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This final lesson brings together all the topics from the course into exam-style problem solving. The key to success in energetics questions is a systematic approach: identify what data you have, decide which method to use, set up the calculation clearly, and check your answer makes sense. This lesson works through multi-step problems covering every area of the syllabus, with detailed solutions and exam technique advice.
Some exam questions give you several thermochemical equations and ask you to calculate ΔH for a target reaction. The approach is:
Calculate ΔH for: C₂H₂(g) + 2H₂(g) → C₂H₆(g)
Given:
Solution:
Use (1) as-is: C₂H₂ on the left. ΔH = −1300 Reverse (2): C₂H₆ on the right. ΔH = +1560 Multiply (3) by 2: 2H₂ on the left. ΔH = 2 × (−286) = −572
Cancel CO₂, H₂O, and O₂ terms:
C₂H₂(g) + 2H₂(g) → C₂H₆(g)
ΔH = −1300 + 1560 + (−572) = −312 kJ mol⁻¹
Sign check: Hydrogenation adds hydrogen across a triple bond, forming more stable single bonds. This should be exothermic. ΔH = −312. Correct.
These problems give you all but one value and ask you to calculate the unknown. The method is always the same: write the Hess's law equation, substitute known values, and solve for the unknown.
Construct a Born-Haber cycle for KBr and calculate EA₁(Br).
| Quantity | Value / kJ mol⁻¹ |
|---|---|
| ΔH°f(KBr) | −394 |
| ΔH°at(K) | +89 |
| ΔH°at(Br) | +112 |
| IE₁(K) | +419 |
| ΔH°latt(KBr) | −679 |
| EA₁(Br) | ? |
ΔH°f = ΔH°at(K) + ΔH°at(Br) + IE₁(K) + EA₁(Br) + ΔH°latt
−394 = (+89) + (+112) + (+419) + EA₁ + (−679)
−394 = +620 + (−679) + EA₁
−394 = −59 + EA₁
EA₁(Br) = −394 + 59 = −335 kJ mol⁻¹
The data book value is −342 kJ mol⁻¹, close to our answer.
| Quantity | Value / kJ mol⁻¹ |
|---|---|
| ΔH°f(MgO) | −602 |
| ΔH°at(Mg) | +148 |
| ΔH°at(O) | +249 |
| IE₁(Mg) | +738 |
| IE₂(Mg) | +1451 |
| EA₁(O) | −141 |
| EA₂(O) | +798 |
| ΔH°latt(MgO) | ? |
ΔH°f = ΔH°at(Mg) + ΔH°at(O) + IE₁ + IE₂ + EA₁ + EA₂ + ΔH°latt
−602 = (+148) + (+249) + (+738) + (+1451) + (−141) + (+798) + ΔH°latt
−602 = +3243 + ΔH°latt
ΔH°latt = −602 − 3243 = −3845 kJ mol⁻¹
The literature value is −3850 kJ mol⁻¹. The enormous magnitude reflects the 2+ and 2− charges and small ionic radii.
graph TD
A["Mg(s) + ½O₂(g)"] -->|"ΔH°f = −602"| H["MgO(s)"]
A -->|"+148"| B["Mg(g) + ½O₂(g)"]
B -->|"+249"| C["Mg(g) + O(g)"]
C -->|"+738"| D["Mg⁺(g) + O(g)"]
D -->|"+1451"| E["Mg²⁺(g) + O(g)"]
E -->|"−141"| F["Mg²⁺(g) + O⁻(g)"]
F -->|"+798"| G["Mg²⁺(g) + O²⁻(g)"]
G -->|"ΔH°latt = −3845"| H
A student burns 0.92 g of ethanol (Mᵣ = 46.0) and heats 200 g of water from 20.0 °C to 31.5 °C. Calculate the experimental ΔH°c and compare it with the value calculated from enthalpies of formation.
Calorimetry: q = mcΔT = 200 × 4.18 × 11.5 = 9614 J = 9.614 kJ Moles = 0.92 / 46.0 = 0.020 mol ΔH°c(experimental) = −9.614 / 0.020 = −481 kJ mol⁻¹
Hess's law (formation data): C₂H₅OH(l) + 3O₂(g) → 2CO₂(g) + 3H₂O(l)
ΔH°c = [2(−394) + 3(−286)] − [(−277) + 0]
ΔH°c = [−788 − 858] − [−277]
ΔH°c = −1646 + 277 = −1369 kJ mol⁻¹
The experimental value (−481) is much less exothermic than the accepted value (−1369) due to significant heat losses in the simple calorimetry setup.
For the reaction: 2SO₂(g) + O₂(g) → 2SO₃(g)
Given:
Step 1: Calculate ΔS°.
ΔS° = [2(256.6)] − [2(248.1) + 205.0]
ΔS° = 513.2 − 701.2 = −188.0 J K⁻¹ mol⁻¹
Convert: ΔS° = −0.1880 kJ K⁻¹ mol⁻¹
Step 2: Calculate ΔG at 298 K.
ΔG = ΔH − TΔS = (−198) − (298)(−0.1880) = −198 + 56.0 = −142.0 kJ mol⁻¹
Feasible at 298 K.
Step 3: Find the temperature above which the reaction becomes infeasible.
T = ΔH / ΔS = −198 / −0.1880 = 1053 K (≈ 780 °C)
This is Case 3 (ΔH negative, ΔS negative): feasible at low temperatures, infeasible above 1053 K. The Contact process operates at 400–450 °C (673–723 K), well within the feasible range but high enough to give a reasonable rate with a V₂O₅ catalyst.
