 0 | CO2(g) | 214 | −393.5 |
| NH3(g) | 193 | −46 | CO(g) | 198 | −110.5 |
| H2O(l) | 70 | −286 | C(s, graphite) | 6 | 0 |
| H2O(g) | 189 | −242 | CH4(g) | 186 | −75 |
| Mg(s) | 33 | 0 | MgO(s) | 27 | −602 |
| Na(s) | 51 | 0 | NaCl(s) | 72 | −411 |
| Cl2(g) | 223 | 0 | NO(g) | 211 | +90 |
| NO2(g) | 240 | +34 | N2O4(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
| Given | N2(g) + 3H2(g) → 2NH3(g); S⊖: N2 192, H2 131, NH3 193 J K−1 mol−1 |
| Prediction | 4 mol of gas → 2 mol of gas, so ΔS⊖ should be negative. |
| Relationship | ΔS⊖ = ΣS⊖(products) − ΣS⊖(reactants) |
| Substitution | ΔS⊖ = 2(193) − [192 + 3(131)] = 386 − 585 |
| Answer | ΔS⊖ = −199 J K−1 mol−1 |
| Check | Negative, 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.
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⊖ | standard Gibbs free energy change of the reaction, kJ mol−1 |
| ΔH⊖ | standard enthalpy change of the reaction, kJ mol−1 |
| T | temperature 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?
| Given | N2(g) + 3H2(g) → 2NH3(g); ΔH⊖ = 2 × (−46) = −92 kJ mol−1; ΔS⊖ = −199 J K−1 mol−1 (Worked example 23.6) |
| Units | ΔS⊖ = −199 ÷ 1000 = −0.199 kJ K−1 mol−1; T = 298 K |
| Substitution | ΔG⊖ = −92 − 298 × (−0.199) = −92 + 59.3 |
| Answer | ΔG⊖ = −32.7 kJ mol−1: feasible at 298 K |
| Check | The 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 |
| Meaning | Positive: calcium carbonate does not decompose at room temperature, even though the entropy change favours it. |
| Method note | Write 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. |
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:
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.
| ΔH | ΔS | −TΔS | ΔG = ΔH − TΔS | feasible? | example |
|---|---|---|---|---|---|
| negative | positive | negative | always negative | at all temperatures | 2H2O2(l) → 2H2O(l) + O2(g) |
| positive | negative | positive | always positive | at no temperature | 3O2(g) → 2O3(g) |
| negative | negative | positive | negative at low T, positive at high T | below T = ΔH/ΔS | N2 + 3H2 → 2NH3; freezing |
| positive | positive | negative | positive at low T, negative at high T | above T = ΔH/ΔS | CaCO3 → CaO + CO2; melting; boiling |
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:
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
| Given | ΔH⊖ = +178.5 kJ mol−1; ΔS⊖ = +161 J K−1 mol−1 (Worked example 23.8) |
| Relationship | feasible when ΔG < 0; boundary when ΔG = 0, so T = ΔH/ΔS |
| Substitution | T = 178.5 ÷ 0.161 |
| Answer | T = 1109 K (836 °C): decomposition is feasible above about 1109 K. |
| Check | Calcium 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 |
| T | 44 ÷ 0.119 = 370 K |
| Evidence | Water 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.
Quick check 23.3–23.4
- 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. - Calculate ΔS⊖ for C(s) + CO2(g) → 2CO(g) from the data table.
answer
2(198) − (6 + 214) = +176 J K−1 mol−1 - 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. - 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. - 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.
Examination questions on this part of the unit. Try each one on paper before opening the answer.
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
Answer and marking guidance
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
| question family | typical demand | chemistry needed |
|---|---|---|
| Definitions and sign tables | define lattice energy, EA, ΔHat, ΔHhyd, ΔHsol, entropy; tick always +, always −, either | the exact process, amounts and states |
| Born–Haber calculations | find ΔHlatt, ΔHf, an EA or ΔHf of a gaseous ion, selecting data | Hess's law with the right multipliers |
| Completing a cycle | label the species on each level | atoms after atomisation, electrons after ionisation, state symbols |
| Comparing lattice or hydration energies | explain which is more exothermic | charge and radius → attraction between ions or to water |
| Solution cycles | find ΔHhyd or ΔHsol | ΔHsol = −ΔHlatt + ΣΔHhyd, per mole of ion |
| Entropy and Gibbs | predict sign of ΔS; calculate ΔS, ΔG, a boundary temperature; interpret a ΔG–T graph; explain temperature effects | gas 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.