A reaction has ΔG = −100 kJ mol⁻¹ at 400 K and ΔH = −160 kJ mol⁻¹. Calculate ΔS.
ΔG = ΔH − TΔS
−100 = −160 − (400)ΔS
(400)ΔS = −160 + 100 = −60
ΔS = −60 / 400 = −0.150 kJ K⁻¹ mol⁻¹ = −150 J K⁻¹ mol⁻¹
CH₂=CHCH₃(g) + 9/2 O₂(g) → 3CO₂(g) + 3H₂O(g)
Using bond enthalpies: C=C +614, C–C +347, C–H +413, O=O +498, C=O +805, O–H +463.
Bonds broken in propene and O₂:
Bonds formed in CO₂ and H₂O:
ΔH = 5680 − 7608 = −1928 kJ mol⁻¹
Given:
ΔH°sol = −(−1037) + (−520) + (−506) = 1037 − 520 − 506 = +11 kJ mol⁻¹
Slightly endothermic. LiF is sparingly soluble — the enthalpy of solution is positive and the entropy increase on dissolving is relatively small (both ions are small and strongly hydrated, restricting the water molecules' freedom).
| What to check | Why |
|---|---|
| Are all units consistent? | ΔH in kJ, ΔS in J — convert before combining |
| Temperature in kelvin? | T(K) = T(°C) + 273 |
| Correct sign on every quantity? | One wrong sign can reverse your answer |
| Stoichiometric coefficients applied? | 2 moles of Cl⁻ means 2 × ΔH°hyd(Cl⁻) |
| Sign check on the answer? | Does the sign make chemical sense? Combustion should be exothermic. |
| Correct formula for the method? | Formation: products − reactants. Combustion: reactants − products. |
| State symbols included? | Essential for full marks in equation-writing questions |
| Bond enthalpy: which bonds actually break? | Only break/make bonds that change in the reaction |
| Formula | Use |
|---|---|
| q = mcΔT | Calorimetry: energy transferred |
| ΔH = ΣΔH°f(products) − ΣΔH°f(reactants) | Hess's law with formation data |
| ΔH = ΣΔH°c(reactants) − ΣΔH°c(products) | Hess's law with combustion data |
| ΔH = Σ(bonds broken) − Σ(bonds formed) | Bond enthalpy method |
| ΔH°f = sum of Born-Haber cycle steps | Born-Haber cycle (rearrange for unknown) |
| ΔH°sol = −ΔH°latt(formation) + ΣΔH°hyd | Dissolving energy cycle |
| ΔS° = ΣS°(products) − ΣS°(reactants) | Entropy change |
| ΔG = ΔH − TΔS | Gibbs free energy |
| T = ΔH / ΔS | Transition temperature (when ΔG = 0) |
This lesson has worked through representative problems from every major area of the energetics course. The keys to exam success are:
Edexcel 9CH0 specification Topics 8 + 13 are integrated synoptically in this lesson, with the highest density of cross-strand connections in the energetics chapter (refer to the official specification document for exact wording). Synoptic energetics questions appear primarily on Paper 3 (synoptic), where 12–15 mark items routinely combine: Hess cycles (Topic 8.2) with Born–Haber cycles (Topic 13); enthalpies of solution and hydration (Topic 13) with entropy and Gibbs free energy (Topic 13); bond enthalpies (Topic 8.3) with kinetics (Topic 9); and lattice-energy trends (Topic 13) with group 2 chemistry (Topic 4). Multi-step problems demand a procedure: identify what is being asked; identify the data given and missing; choose the appropriate cycle (Hess, Born–Haber, or thermodynamic); calculate; sanity-check sign and order of magnitude; relate to spontaneity and/or equilibrium. Mastery of this lesson is the discriminator between a high A and an A* on Paper 3.
Question (12 marks):
A student investigates the thermal decomposition of MgCO₃(s) → MgO(s) + CO₂(g).
Data:
(a) Use Hess's law to calculate ΔH° for the decomposition. (2) (b) Calculate ΔS° for the decomposition. (2) (c) Determine the temperature above which decomposition is thermodynamically spontaneous. (3) (d) The lattice energy of MgCO₃ is −3122 kJ mol⁻¹; that of MgO is −3791 kJ mol⁻¹. Comment on how the difference relates to the thermal decomposition temperature you calculated. (3) (e) Predict (with reasoning) how the decomposition temperature of BaCO₃ would compare. (2)
Solution with mark scheme:
(a) ΔH° = ΣΔH°_f(prod) − ΣΔH°_f(react) = (−602) + (−394) − (−1096) = +100 kJ mol⁻¹.
M1 — Hess equation. A1 — value with sign.
(b) ΔS° = ΣS°(prod) − ΣS°(react) = (27 + 214) − 66 = +175 J K⁻¹ mol⁻¹.
M1 — substitution. A1 — value with units.
(c) ΔG° = ΔH° − TΔS° = 0 ⟹ T = ΔH°/ΔS° = 100 / 0.175 = 571 K (≈ 298 °C).
M1 — recognise condition. M1 — convert ΔS° to kJ K⁻¹ (or ΔH° to J). A1 — answer with units.
(d) B1 — the lattice energy of MgO is more exothermic than MgCO₃ by 669 kJ mol⁻¹; this drives the reaction forward thermodynamically.
B1 — together with the entropy gain from CO₂ release, the difference in lattice energies sets a moderate threshold T (~571 K), accessible at ordinary furnace temperatures.
B1 — the calculated threshold (571 K = 298 °C) is consistent with the observed decomposition of MgCO₃ in the range 300–500 °C; the kinetic onset typically lags the thermodynamic threshold.
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