Definitions to learn
| term | definition | example equation |
|---|---|---|
| enthalpy change of atomisation | enthalpy change when one mole of gaseous atoms is formed from the element in its standard state under standard conditions | ½Cl2(g) → Cl(g) |
| lattice energy | enthalpy change when one mole of an ionic compound is formed from its gaseous ions under standard conditions | Na+(g) + Cl−(g) → NaCl(s) |
| first electron affinity | enthalpy change when one mole of electrons is added to one mole of gaseous atoms to form one mole of gaseous 1− ions | O(g) + e− → O−(g) |
| second electron affinity | enthalpy change when one mole of electrons is added to one mole of gaseous 1− ions to form one mole of gaseous 2− ions | O−(g) + e− → O2−(g) |
| enthalpy change of hydration | enthalpy change when one mole of a gaseous ion dissolves in sufficient water to form an infinitely dilute solution | Mg2+(g) → Mg2+(aq) |
| enthalpy change of solution | enthalpy change when one mole of an ionic solid dissolves in sufficient water to form an infinitely dilute solution | KCl(s) → K+(aq) + Cl−(aq) |
| entropy, S | the number of possible arrangements of the particles and their energy in a given system | — |
| Gibbs free energy change | ΔG⊖ = 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
- ΔHat forms one mole of gaseous atoms and is always endothermic; for a diatomic element it is half the bond energy.
- Lattice energy forms one mole of ionic compound from gaseous ions and is always exothermic.
- First EA adds one mole of electrons to one mole of gaseous atoms, usually exothermic; the second EA is endothermic because the electron is repelled by a negative ion.
- EA1 becomes less exothermic down Groups 16 and 17 (greater distance and shielding); F and O are anomalously low because their small outer shells are crowded.
- Born–Haber cycle: ΔHf = ΣΔHat + ΣIE + ΣEA + ΔHlatt, with the formula deciding every multiplier.
- Lattice energy is more exothermic for higher ionic charges and smaller ions (higher charge density); charge dominates.
23.2 Enthalpies of solution and hydration
- ΔHhyd: one mole of gaseous ions → aqueous ions; always exothermic.
- ΔHsol: one mole of solid → aqueous ions; either sign.
- ΔHsol = −ΔHlatt + ΣΔHhyd; divide by the number of ions when finding one ion's ΔHhyd.
- ΔHhyd is more exothermic for smaller, more highly charged ions, which attract water molecules more strongly.
23.3 Entropy change
- Entropy is the number of possible arrangements of particles and their energy; S(solid) < S(liquid) << S(gas).
- ΔS is positive for melting, boiling, dissolving, heating, and reactions that increase the moles of gas.
- ΔS⊖ = ΣS⊖(products) − ΣS⊖(reactants), with coefficients; elements have non-zero S⊖.
23.4 Gibbs free energy change
- ΔG⊖ = ΔH⊖ − TΔS⊖, with T in K and ΔS in kJ K−1 mol−1; feasible when ΔG is negative.
- ΔG against T is a straight line: intercept ΔH, gradient −ΔS.
- When ΔH and ΔS have the same sign, feasibility changes at T = ΔH/ΔS — a minimum temperature if both are positive, a maximum if both are negative.
- Feasibility says nothing about rate: a feasible reaction can be too slow to observe.
Examination checklist
- Can I write, with state symbols, the equation for every defined enthalpy change in this unit?
- Do my definitions contain "one mole", the right species (atoms, ions, compound) and "gaseous" where needed?
- In a Born–Haber cycle, have I multiplied each term by the moles the formula requires, and halved bond energies for one mole of atoms?
- Have I shown atoms (not molecules) after atomisation and the electrons after each ionisation?
- When comparing lattice or hydration enthalpies, have I named the ions, compared charge and radius, and stated the stronger attraction between ions or to water molecules?
- When finding ΔHhyd of one ion from a 1:2 salt, have I divided by two?
- For the sign of ΔS, have I referred to the change in moles of gas (or the change of state)?
- In ΔG calculations, is T in kelvin and ΔS in kJ K−1 mol−1? Have I written ΔH and ΔS separately first?
- When explaining the effect of temperature, have I said how TΔS changes and what that does to the sign of ΔG?
Knowledge organiser
| idea | key facts and relationships | must-remember distinctions and common errors |
|---|---|---|
| Atomisation | X(standard state) → one mole X(g); always +; ½ bond energy for X2 | atoms, not ions; Br2(l) and I2(s) need vaporisation too |
| Lattice energy | gaseous 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 affinity | EA1: X(g) + e− → X−(g), usually −; EA2: X−(g) + e− → X2−(g), + | adds, not removes, an electron; "less exothermic", not "decreases" |
| Group trends in EA | less exothermic down Groups 16 and 17: distance, shielding | F and O smaller than expected: crowded small shell |
| Born–Haber | ΔHf = ΣΔHat + ΣIE + ΣEA + ΔHlatt | multipliers; signs in brackets; ignore distractor data |
| Hydration | Xn±(g) → Xn±(aq); always −; more negative for small, highly charged ions | explanation needs attraction to water molecules |
| Solution | ΔHsol = −ΔHlatt + ΣΔHhyd; either sign | ÷ number of ions for one ion's ΔHhyd |
| Entropy | arrangements of particles and energy; J K−1 mol−1; ΔS = ΣS(products) − ΣS(reactants) | moles of gas decide the sign; elements' S ≠ 0 |
| Gibbs | ΔG = ΔH − TΔS; feasible if ΔG < 0; Tboundary = ΔH/ΔS | ΔS ÷ 1000; T in K; feasible ≠ fast |
| ΔG–T graph | straight line; intercept ΔH; gradient −ΔS | gradient in kJ → × 1000 and change sign for ΔS in J |